text: 1) Starts from "Fluctuations of wind" (O. M.Phillips) : the wind wave formation on water surface by wind is started by a random distribution of normal pressure acting on the water from the wind. By the mechanism developed by O. M. Phillips (in 1957), the water surface is initially at rest and wave generation is started by adding turbulent wind flows and then, by the fluctuations of the wind, normal pressure acting on the water surface. From this pressure fluctuation arise normal and tangential stresses to the surface water, which generates wave behavior on the water surface. It is assumed that:

text: 1) Starts from "Fluctuations of wind" (O. M.Phillips) : the wind wave formation on water surface by wind is started by a random distribution of normal pressure acting on the water from the wind. By the mechanism developed by O. M. Phillips (in 1957), the water surface is initially at rest and wave generation is started by adding turbulent wind flows and then, by the fluctuations of the wind, normal pressure acting on the water surface. From this pressure fluctuation arise normal and tangential stresses to the surface water, which generates wave behavior on the water surface. It is assumed that:

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prompt_style: provide a complete and concise answer to the question based on the context.

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prompt_class: Thomas

text: Internal tides are generated as the surface tides move stratified water up and down sloping topography, which produces a wave in the ocean interior.  So internal tides are internal waves at a tidal frequency.  The other major source of internal waves is the wind which produces internal waves near the inertial frequency.  When a small water parcel is displaced from its equilibrium position, it will return either downwards due to gravity or upwards due to buoyancy.  The water parcel will overshoot its original equilibrium position and this disturbance will set off an internal gravity wave.  Munk (1981) notes, "Gravity waves in the ocean's interior are as common as waves at the sea surface-perhaps even more so, for no one has ever reported an interior calm."

text: Internal tides are generated as the surface

entity_name: Tide

text: tides

text: move stratified water up and down sloping topography, which produces a wave in the ocean interior.  So internal tides are

entity_name: Internal wave

text: internal waves

text: at a tidal frequency.  The other major source of internal waves is the wind which produces internal waves near the inertial frequency.  When a small water parcel is displaced from its equilibrium position, it will return either downwards due to gravity or upwards due to buoyancy.  The water parcel will overshoot its original equilibrium position and this disturbance will set off an internal gravity wave.  Munk (1981) notes, "Gravity waves in the ocean's interior are as common as waves at the sea surface-perhaps even more so, for no one has ever reported an interior calm."

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answers: The water parcel will overshoot its original equilibrium position

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answers: Internal tides

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answers: water parcel is displaced from its equilibrium position

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answers: Internal tides are internal waves at a tidal frequency

answers: NDQ_006458

answers: Internal tides are internal waves at a tidal frequency

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answers: surface tides

answers: NDQ_006460

answers: The water parcel will overshoe its original equilibrium position

answers: NDQ_006461

answers: buoyancy

answer: Yes

answer: Yes

answer: No

answer: Yes

answer: No

answer: 1

text: With the proceeds of the loan, Loomis was able to pay off Kamm. Sheriff Sears of Multnomah County, released the lien.  With the lien gone, the lease of Ocean Wave to the CR&PSN went through.  Ocean Wave began running on July 18, 1895.  Thereafter Ocean Wave was operated on the Columbia River, and advertised, as one of the steamboats of the White Collar Line.

text: With the proceeds of the loan, Loomis was able to pay off Kamm. Sheriff Sears of

entity_name: Multnomah County, Oregon

text: Multnomah County

text: , released the lien.  With the lien gone, the lease of Ocean Wave to the CR&PSN went through.  Ocean Wave began running on July 18, 1895.  Thereafter Ocean Wave was operated on the Columbia River, and advertised, as one of the steamboats of the White Collar Line.

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text: A beach break takes place where waves break on a usually sandy seabed.  An example of a classic beach break is Hossegor in Southern France, which is famous for waves of up to .

text: A

text: beach break

text: takes place where waves break on a usually sandy seabed.  An example of a classic beach break is

entity_name: Soorts-Hossegor

text: Hossegor

text: in

entity_name: Southern France

text: Southern France

text: , which is famous for waves of up to .

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text: When directly generated and affected by local winds, a wind wave system is called a wind sea. After the wind ceases to blow, wind waves are called swells. More generally, a swell consists of wind-generated waves that are not significantly affected by the local wind at that time. They have been generated elsewhere or some time ago. Wind waves in the ocean are called ocean surface waves.

text: When directly generated and affected by local winds, a wind wave system is called a wind sea. After the wind ceases to blow, wind waves are called

entity_name: Swell (ocean)

text: swells

text: . More generally, a swell consists of wind-generated waves that are not significantly affected by the local wind at that time. They have been generated elsewhere or some time ago. Wind waves in the ocean are called ocean surface waves.

method: UvABottomUpChangeOrder

method: UNH-tfidf-stem

method: UNH-tfidf-ptsim

method: UNH-tfidf-lem

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text: On February 17, Ohka, as the 2009 Catch the Wave winner, was granted entrance into a tournament to determine the inaugural Wave Single Champion and defeated rival Misaki Ohata in her semifinal match. On March 17, Ohka defeated Kana in the finals to win the tournament and become the inaugural Wave Single Champion. Ohka made her first successful title defense on April 21 against Yuu Yamagata. On July 15, Ohka became a double champion in Wave, when she and Hikaru Shida defeated Triple Tails.S (Kana and Mio Shirai) for the Wave Tag Team Championship. However, after a reign of only a month, Shidarezakura lost the Wave Tag Team Championship to Yoko Hatanaka (Gami and Tomoka Nakagawa) in their first defense on August 15. On August 25, Ohka made her second successful defense of the Wave Single Championship against rival and winner of the 2013 Catch the Wave, Misaki Ohata. From September 1 to October 6, Ohka took part in the 2013 Dual Shock Wave tournament, where she teamed with Kana under the team name Giann's. The team made it all the way to the finals of the tournament, before losing to Las Aventureras (Ayako Hamada and Yuu Yamagata) in a three-way match, which also included Muscle Venus (Hikaru Shida and Tsukasa Fujimoto). On October 30, Ohka made her third successful defense of the Wave Single Championship against Tomoka Nakagawa, avenging a loss suffered during the 2013 Dual Shock Wave. On November 20, Ohka combined her two tag teams with Hikaru Shida and Kana to form a trio named Shidare Giann's for a 6-Person Tag Tournament. In their first round Two Out of Three Falls match, the three defeated Urayama Arrows (Natsuki Urabe, Rina Yamashita and Yako Fujigasaki). On November 27, Shidare Giann's was eliminated from the tournament in a semifinal submission match by Revolucion Yoko Hatanaka (Gami, Kyoko Kimura and Tomoka Nakagawa). On December 15, Ohka made her fourth successful defense of the Wave Single Championship against Shuu Shibutani. Following Gami's retirement from professional wrestling at the end of 2013, Ohka became the new official representative of Wave. Ohka made her fifth successful defense of the Wave Single Championship on January 26, 2014, when she wrestled Misaki Ohata to a thirty-minute time limit draw. On March 2, Ohka made her sixth successful defense against JWP representative Kayoko Haruyama as part of a storyline rivalry between the two promotions. Ohka's seventh successful title defense took place on April 20, when she defeated Hikaru Shida. From May 5 to June 22, Ohka took part in the round-robin portion of the 2014 Catch the Wave tournament, winning her block with a record of three wins, two draws and one loss, suffered against Tsukasa Fujimoto. On July 27, Ohka was eliminated from the tournament in the semifinals by Misaki Ohata. On August 24, Ohka's seventeen-month reign as the Wave Single Champion came to an end, when she lost the title to the 2014 Catch the Wave winner Hikaru Shida in her eighth defense.

text: On February 17, Ohka, as the 2009 Catch the Wave winner, was granted entrance into a

entity_name: Wave Single Championship

entity_section: Regina di Wave tournament

text: tournament

text: to determine the inaugural

text: Wave Single Champion

text: and defeated rival Misaki Ohata in her semifinal match. On March 17, Ohka defeated Kana in the finals to win the tournament and become the inaugural Wave Single Champion. Ohka made her first successful title defense on April 21 against Yuu Yamagata. On July 15, Ohka became a double champion in Wave, when she and Hikaru Shida defeated Triple Tails.S (Kana and Mio Shirai) for the Wave Tag Team Championship. However, after a reign of only a month, Shidarezakura lost the Wave Tag Team Championship to Yoko Hatanaka (Gami and Tomoka Nakagawa) in their first defense on August 15. On August 25, Ohka made her second successful defense of the Wave Single Championship against rival and winner of the

entity_name: Catch the Wave

text: 2013 Catch the Wave

text: , Misaki Ohata. From September 1 to October 6, Ohka took part in the

entity_name: Dual Shock Wave

text: 2013 Dual Shock Wave

text: tournament, where she teamed with Kana under the team name Giann's. The team made it all the way to the finals of the tournament, before losing to Las Aventureras (Ayako Hamada and Yuu Yamagata) in a three-way match, which also included Muscle Venus (Hikaru Shida and Tsukasa Fujimoto). On October 30, Ohka made her third successful defense of the Wave Single Championship against Tomoka Nakagawa, avenging a loss suffered during the 2013 Dual Shock Wave. On November 20, Ohka combined her two tag teams with Hikaru Shida and Kana to form a trio named Shidare Giann's for a 6-Person Tag Tournament. In their first round Two Out of Three Falls match, the three defeated Urayama Arrows (Natsuki Urabe, Rina Yamashita and Yako Fujigasaki). On November 27, Shidare Giann's was eliminated from the tournament in a semifinal

entity_name: Professional wrestling match types

entity_section: Variations of singles matches

text: submission match

text: by Revolucion Yoko Hatanaka (Gami, Kyoko Kimura and Tomoka Nakagawa). On December 15, Ohka made her fourth successful defense of the Wave Single Championship against Shuu Shibutani. Following Gami's retirement from professional wrestling at the end of 2013, Ohka became the new official representative of Wave. Ohka made her fifth successful defense of the Wave Single Championship on January 26, 2014, when she wrestled Misaki Ohata to a thirty-minute time limit draw. On March 2, Ohka made her sixth successful defense against JWP representative Kayoko Haruyama as part of a storyline rivalry between the two promotions. Ohka's seventh successful title defense took place on April 20, when she defeated Hikaru Shida. From May 5 to June 22, Ohka took part in the round-robin portion of the

text: 2014 Catch the Wave

text: tournament, winning her block with a record of three wins, two draws and one loss, suffered against Tsukasa Fujimoto. On July 27, Ohka was eliminated from the tournament in the semifinals by Misaki Ohata. On August 24, Ohka's seventeen-month reign as the Wave Single Champion came to an end, when she lost the title to the 2014 Catch the Wave winner Hikaru Shida in her eighth defense.

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answer: No

answer: No

answer: No

answer: No

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text: P-waves are a type of elastic wave, and are one of the two main types of elastic body waves, called seismic waves in seismology, that travel through a continuum and are the first waves from an earthquake to arrive at a seismograph. The continuum is made up of gases (as sound waves), liquids, or solids, including the Earth. P-waves can be produced by earthquakes and recorded by seismographs. The name P-wave can stand for either pressure wave  as it is formed from alternating compressions and rarefactions or primary wave, as it has the highest velocity and is therefore the first wave to be recorded.

text: P-waves are a type of

text: elastic wave

text: , and are one of the two main types of elastic

text: body waves

text: , called

text: seismic waves

text: in seismology, that travel through a

text: continuum

text: and are the first waves from an earthquake to arrive at a seismograph. The

text: continuum

text: is made up of

text: gas

text: es (as

text: sound

text: waves), liquids, or solids, including the

text: Earth

text: . P-waves can be produced by

text: earthquakes

text: and recorded by

text: seismographs

text: . The name P-wave can stand for either pressure wave  as it is formed from alternating

text: compression

text: s and

text: rarefaction

text: s or primary wave, as it has the highest velocity and is therefore the first wave to be recorded.

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text: The presence of coastal regions both in the Atlantic and the Pacific oceans increases the risk of hurricanes and tropical storms. Waves in the trade winds in the Atlantic Ocean—areas of converging winds that move along the same track as the prevailing wind—create instabilities in the atmosphere that may lead to the formation of hurricanes.  Some of the events of this type that have affected the country are:

text: The presence of coastal regions both in the Atlantic and the Pacific oceans increases the risk of

text: hurricane

text: s and

text: tropical storm

text: s. Waves in the trade winds in the Atlantic Ocean—areas of converging winds that move along the same track as the prevailing wind—create instabilities in the

text: atmosphere

text: that may lead to the formation of

text: hurricanes

text: .  Some of the events of this type that have affected the country are:

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answer: Yes

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answer: 1

text: Toward the end of September 2001, a poorly defined tropical wave moved westward across the tropical Atlantic Ocean through an area of hostile wind shear, which was caused by a large upper-level low within a trough to the northeast of the Lesser Antilles. A few days later, the upper-level low detached from the trough and moved southwestward over the Caribbean Sea, allowing for an upper-level ridge, or high-pressure area, to form over the tropical wave. The change provided a favorable environment for tropical development, and an area of convection soon blossomed along the wave's axis. As the tropical wave approached the Lesser Antilles, a mid-level wind circulation formed within the deepest part of the convection, and a low-level circulation became gradually more pronounced on satellite imagery. Although its low-level circulation was small and poorly defined, the system increased in organization enough to be classified as Tropical Depression Eleven at 12:00 UTC on October 4, located about 100 mi (160 km) southeast of Barbados. Operationally, however, Hurricane Hunters did not confirm the depression's formation until nine hours later.

text: Toward the end of September 2001, a poorly defined

text: tropical wave

text: moved westward across the tropical Atlantic Ocean through an area of hostile

text: wind shear

text: , which was caused by a large

text: upper-level low

text: within a

text: trough

text: to the northeast of the

text: Lesser Antilles

text: . A few days later, the upper-level low detached from the trough and moved southwestward over the Caribbean Sea, allowing for an upper-level

text: ridge

text: , or high-pressure area, to form over the tropical wave. The change provided a favorable environment for

text: tropical development

text: , and an area of

text: convection

text: soon blossomed along the wave's axis. As the tropical wave approached the Lesser Antilles, a mid-level

text: wind circulation

text: formed within the deepest part of the convection, and a low-level circulation became gradually more pronounced on satellite imagery. Although its low-level circulation was small and poorly defined, the system increased in organization enough to be classified as Tropical Depression Eleven at 12:00

text: UTC

text: on October 4, located about 100 mi (160 km) southeast of

text: Barbados

text: . Operationally, however,

text: Hurricane Hunters

text: did not confirm the depression's formation until nine hours later.

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answers: Tropical Depression Eleven

answers: NDQ_006453

answers: tropical wave

answers: NDQ_006455

answers: The change provided a favorable environment for tropical development

answers: NDQ_006456

answers: low-level

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answers: low-level circulation

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answers: a poorly defined tropical wave

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answers: upper-level low

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answers: Atlantic Ocean

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answer: Yes

answer: Yes

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text: The storm moved ashore with a high storm surge, estimated at  in Bharuch. Winds reached 85 km/h (53 mph) in Veraval, while heavy rainfall spread across the region, totaling over  in some parts of Gujarat. South of the landfall point, high winds and waves washed 10 boats ashore near Mumbai, forcing the crews to be rescued by helicopters. The storm disrupted wheat production and port operations in western India. In Gujarat, the storm uprooted trees and damaged  of crop fields, with 2,113 cattle killed between Gujarat and neighboring Maharashtra to the south. The storm damaged 41,134 houses in the two states, and overall damage was estimated at RS$196 million (US$5.6 million). There were 47 deaths related to the cyclone.

text: The storm moved ashore with a high

text: storm surge

text: , estimated at  in

text: Bharuch

text: . Winds reached 85 km/h (53 mph) in

text: Veraval

text: , while heavy rainfall spread across the region, totaling over  in some parts of Gujarat. South of the landfall point, high winds and waves washed 10 boats ashore near Mumbai, forcing the crews to be rescued by helicopters. The storm disrupted wheat production and port operations in western India. In Gujarat, the storm uprooted trees and damaged  of crop fields, with 2,113 cattle killed between Gujarat and neighboring

text: Maharashtra

text: to the south. The storm damaged 41,134 houses in the two states, and overall damage was estimated at RS$196 million (US$5.6 million). There were 47 deaths related to the cyclone.

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text: The transfer of energy between the wind blowing over the surface of an ocean and the ocean's upper layer is an important element in wave dynamics.  The spectral wave transport equation is used to describe the change in wave spectrum over changing topography.  It simulates wave generation, wave movement (propagation within a fluid), wave shoaling, refraction, energy transfer between waves, and wave dissipation.  Since surface winds are the primary forcing mechanism in the spectral wave transport equation, ocean wave models use information produced by numerical weather prediction models as inputs to determine how much energy is transferred from the atmosphere into the layer at the surface of the ocean. Along with dissipation of energy through whitecaps and resonance between waves, surface winds from numerical weather models allow for more accurate predictions of the state of the sea surface.<ref>{{cite journal|last=Bender|first=Leslie C.|title=Modification of the Physics and Numerics in a Third-Generation Ocean Wave Model|journal=Journal of Atmospheric and Oceanic Technology|date=January 1996|volume=13|issue=3|pages=726 |doi=10.1175/1520-0426(1996)013

text: The transfer of energy between the wind blowing over the surface of an ocean and the ocean's upper layer is an important element in wave dynamics.  The

text: spectral wave transport equation

text: is used to describe the change in wave spectrum over changing topography.  It simulates wave generation, wave movement (propagation within a fluid),

text: wave shoaling

text: refraction

text: , energy transfer between waves, and wave dissipation.  Since surface winds are the primary forcing mechanism in the spectral wave transport equation, ocean wave models use information produced by numerical weather prediction models as inputs to determine how much energy is transferred from the atmosphere into the layer at the surface of the ocean. Along with dissipation of energy through

text: whitecaps

text: and

text: resonance

text: between waves, surface winds from numerical weather models allow for more accurate predictions of the state of the sea surface.<ref>{{cite journal|last=Bender|first=Leslie C.|title=Modification of the Physics and Numerics in a Third-Generation Ocean Wave Model|journal=

entity_name: Journal of Atmospheric and Oceanic Technology

text: Journal of Atmospheric and Oceanic Technology

text: |date=January 1996|volume=13|issue=3|pages=726 |doi=10.1175/1520-0426(1996)013

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answers: Wave shoaling

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answers: NDQ_006457

answers: Wave energy is lowest at the surface and increases with depth.

answers: NDQ_006458

answers: Wave dissipation

answers: NDQ_006459

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answers: NDQ_006460

answers: surface of the ocean

answers: NDQ_006461

answers: wave shoaling

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: 1

text: In physics, a surface wave is a mechanical wave that propagates along the interface between differing media, usually as a gravity wave between two fluids with different densities.  A surface wave can also be an elastic (or a seismic) wave, such as with a Rayleigh or Love wave. It can also be an electromagnetic wave guided by a refractive index gradient, or along an interface between two media having different dielectric constants. In radio transmission, a ground wave is a surface wave that propagates close to the surface of the Earth.

text: In

text: physics

text: , a surface wave is a

text: mechanical wave

text: that propagates along the

text: interface

text: between differing media, usually as a

text: gravity wave

text: between two

text: fluid

text: s with different densities.  A surface wave can also be an elastic (or a

text: seismic

text: ) wave, such as with a

text: Rayleigh

text: or

text: Love

text: wave. It can also be an

text: electromagnetic wave

text: guided by a

text: refractive index

text: gradient

text: , or along an interface between two media having different dielectric constants. In

text: radio

text: transmission

text: , a ground wave is a surface wave that propagates close to the surface of the

text: Earth

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answers: NDQ_006460

answers: 0

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answers: NDQ_006452

answers: surface wave

answers: NDQ_006453

answers: ground wave

answers: NDQ_006455

answers: interface between differing media

answers: NDQ_006456

answers: gravity

answers: NDQ_006457

answers: surface wave

answers: NDQ_006458

answers: ground wave

answers: NDQ_006459

answers: Rayleigh or Love wave

answers: NDQ_006460

answers: It can also be an electromagnetic wave

answers: NDQ_006461

answers: gravity wave

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Al Gal is a beach area located on the west coast of Israel near the city of Bat Yam. It is an exposed beach break and reef break that has fairly consistent surf, specially during the months of summer when most of the surf comes in the form of wind waves.

text: Al Gal is a beach area located on the west coast of

text: Israel

text: near the city of

text: Bat Yam

text: . It is an exposed

text: beach break

text: and

text: reef break

text: that has fairly consistent surf, specially during the months of summer when most of the surf comes in the form of

text: wind waves

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answers: 4

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answers: NDQ_006452

answers: reef break

answers: NDQ_006453

answers: wind waves

answers: NDQ_006455

answers: wind

answers: NDQ_006456

answers: fast

answers: NDQ_006457

answers: surface

answers: NDQ_006458

answers: reef break

answers: NDQ_006459

answers: wind

answers: NDQ_006460

answers: coast

answers: NDQ_006461

answers: consistent surf

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: 1

text: Although Hurricane Katrina made landfall well to the west, Alabama and the Florida Panhandle were both affected by tropical-storm force winds and a storm surge varying from  around Mobile Bay, with higher waves on top. Sustained winds of  were recorded in Mobile, Alabama, and the storm surge there was approximately . The surge caused significant flooding several miles inland along Mobile Bay. Four tornadoes were also reported in Alabama. Ships, oil rigs, boats and fishing piers were washed ashore along Mobile Bay: the cargo ship M/V Caribbean Clipper and many fishing boats were grounded at Bayou La Batre.

text: Although Hurricane Katrina made landfall well to the west, Alabama and the Florida Panhandle were both affected by tropical-storm force winds and a storm surge varying from  around

text: Mobile Bay

text: , with higher waves on top. Sustained winds of  were recorded in

text: Mobile, Alabama

text: , and the storm surge there was approximately . The surge caused significant flooding several miles inland along Mobile Bay. Four tornadoes were also reported in Alabama. Ships, oil rigs, boats and fishing

text: pier

text: s were washed ashore along Mobile Bay: the cargo ship M/V Caribbean Clipper and many fishing boats were grounded at

text: Bayou La Batre

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text: Due to advance warning, there was minimal damage to shipping in the region. However, high waves damaged the steamer Madison with 90 people on board and caused it to drift off Cape Charles, which necessitated rescue from the Coast Guard. Inland flooding occurred along the James River as far west as Richmond, where damage was limited to downed trees and broken windows. The pier of the Jamestown Ferry was washed out in Surry  and a marina at Jordan Point near Hopewell was wrecked after the river reached the highest level on record. A powerful storm surge moved up the Chesapeake Bay and flooded waterfront locations. At Colonial Beach along the Potomac River, the surge flooded the town with  of water and wrecked a local amusement park. The Potomac in Alexandria was at its highest level since 1899, causing floods  deep along U.S. Route 1, and flooding the Old Town section. High winds in the city caused power outages, and flooding along the Cameron Run washed out a bridge. The combination of rain and winds damaged crops in Fairfax and Loudoun counties, mainly to corn and peaches. Statewide, the storm caused $5.25 million in crop damage, largely to corn and tobacco. Damage in the state was estimated at $17.5 million, and there were 15 deaths. After the storm, about 350 people helped clear debris from the streets of Norfolk.

text: Due to advance warning, there was minimal damage to shipping in the region. However, high waves damaged the steamer Madison with 90 people on board and caused it to drift off Cape Charles, which necessitated rescue from the Coast Guard. Inland flooding occurred along the

text: James River

text: as far west as

text: Richmond

text: , where damage was limited to downed trees and broken windows. The pier of the

text: Jamestown Ferry

text: was washed out in

text: Surry

text: and a marina at

text: Jordan Point

text: near

text: Hopewell

text: was wrecked after the river reached the highest level on record. A powerful storm surge moved up the Chesapeake Bay and flooded waterfront locations. At

text: Colonial Beach

text: along the

text: Potomac River

text: , the surge flooded the town with  of water and wrecked a local amusement park. The Potomac in

text: Alexandria

text: was at its highest level since 1899, causing floods  deep along

text: U.S. Route 1

text: , and flooding the

entity_name: List of neighborhoods in Alexandria, Virginia

text: Old Town section

text: . High winds in the city caused power outages, and flooding along the

text: Cameron Run

text: washed out a bridge. The combination of rain and winds damaged crops in

text: Fairfax

text: and

text: Loudoun

text: counties, mainly to corn and peaches. Statewide, the storm caused $5.25 million in crop damage, largely to corn and tobacco. Damage in the state was estimated at $17.5 million, and there were 15 deaths. After the storm, about 350 people helped clear debris from the streets of Norfolk.

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answer: Yes

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answer: No

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answer: 1

text: Olaf formed from a tropical wave that left the coast of Africa on September 17. Over the next two weeks it moved westbound into the East Pacific Ocean. Initially, the wave was not in an environment conductive for further development. However, on October 2, a low-level circulation was noted on satellite imagery. This circulation quickly became better defined over the next several hours while located 400 miles (645 km) south of Acapulco, Mexico. The next day, Dvorak Classifications, a tool that estimates a tropical cyclone intensity, were placed at 1.5. This is equivalent to winds of around 30 mph (50 km/h). In addition, a ship nearby reported winds of 35 mph (45 km/h). Microwave imagery also indicated that the center was near the associated convection. Based on this, the system was upgraded into a tropical depression.

text: Olaf formed from a tropical wave that left the coast of Africa on September 17. Over the next two weeks it moved westbound into the East Pacific Ocean. Initially, the wave was not in an environment conductive for further development. However, on October 2, a low-level circulation was noted on

text: satellite imagery

text: . This circulation quickly became better defined over the next several hours while located 400 miles (645 km) south of

text: Acapulco

text: , Mexico. The next day, Dvorak Classifications, a tool that estimates a tropical cyclone intensity, were placed at 1.5. This is equivalent to winds of around 30 mph (50 km/h). In addition, a ship nearby reported winds of 35 mph (45 km/h). Microwave imagery also indicated that the center was near the associated convection. Based on this, the system was upgraded into a tropical depression.

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answer: Yes

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text: Rough seas killed a person on a Navy Destroyer the USS Goldsborough DDG-20 in Pearl Harbor when the seaman hit a stanchion, with four others injured on the ship. One of the four injured was swept overboard two miles (three kilometers) from the harbor. Before the arrival of the hurricane, around 1,000 evacuated the low-lying coastline to shelters.Rough waves destroyed four and damaged two deep-water communication cables between Oahu and Kauai. In Oahu, damage from wind and surf was heaviest on the southwest coast between Nānākuli and Mākaha. The storm surge washed sand into streets in Waikīkī and flooded cars in areas of basement parking. Wind damage was greatest in areas where winds blew from southerly directions off of mountains. The winds damaged several small aircraft and a Douglas DC-3 plane in Honolulu. Gusty winds shattered glass windows in the Honolulu International Airport, injuring several passengers. Some flights in and out of the Honolulu airport were delayed, while other domestic airports were temporarily closed. The passage of the hurricane damaged at least 6,391 homes, 21 hotels, and two condominium buildings on the island. Additionally, 418 buildings, including 30 businesses, were destroyed on Oahu.

text: Rough seas killed a person on a Navy Destroyer the USS Goldsborough DDG-20 in

text: Pearl Harbor

text: when the seaman hit a

text: stanchion

text: , with four others injured on the ship. One of the four injured was swept overboard two miles (three kilometers) from the harbor. Before the arrival of the hurricane, around 1,000 evacuated the low-lying coastline to shelters.Rough waves destroyed four and damaged two

text: deep-water communication cables

text: between Oahu and Kauai. In

text: Oahu

text: , damage from wind and surf was heaviest on the southwest coast between

text: Nānākuli

text: and

text: Mākaha

text: . The storm surge washed sand into streets in

text: Waikīkī

text: and flooded cars in areas of basement parking. Wind damage was greatest in areas where winds blew from southerly directions off of mountains. The winds damaged several small aircraft and a

text: Douglas DC-3

text: plane in

text: Honolulu

text: . Gusty winds shattered glass windows in the

text: Honolulu International Airport

text: , injuring several passengers. Some flights in and out of the Honolulu airport were delayed, while other domestic airports were temporarily closed. The passage of the hurricane damaged at least 6,391 homes, 21 hotels, and two condominium buildings on the island. Additionally, 418 buildings, including 30 businesses, were destroyed on Oahu.

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answers: Rough waves

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answers: the bottle bobs

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: 1

text: Erris has considerable potential for ocean energy in terms of its location next to the Atlantic Ocean and constant winds from the sea. These resources have been earmarked for development. There are opportunities for the development of ocean wave power projects, tidal power, hydroelectric schemes, and, wind farms amongst other clean, alternative energy generation opportunities for which the area is eminently suitable.

text: Erris has considerable potential for ocean energy in terms of its location next to the

text: Atlantic Ocean

text: and constant winds from the sea. These resources have been earmarked for development. There are opportunities for the development of ocean

text: wave power

text: projects,

text: tidal power

text: hydroelectric

text: schemes, and,

text: wind farms

text: amongst other clean, alternative energy generation opportunities for which the area is eminently suitable.

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text: In Surigao City,  of rainfall was recorded, much of which fell in under 12 hours. Storm surges were also recorded in many places. In the island of Leyte and Samar, PAGASA measured 5–6 meter (15–19 ft) waves. In Tacloban, Leyte, the terminal building of Tacloban Airport was destroyed by a  storm surge up to the height of the second story. Along the airport, a storm surge of  was estimated. Waves of  were also estimated. On the western coast of Samar, the storm surge was not as significant.

text: In

text: Surigao City

text: ,  of rainfall was recorded, much of which fell in under 12 hours.

text: Storm surge

text: s were also recorded in many places. In the island of

text: Leyte

text: and

text: Samar

text: PAGASA

text: measured 5–6 meter (15–19 ft) waves. In

text: Tacloban

text: Leyte

text: , the terminal building of

text: Tacloban Airport

text: was destroyed by a  storm surge up to the height of the second story. Along the airport, a storm surge of  was estimated. Waves of  were also estimated. On the western coast of Samar, the storm surge was not as significant.

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answers: up to the height of the second story

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answers: Storm surge

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answers: 5–6 meter

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text: The storm caused flooding in seven counties within the state as a result of  of rainfall. Winds peaked at  which downed trees and power lines, and left 65,000 homes without power. A storm surge of  to  was reported, along with moderate waves that caused minor beach erosion. No deaths are attributed to the storm.

text: The storm caused flooding in seven counties within the state as a result of  of rainfall. Winds peaked at  which downed trees and power lines, and left 65,000 homes without power. A storm surge of  to  was reported, along with moderate waves that caused minor beach erosion. No deaths are attributed to the storm.

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answers: waves that caused minor beach erosion

answer: Yes

answer: Yes

answer: Yes

answer: Yes

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answer: 1

text: In South Florida, Sandy lashed the area with rough surf, strong winds, and brief squalls. Along the coast of Miami-Dade County, waves reached , but may have been as high as  in Palm Beach County. In the former county, minor pounding occurred on  few coastal roads. Further north in Broward County, State Road A1A was inundated with sand and water, causing more than a  stretch of the road to be closed for the entire weekend. Additionally, coastal flooding extended inland up to 2 blocks in some locations and a few houses in the area suffered water damage. In Manalapan, which is located in southern Palm Beach County, several beachfront homes were threatened by erosion. The Lake Worth Pier was also damaged by rough seas. In Palm Beach County alone, losses reached $14 million. Sandy caused closures and cancellations of some activities at schools in Palm Beach, Broward and Miami-Dade counties. Storm surge from Sandy also caused flooding and beach erosion along coastal areas in South Florida. Gusty winds also impacted South Florida, peaking at  in Jupiter and Fowey Rocks Light, which is near Key Biscayne. The storm left power outages across the region, which left many traffic lights out of order.

text: In South Florida, Sandy lashed the area with rough surf, strong winds, and brief squalls. Along the coast of

text: Miami-Dade County

text: , waves reached , but may have been as high as  in

text: Palm Beach County

text: . In the former county, minor pounding occurred on  few coastal roads. Further north in

text: Broward County

text: State Road A1A

text: was inundated with sand and water, causing more than a  stretch of the road to be closed for the entire weekend. Additionally, coastal flooding extended inland up to 2 blocks in some locations and a few houses in the area suffered water damage. In

text: Manalapan

text: , which is located in southern Palm Beach County, several beachfront homes were threatened by erosion. The

text: Lake Worth

text: Pier was also damaged by rough seas. In Palm Beach County alone, losses reached $14 million. Sandy caused closures and cancellations of some activities at schools in

text: Palm Beach

text: Broward

text: and

text: Miami-Dade

text: counties. Storm surge from Sandy also caused flooding and beach erosion along coastal areas in South Florida. Gusty winds also impacted South Florida, peaking at  in

text: Jupiter

text: and

text: Fowey Rocks Light

text: , which is near

text: Key Biscayne

text: . The storm left power outages across the region, which left many traffic lights out of order.

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answers: rough seas

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: Yes

answer: 1

text: At the onset of the design process is a detailed analysis of the existing data of natural weather conditions of the site location, optimizing the use of natural elements to shape the design of the building—the same “thinking model” used by nature. In the same manner that a sailboat is designed to take advantage of the wind and waves, Nati espouses the idea that a building should adhere to the same concept, by optimizing the natural elements to create an efficient and high performing building design.

text: At the onset of the design process is a detailed analysis of the existing data of natural weather conditions of the site location, optimizing the use of natural elements to shape the design of the building—the same “thinking model” used by nature. In the same manner that a sailboat is designed to take advantage of the wind and waves, Nati espouses the idea that a building should adhere to the same concept, by optimizing the natural elements to create an efficient and high performing building design.

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answers: a sailboat

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answers: NDQ_006461

answers: the same “thinking model” used by nature

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: 1

text: The Tropical Rainfall Measuring Mission satellite, jointly operated by NASA and JAXA, estimated that Bijli produced a maximum of  of rain over coastal Bangladesh, with rainfall rates reaching nearly 50 mm/h (2 in/h). High winds downed several trees; numerous homes sustained damage and several ships on offshore islands were reportedly caught in the storm. High winds and heavy rains have also knocked out power to some communities. A storm surge of  was recorded in the Cox's Bazar District with reports higher amounts in localized areas. At least 12 huts, 50 betel beef fields, and a large amount of salt have been damaged by the storm. Later reports indicated that thousands of homes have been damaged or destroyed by the storm. The first fatality caused by Bijli occurred when a tree knocked down by high winds fell on a 9-year-old boy, killing him on impact and injuring his sister. In the Cox's Bazar District, a school teacher and two students were killed. One of the two children was trampled to death during the evacuation. The other child was killed when his home collapsed on top of him.

text: The

text: Tropical Rainfall Measuring Mission

text: satellite, jointly operated by

text: NASA

text: and

text: JAXA

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answers: storm surge

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answers: fast

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answers: High winds downed several trees

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answers: A storm surge

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answers: storm surge

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answers: A storm surge

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answer: Yes

answer: Yes

answer: No

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answer: 1

text: Breaking of water surface waves may occur anywhere that the amplitude is sufficient, including in mid-ocean.  However, it is particularly common on beaches because wave heights are amplified in the region of shallower water (because the group velocity is lower there).  See also waves and shallow water.

text: Breaking of water surface waves may occur anywhere that the amplitude is sufficient, including in mid-ocean.  However, it is particularly common on beaches because wave heights are amplified in the region of shallower water (because the group velocity is lower there).  See also

text: waves and shallow water

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answers: Breaking of water surface waves

answers: NDQ_006453

answers: shallower water

answers: NDQ_006455

answers: the amplitude is sufficient

answers: NDQ_006456

answers: group

answers: NDQ_006457

answers: shallower water

answers: NDQ_006458

answers: shallower water

answers: NDQ_006459

answers: shallower water

answers: NDQ_006460

answers: beaches

answers: NDQ_006461

answers: because the group velocity is lower

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Upon making landfall on Cape May, New Jersey, the cyclone produced a 5 foot (1.5 m) storm surge on the Delaware Bay side of the city. Lasting for several hours, the hurricane-force winds were described as "[blowing] with great violence", causing widespread devastation across the region. In Little Egg Harbor, its passage caused damage to the port. Strong winds reached as far inland as Philadelphia, Pennsylvania, where winds of over 40 mph (60 km/h) downed trees and chimneys; in the city, precipitation accrued to 3.92 inches (99.6 mm). Further to the north, the hurricane destroyed a windmill at Bergen Point, New Jersey. Though the hurricane struck at low tide, it produced a storm surge of over 29 feet (9 m) along several portions of the New Jersey coastline, causing significant overwash.

text: Upon making landfall on

text: Cape May, New Jersey

text: , the cyclone produced a 5 foot (1.5 m) storm surge on the

text: Delaware Bay

text: side of the city. Lasting for several hours, the hurricane-force winds were described as "[blowing] with great violence", causing widespread devastation across the region. In

text: Little Egg Harbor

text: , its passage caused damage to the port. Strong winds reached as far inland as

text: Philadelphia, Pennsylvania

text: , where winds of over 40 mph (60 km/h) downed trees and chimneys; in the city, precipitation accrued to 3.92 inches (99.6 mm). Further to the north, the hurricane destroyed a windmill at

text: Bergen Point, New Jersey

text: . Though the hurricane struck at low tide, it produced a storm surge of over 29 feet (9 m) along several portions of the New Jersey coastline, causing significant

text: overwash

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text: Hurricane Iris moved ashore in Belize with winds of , although the highest measured winds were  at a station in Big Creek. Because of its small diameter, Iris produced heavy damage only in a  area of southern Belize. In that region, the hurricane produced a storm surge of up to , with waves of over  in height, causing street flooding and some damage to the offshore cayes.

text: Hurricane Iris moved ashore in Belize with winds of , although the highest measured winds were  at a station in Big Creek. Because of its small diameter, Iris produced heavy damage only in a  area of southern Belize. In that region, the hurricane produced a

text: storm surge

text: of up to , with waves of over  in height, causing street flooding and some damage to the offshore cayes.

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text: The sea off Cape Agulhas is notorious for winter storms and mammoth rogue waves, which can range up to 30 metres (100 ft) high and can sink even large ships. Over the past few hundred years it has been believed that around 150 ships have sunk around Agulhas. These conditions are caused by a number of factors. The naturally strong winds of the roaring forties, which blow from west to east, and the cold Antarctic Circumpolar Current flowing in the same direction, come up against the warmer Agulhas Current in the region of the cape. These conflicting currents of water of different densities, and the west winds blowing against the Agulhas Current, can create extremely hazardous wave conditions; these are further exacerbated by the shallow waters of the Agulhas Bank, a broad, shallow part of the continental shelf which juts 250 kilometres (155 mi) south from the cape, after which it falls steeply away to the abyssal plain.

text: The sea off Cape Agulhas is notorious for winter storms and mammoth

text: rogue wave

text: s, which can range up to 30 metres (100 ft) high and can sink even large ships. Over the past few hundred years it has been believed that around 150 ships have sunk around Agulhas. These conditions are caused by a number of factors. The naturally strong winds of the

text: roaring forties

text: , which blow from west to east, and the cold

text: Antarctic Circumpolar Current

text: flowing in the same direction, come up against the warmer

text: Agulhas Current

text: in the region of the cape. These conflicting currents of water of different densities, and the west winds blowing against the Agulhas Current, can create extremely hazardous wave conditions; these are further exacerbated by the shallow waters of the

text: Agulhas Bank

text: , a broad, shallow part of the

text: continental shelf

text: which juts 250 kilometres (155 mi) south from the cape, after which it falls steeply away to the

text: abyssal plain

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answers: rogue waves

answers: NDQ_006453

answers: rogue waves

answers: NDQ_006455

answers: conflicting currents of water of different densities, and the west winds blowing against the Agulhas Current

answers: NDQ_006456

answers: currents

answers: NDQ_006457

answers: Mammoth rogue waves

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answers: rogue waves

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answers: conflicting currents of water

answers: NDQ_006460

answers: Cape

answers: NDQ_006461

answers: water of different densities

answer: Yes

answer: Yes

answer: No

answer: Yes

answer: No

answer: 1

text: The powerful cyclone brought intense winds, heavy rainfall, and high waves to Andhra Pradesh in eastern India. Hurricane-force winds – at least 120 km/h (75 mi) – penetrated 100 km (60 mi) inland. Peak gusts were estimated at 200 km/h (124 mph), based on anemometers that were blown away in Yanam. The highest recorded sustained wind was 111 km/h (69 mph) by a ship at the Kakinada Port, only 50 km (30 mi) from the landfall location. The storm dropped heavy rainfall near the coast, peaking at  in Amalapuram. Rainfall rates of over  occurred over 3 hours in a 40 km (25 mi) stretch of land. Along a 60 km (37 mi) portion of the coast,  waves accompanied a  storm surge, spreading 5 km (3 mi) inland. The storm struck just three weeks after another storm killed 350 people. Storm damage extended 130 km (80 mi) inland. Widespread areas of crop fields were inundated with floodwaters, washing away tons of rice, coconuts, and bananas. The winds knocked down about 5 million coconut trees. It was estimated that the storm destroyed  of rice paddy, along with  of other crops. About 13,500 livestock and 1 million chickens were killed by the storm; many of them rotted on arable fields after the waters receded.

text: The powerful cyclone brought intense winds, heavy rainfall, and high waves to Andhra Pradesh in eastern India. Hurricane-force winds – at least 120 km/h (75 mi) – penetrated 100 km (60 mi) inland. Peak gusts were estimated at 200 km/h (124 mph), based on

text: anemometer

text: s that were blown away in

text: Yanam

text: . The highest recorded sustained wind was 111 km/h (69 mph) by a ship at the

text: Kakinada Port

text: , only 50 km (30 mi) from the landfall location. The storm dropped heavy rainfall near the coast, peaking at  in

text: Amalapuram

text: . Rainfall rates of over  occurred over 3 hours in a 40 km (25 mi) stretch of land. Along a 60 km (37 mi) portion of the coast,  waves accompanied a

text: storm surge

text: , spreading 5 km (3 mi) inland. The storm struck just three weeks after another storm killed 350 people. Storm damage extended 130 km (80 mi) inland. Widespread areas of crop fields were inundated with floodwaters, washing away tons of rice, coconuts, and bananas. The winds knocked down about 5 million coconut trees. It was estimated that the storm destroyed  of rice paddy, along with  of other crops. About 13,500 livestock and 1 million chickens were killed by the storm; many of them rotted on arable fields after the waters receded.

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answers: high waves

answers: NDQ_006453

answers: storm surge

answers: NDQ_006455

answers: cyclone

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answers: fast

answers: NDQ_006457

answers: Waves accompanied a storm surge

answers: NDQ_006458

answers: High waves

answers: NDQ_006459

answers: cyclone

answers: NDQ_006460

answers: landfall

answers: NDQ_006461

answers: high waves

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: 1

text: 2) starts from "wind shear forces" on the water surface (J.W.Miles, applied to mainly 2D deep water gravity waves) ; John W. Miles suggested a surface wave generation mechanism which is initiated by turbulent wind shear flows Ua(y), based on the inviscid Orr-Sommerfeld equation in 1957. He found the energy transfer from wind to water surface as a wave speed, c is proportional to the curvature of the velocity profile of wind Ua’’(y) at point where the mean wind speed is equal to the wave speed (Ua=c, where, Ua is the Mean turbulent wind speed). Since the wind profile Ua(y) is logarithmic to the water surface, the curvature Ua’’(y) have negative sign at the point of Ua=c. This relations show the wind flow transferring its kinetic energy to the water surface at their interface, and arises wave speed, c.

text: 2) starts from "wind shear forces" on the water surface (J.W.Miles, applied to mainly 2D deep water gravity waves) ; John W. Miles suggested a surface wave generation mechanism which is initiated by turbulent wind shear flows Ua(y), based on the inviscid Orr-Sommerfeld equation in 1957. He found the energy transfer from wind to water surface as a wave speed, c is proportional to the curvature of the velocity profile of wind Ua’’(y) at point where the mean wind speed is equal to the wave speed (Ua=c, where, Ua is the Mean turbulent wind speed). Since the wind profile Ua(y) is logarithmic to the water surface, the curvature Ua’’(y) have negative sign at the point of Ua=c. This relations show the wind flow transferring its kinetic energy to the water surface at their interface, and arises wave speed, c.

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answers: Waves break when they become too tall to be supported by their base

answers: NDQ_006453

answers: Gravity waves

answers: NDQ_006455

answers: wind shear forces

answers: NDQ_006456

answers: turbulent

answers: NDQ_006457

answers: wave energy is lowest at the surface and increases with depth

answers: NDQ_006458

answers: 2D deep water gravity waves

answers: NDQ_006459

answers: wind shear forces

answers: NDQ_006460

answers: water surface

answers: NDQ_006461

answers: the curvature Ua’’(y) have negative sign

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: Yes

answer: 1

text: The origins of Hurricane Otis are believed to have been in a tropical wave that emerged from the west coast of Africa on September 9. The wave moved westward across the Atlantic Ocean, spawning Tropical Depression Seventeen on September 17. The southern portion of the wave continued westward, crossing into the eastern Pacific Ocean on September 22. As the wave entered a monsoon-like environment, convection increased on September 23. An associated area of disorganized clouds and thunderstorms persisted off the coast of Mexico for several days, although due to wind shear and its proximity to land, short-term tropical cyclone development—if any—was expected to occur slowly. On September 27, it began to show signs of organization; the National Hurricane Center (NHC) remarked upon the potential for a tropical cyclone to develop within the next day. It is estimated that the system became a tropical depression at 0000 UTC on September 28, while located about  to the south of Manzanillo, Mexico.

text: The origins of Hurricane Otis are believed to have been in a

text: tropical wave

text: that emerged from the west coast of

text: Africa

text: on September 9. The wave moved westward across the

text: Atlantic Ocean

text: , spawning

text: Tropical Depression Seventeen

text: on September 17. The southern portion of the wave continued westward, crossing into the eastern

text: Pacific Ocean

text: on September 22. As the wave entered a monsoon-like environment,

text: convection

text: increased on September 23. An associated area of disorganized clouds and thunderstorms persisted off the coast of

text: Mexico

text: for several days, although due to

text: wind shear

text: and its proximity to land, short-term tropical cyclone development—if any—was expected to occur slowly. On September 27, it began to show signs of organization; the

text: National Hurricane Center

text: (NHC) remarked upon the potential for a tropical cyclone to develop within the next day. It is estimated that the system became a tropical depression at 0000 UTC on September 28, while located about  to the south of

text: Manzanillo, Mexico

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answers: 4

answers: NDQ_006461

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answers: NDQ_006452

answers: Tropical Depression Seventeen

answers: NDQ_006453

answers: Tropical depression

answers: NDQ_006455

answers: emerged from the west coast of Africa

answers: NDQ_006456

answers: westward

answers: NDQ_006457

answers: convection increased on September 23

answers: NDQ_006458

answers: tropical wave

answers: NDQ_006459

answers: tropical wave

answers: NDQ_006460

answers: The wave moved westward across the Atlantic Ocean

answers: NDQ_006461

answers: due to wind shear

answer: Yes

answer: Yes

answer: No

answer: No

answer: No

answer: 1

text: After surviving many storms, the Nueces was at last badly damaged by Hurricane Celia on 3 August 1970. Celia was more of a wind storm, with gusts over 200 mph, and did comparatively little damage by tidal surge. The storm knocked down brick walls and flung signs, pieces of metal, wooden timbers, and other debris through the air and sometimes through buildings. Downtown was piled with rubble. The Nueces Hotel was deemed too badly damaged to be worth saving.

text: After surviving many storms, the Nueces was at last badly damaged by

text: Hurricane Celia

text: on 3 August 1970. Celia was more of a

text: wind storm

text: , with gusts over 200 mph, and did comparatively little damage by tidal surge. The storm knocked down brick walls and flung signs, pieces of metal, wooden timbers, and other debris through the air and sometimes through buildings. Downtown was piled with rubble. The Nueces Hotel was deemed too badly damaged to be worth saving.

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answers: Tidal surge

answers: NDQ_006453

answers: Tidal surge

answers: NDQ_006455

answers: hurricane

answers: NDQ_006456

answers: 200 mph

answers: NDQ_006457

answers: tidal surge

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answers: tidal surge

answers: NDQ_006459

answers: wind

answers: NDQ_006460

answers: Tidal surge

answers: NDQ_006461

answers: tidal surge

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: 1

text: Wind causes waves which result in other difficulties. Waves make navigation difficult and dangerous near shallow water. Also, waves create buoyancy stresses on the structure of a hull. The weight of breaking waves on the fabric of the ship force the crew to reduce speed or even travel in the same direction as the waves to prevent damage. Also, wind stresses the rigging of sailing ships.

text: Wind causes

text: wave

text: s which result in other difficulties. Waves make navigation difficult and dangerous near shallow water. Also, waves create buoyancy stresses on the structure of a hull. The weight of breaking waves on the fabric of the ship force the crew to reduce speed or even travel in the same direction as the waves to prevent damage. Also, wind stresses the rigging of sailing ships.

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answers: When they become too tall to be supported by their base

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answers: shallow water

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answers: Wind

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answers: buoyancy

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answers: The weight of breaking waves

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answers: buoyancy stresses

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: 1

text: Although the hurricane never made landfall on Cuba, the storm's close proximity to the northern stretches of the island led to considerable impacts. A strong storm surge combined with wind-swept waves topped the Havana seawall, flooding areas of the city as far as six blocks inland and prompting the evacuation of homes at risk. The inundation also disabled some of Havana's tram systems and halted automotive traffic.

text: Although the hurricane never made landfall on Cuba, the storm's close proximity to the northern stretches of the island led to considerable impacts. A strong

text: storm surge

text: combined with wind-swept waves topped the

text: Havana

text: seawall

text: , flooding areas of the city as far as six blocks inland and prompting the evacuation of homes at risk. The inundation also disabled some of Havana's

text: tram

text: systems and halted automotive traffic.

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answers: A strong storm surge combined with wind-swept waves

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answers: NDQ_006460

answers: landfall

answers: NDQ_006461

answers: strong storm surge combined with wind-swept waves

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: 1

text: The lifeboat has a maximum speed of  and a cruising speed of . Cape-class lifeboats have fuel capacities of  and ranges of  when cruising. Cape Dauphin is capable of operating at wind speeds of  and wave heights of . It can tow ships with displacements of up to  and can withstand  winds and -high breaking waves.

text: The lifeboat has a maximum speed of  and a cruising speed of . Cape-class lifeboats have fuel capacities of  and ranges of  when cruising. Cape Dauphin is capable of operating at wind speeds of  and wave heights of . It can tow ships with

text: displacements

text: of up to  and can withstand  winds and -high breaking waves.

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answer: Yes

answer: Yes

answer: Yes

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text: Throughout Cuba, Hurricane Georges produced torrential rainfall, peaking at 24.41 inches (620 mm) in Limonar in the province of Guantánamo. Several other locations reported over a foot (300 mm) of precipitation as well. Storm surge of 4–6 feet (1–2 m) was expected along the eastern coastline, along with dangerous waves on top of the surge. Though winds were reduced by the time Georges hit Cuba, it still retained winds of 75 mph (120 km/h), along with stronger gusts in squalls. Waves exceeding 16 ft (4.8 m) impacted coastal regions of the county, with some areas reporting that waves were topping the sea wall.

text: Throughout Cuba, Hurricane Georges produced torrential rainfall, peaking at 24.41 inches (620 mm) in Limonar in the province of

text: Guantánamo

text: . Several other locations reported over a foot (300 mm) of precipitation as well. Storm surge of 4–6 feet (1–2 m) was expected along the eastern coastline, along with dangerous waves on top of the surge. Though winds were reduced by the time Georges hit Cuba, it still retained winds of 75 mph (120 km/h), along with stronger gusts in squalls. Waves exceeding 16 ft (4.8 m) impacted coastal regions of the county, with some areas reporting that waves were topping the sea wall.

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text: A curved phasefront may be synthesized from an infinite number of these "natural modes" i.e., from plane wave phasefronts oriented in different directions in space.  Far from its sources, an expanding spherical wave is locally tangent to a planar phase front (a single plane wave out of the infinite spectrum), which is transverse to the radial direction of propagation.  In this case, a Fraunhofer diffraction pattern is created, which emanates from a single spherical wave phase center.  In the near field, no single well-defined spherical wave phase center exists, so the wavefront isn't locally tangent to a spherical ball.  In this case, a Fresnel diffraction pattern would be created, which emanates from an extended source, consisting of a distribution of (physically identifiable) spherical wave sources in space.  In the near field, a full spectrum of plane waves is necessary to represent the Fresnel near-field wave, even locally.  A "wide" wave moving forward (like an expanding ocean wave coming toward the shore) can be regarded as an infinite number of "plane wave modes", all of which could (when they collide with something in the way) scatter independently of one other. These mathematical simplifications and calculations are the realm of Fourier analysis and synthesis – together, they can describe what happens when light passes through various slits, lenses or mirrors curved one way or the other, or is fully or partially reflected. Fourier optics forms much of the theory behind image processing techniques, as well as finding applications where information needs to be extracted from optical sources such as in quantum optics. To put it in a slightly more complex way, similar to the concept of frequency and time used in traditional  Fourier transform theory, Fourier optics makes use of the spatial frequency domain (k, k) as the conjugate of the spatial (x, y) domain. Terms and concepts such as transform theory, spectrum, bandwidth, window functions and sampling from one-dimensional signal processing are commonly used.

text: A curved phasefront may be synthesized from an infinite number of these "natural modes" i.e., from plane wave phasefronts oriented in different directions in space.  Far from its sources, an expanding spherical wave is locally tangent to a planar phase front (a single plane wave out of the infinite spectrum), which is transverse to the radial direction of propagation.  In this case, a

text: Fraunhofer diffraction

text: pattern is created, which emanates from a single spherical wave phase center.  In the near field, no single well-defined spherical wave phase center exists, so the wavefront isn't locally tangent to a spherical ball.  In this case, a

text: Fresnel diffraction

text: pattern would be created, which emanates from an extended source, consisting of a distribution of (physically identifiable) spherical wave sources in space.  In the near field, a full spectrum of plane waves is necessary to represent the Fresnel near-field wave, even locally.  A "wide"

text: wave

text: moving forward (like an expanding ocean wave coming toward the shore) can be regarded as an infinite number of "

text: plane wave modes

text: ", all of which could (when they collide with something in the way) scatter independently of one other. These mathematical simplifications and calculations are the realm of

text: Fourier analysis and synthesis

text: – together, they can describe what happens when light passes through various slits, lenses or mirrors curved one way or the other, or is fully or partially reflected. Fourier optics forms much of the theory behind

text: image processing techniques

text: , as well as finding applications where information needs to be extracted from optical sources such as in

text: quantum optics

text: . To put it in a slightly more complex way, similar to the concept of

text: frequency

text: and

text: time

text: used in traditional

text: Fourier transform theory

text: , Fourier optics makes use of the

text: spatial frequency

text: domain (k, k) as the conjugate of the spatial (x, y) domain. Terms and concepts such as transform theory, spectrum, bandwidth, window functions and sampling from one-dimensional

text: signal processing

text: are commonly used.

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answers: Fourier optics forms much of the theory behind image processing techniques

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answers: Fresnel diffraction pattern

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: As the strong wind passed over the North Sea, a storm surge was recorded all along the east coast of the United Kingdom on 3 January, advancing from the northern North Sea, water levels in the north of England rose higher than those of the North Sea flood of 1953, although they were lower in the south. The storm surge was far more severe on the north German coast reaching levels never previously recorded, reaching 6.45 m above mean sea level at Hamburg (4.5 m above mean high water levels). Fortunately dykes had been raised after the devastating North Sea flood of 1962 which was 0.85m lower.

text: As the strong wind passed over the North Sea, a storm surge was recorded all along the east coast of the United Kingdom on 3 January, advancing from the northern North Sea, water levels in the north of England rose higher than those of the

text: North Sea flood of 1953

text: , although they were lower in the south. The storm surge was far more severe on the north German coast reaching levels never previously recorded, reaching 6.45 m above mean sea level at Hamburg (4.5 m above mean high water levels). Fortunately dykes had been raised after the devastating

text: North Sea flood of 1962

text: which was 0.85m lower.

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answers: 6.45 m above mean sea level

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answer: No

answer: No

answer: Yes

answer: No

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answer: 1

text: This wave pattern occurs often in nature, including ocean waves, sound waves, and light waves.

text: This

text: wave

text: pattern occurs often in nature, including

text: ocean waves

text: sound

text: waves, and

text: light

text: waves.

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answers: this wave pattern occurs often

answer: No

answer: No

answer: No

answer: No

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answer: 1

text: In fluid dynamics, wind waves, or wind-generated waves, are surface waves that occur on the free surface of oceans, seas, lakes, rivers, and canals or even on small puddles and ponds. They result from the wind blowing over an area of fluid surface. Waves in the oceans can travel thousands of miles before reaching land. Wind waves range in size from small ripples, to waves over  high.

text: In

text: fluid dynamics

text: , wind waves, or wind-generated waves, are

text: surface wave

text: s that occur on the

text: free surface

text: of

text: ocean

text: s,

text: sea

text: s,

text: lake

text: s,

text: river

text: s, and

text: canal

text: s or even on small

text: puddle

text: s and

text: pond

text: s. They result from the

text: wind

text: blowing over an area of fluid surface. Waves in the oceans can travel thousands of miles before reaching land. Wind waves range in size from small

text: ripples

text: , to waves over  high.

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answers: high

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answers: puddles

answers: NDQ_006455

answers: the wind blowing over an area of fluid surface

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answers: high

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answers: surface waves

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answers: They result from the wind blowing over an area of fluid surface

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answers: high

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answers: Waves in the oceans

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answers: surface waves

answer: Yes

answer: Yes

answer: Yes

answer: Yes

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answer: 2

text: Research on the origin of seismic noise indicates that the low frequency part of the spectrum (below 1 Hz) is due to natural causes, chiefly ocean waves. In particular the peak between 0.1 and 0.3 Hz is clearly associated with the interaction of water waves of nearly equal frequencies but opposite directions. At high frequency (above 1 Hz), seismic noise is mainly produced by human activities such as road traffic and industrial work; but there are also natural sources, like rivers. Around 1 Hz, wind and other atmospheric phenomena are also a major source of ground vibrations.

text: Research on the origin of seismic noise indicates that the low frequency part of the

text: spectrum

text: (below 1 Hz) is due to natural causes, chiefly

text: ocean wave

text: s. In particular the peak between 0.1 and 0.3 Hz is clearly associated with the interaction of water waves of nearly equal frequencies but opposite directions. At high frequency (above 1 Hz), seismic noise is mainly produced by human activities such as road traffic and industrial work; but there are also natural sources, like rivers. Around 1 Hz, wind and other atmospheric phenomena are also a major source of ground vibrations.

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answers: ground vibrations

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answers: ocean waves

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answers: ocean waves

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answers: opposite directions

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answers: NDQ_006458

answers: interaction of water waves

answers: NDQ_006459

answers: ocean waves

answers: NDQ_006460

answers: ocean waves

answers: NDQ_006461

answers: interaction of water waves

answer: Yes

answer: Yes

answer: No

answer: Yes

answer: No

answer: 1

text: The highest storm tide noted in historical accounts was produced by the 1899 Cyclone Mahina, estimated at almost 44 ft (13 metres) at Bathurst Bay, Australia, but research published in 2000 saw the majority of this was likely wave run-up, due to the steep coastal topography. In the United States, one of the greatest recorded storm surges was generated by 2005's Hurricane Katrina, which produced a maximum storm surge of more than 25 ft (8 metres) in the communities of Waveland (41.5 ft), Bay St. Louis (38 ft), Diamondhead (30 ft) and Pass Christian (35 ft) in Mississippi. Another record storm surge occurred in this same area from Hurricane Camille in August 1969, with the highest storm tide of record noted from a high water mark as 24.6 ft (7.5 m), also found in Pass Christian (the back side of St. Louis Bay got up to 35 ft). A high storm surge occurred in New York City from Hurricane Sandy in October 2012, with a high tide of 14 ft (4.2 m).

text: The highest storm tide noted in historical accounts was produced by the 1899

text: Cyclone Mahina

text: , estimated at almost 44 ft (13 metres) at

text: Bathurst Bay

text: Australia

text: , but research published in 2000 saw the majority of this was likely wave run-up, due to the steep coastal topography. In the

text: United States

text: , one of the greatest recorded storm surges was generated by 2005's

text: Hurricane Katrina

text: , which produced a maximum storm surge of more than 25 ft (8 metres) in the communities of

text: Waveland

text: (41.5 ft),

text: Bay St. Louis

text: (38 ft),

text: Diamondhead

text: (30 ft) and

text: Pass Christian

text: (35 ft) in

text: Mississippi

text: . Another record storm surge occurred in this same area from

text: Hurricane Camille

text: in August 1969, with the highest storm tide of record noted from a high water mark as 24.6 ft (7.5 m), also found in Pass Christian (the back side of

text: St. Louis Bay

text: got up to 35 ft). A high storm surge occurred in

text: New York City

text: from

text: Hurricane Sandy

text: in October 2012, with a high tide of 14 ft (4.2 m).

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answers: high tide

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answers: fast

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answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: A prophylactic method introduced after the North Sea Flood of 1953 is the construction of dams and floodgates (storm surge barriers). They are open and allow free passage but close when the land is under threat of a storm surge. Major storm surge barriers are the Oosterscheldekering and Maeslantkering in the Netherlands which are part of the Delta Works project, the Thames Barrier protecting London and the Saint Petersburg Dam in Russia.

text: A prophylactic method introduced after the

text: North Sea Flood of 1953

text: is the construction of dams and

text: floodgate

text: s (storm surge barriers). They are open and allow free passage but close when the land is under threat of a storm surge. Major storm surge barriers are the

text: Oosterscheldekering

text: and

text: Maeslantkering

text: in the Netherlands which are part of the

text: Delta Works

text: project, the

text: Thames Barrier

text: protecting

text: London

text: and the

text: Saint Petersburg Dam

text: in Russia.

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answers: They are open and allow free passage

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Certain basic factors he pointed out are still relevant today. A point winding is almost two dimensional, rather like the spring of a watch spiral. A root winding is three-dimensional rather like a spiral staircase, more properly a helix. Thus point winding tends to produce more of a curl, but both produce waved hair when pulled slightly. Point produces a thicker winding and so heat takes longer to penetrate the core of the winding. Root winding is heated over a greater length and the thickness of the winding will depend on the overlap between turns.

text: Certain basic factors he pointed out are still relevant today. A point winding is almost two dimensional, rather like the spring of a watch

text: spiral

text: . A root winding is three-dimensional rather like a spiral staircase, more properly a

text: helix

text: . Thus point winding tends to produce more of a curl, but both produce waved hair when pulled slightly. Point produces a thicker winding and so heat takes longer to penetrate the core of the winding. Root winding is heated over a greater length and the thickness of the winding will depend on the overlap between turns.

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answers: point winding

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answers: point winding

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answers: when pulled slightly

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answers: waved

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answers: Heat takes longer to penetrate the core of the winding

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answers: Point produces a thicker winding

answers: NDQ_006459

answers: point winding

answers: NDQ_006460

answers: point winding

answers: NDQ_006461

answers: point winding is almost two dimensional

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: 1

text: Ocean waves are defined as a collection of dislocated water parcels that undergo a cycle of being forced past their normal position and being restored back to their normal position. Wind caused ripples and eddies form waves that gradually gain speed and distance (fetch). Waves increase in energy and speed, and then become longer and stronger. The fully developed sea has the strongest wave action that experiences storms lasting 10-hours and creates 15 meter wave heights  in the open ocean.

text: Ocean wave

text: s are defined as a collection of dislocated water parcels that undergo a cycle of being forced past their normal position and being restored back to their normal position. Wind caused ripples and eddies form waves that gradually gain speed and distance (fetch). Waves increase in energy and speed, and then become longer and stronger. The fully developed sea has the strongest wave action that experiences storms lasting 10-hours and creates 15 meter wave heights  in the open ocean.

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answers: 15 meter

answers: NDQ_006453

answers: eddies

answers: NDQ_006455

answers: Wind

answers: NDQ_006456

answers: dislocated

answers: NDQ_006457

answers: surface

answers: NDQ_006458

answers: Waves increase in energy

answers: NDQ_006459

answers: fully developed sea

answers: NDQ_006460

answers: shoreline

answers: NDQ_006461

answers: normal position and being restored back to their normal position

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: 1

text: Wave power involves converting the energy in ocean surface waves into electricity using devices either fixed to the shore, the seabed or floating out at sea. Wave energy varies with time, depending on when and where the winds and storms that drive the waves occur. Tidal energy is more regular and predictable.

text: Wave power

text: involves converting the energy in

text: ocean surface wave

text: s into electricity using devices either fixed to the shore, the seabed or floating out at sea. Wave energy varies with time, depending on when and where the winds and storms that drive the waves occur. Tidal energy is more regular and predictable.

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answers: NDQ_006452

answers: Tidal energy

answers: NDQ_006453

answers: Tidal

answers: NDQ_006455

answers: winds and storms

answers: NDQ_006456

answers: the seabed

answers: NDQ_006457

answers: the seabed

answers: NDQ_006458

answers: Tidal energy

answers: NDQ_006459

answers: storms

answers: NDQ_006460

answers: shore

answers: NDQ_006461

answers: Tidal energy

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: No

answer: 1

text: The island is a low, flat, sandy cay, 240m by 90m, and is subject to erosion. It changes its shape seasonally. The sand build up depends largely on the direction of prevailing winds and waves; it has taken an elongated shape for some years, the shape of a crescent moon for a few years, and the shape of a letter "S". Like Lankiam Cay, it is also barren of any vegetation. No underground water source has been found in the area.

text: The island is a low, flat, sandy

text: cay

text: , 240m by 90m, and is subject to erosion. It changes its shape seasonally. The sand build up depends largely on the direction of prevailing winds and waves; it has taken an elongated shape for some years, the shape of a crescent moon for a few years, and the shape of a letter "S". Like

text: Lankiam Cay

text: , it is also barren of any vegetation. No underground water source has been found in the area.

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answers: It changes its shape seasonally

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answers: direction of prevailing winds

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answers: depends largely on the direction of prevailing winds

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: 1

text: Strong winds from Isabel extended from North Carolina to New England and westward to West Virginia. The winds, combined with previous rainfall which moistened the soil, downed many trees and power lines across its path, leaving about 6 million electricity customers without power at some point. Coastal areas suffered from waves and its powerful storm surge, with areas in eastern North Carolina and southeast Virginia reporting severe damage from both winds and the storm surge. Throughout its path, Isabel resulted in $3.6 billion in damage (2003 USD; $

text: Strong winds from Isabel extended from

text: North Carolina

text: to

text: New England

text: and westward to

text: West Virginia

text: . The winds, combined with previous rainfall which moistened the soil, downed many trees and power lines across its path, leaving about 6 million electricity customers without power at some point. Coastal areas suffered from waves and its powerful storm surge, with areas in eastern North Carolina and southeast

text: Virginia

text: reporting severe damage from both winds and the storm surge. Throughout its path, Isabel resulted in $3.6 billion in damage (2003 USD; $

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answers: Strong winds from Isabel

answers: NDQ_006453

answers: Storm surge

answers: NDQ_006455

answers: Strong winds

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answers: fast

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answers: Surface wave energy is lowest at the surface

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answers: Strong winds

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answers: Coastal areas

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answers: waves and its powerful storm surge

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: 1

text: A tropical wave that is associated with the formation of Hillary, moved off Western Africa on August 4. The wave initially had a large area of deep convention, but the convention quickly diminished as the system moved across the eastern portion of the tropical Atlantic Ocean. The wave continued westward without much development or organization, and crossed northern South America and then entered the northern Pacific Ocean on August 17. Mid-level circulation and convention organized with the wave, as it was south of Guatemala on August 18. The system's organization persisted, but without defining a well-established center of circulation, at the surface.Tropical Depression Eight-E finally formed from the area of disturbed weather south of the Gulf of Tehuantepec,  south of Puerto Angel, Mexico, on August 19. It strengthened to a tropical storm late that evening, and reached hurricane strength 24 hours later. Moving parallel to the Mexican coast and about  off-shore, it reached Category 2 on the Saffir-Simpson Hurricane Scale late on August 21. Tropical storm  winds affected the coast and a tropical storm warning was issued for a while. Hilary dissipated not long after weakening to a tropical storm on August 25.

text: A tropical wave that is associated with the formation of Hillary, moved off Western Africa on August 4. The wave initially had a large area of deep convention, but the convention quickly diminished as the system moved across the eastern portion of the tropical Atlantic Ocean. The wave continued westward without much development or organization, and crossed northern South America and then entered the northern Pacific Ocean on August 17. Mid-level circulation and convention organized with the wave, as it was south of

text: Guatemala

text: on August 18. The system's organization persisted, but without defining a well-established center of circulation, at the surface.Tropical Depression Eight-E finally formed from the area of disturbed weather south of the

text: Gulf of Tehuantepec

text: ,  south of

text: Puerto Angel

text: , Mexico, on August 19. It strengthened to a tropical storm late that evening, and reached hurricane strength 24 hours later. Moving parallel to the

text: Mexican

text: coast and about  off-shore, it reached Category 2 on the

text: Saffir-Simpson Hurricane Scale

text: late on August 21. Tropical storm  winds affected the coast and a

text: tropical storm warning

text: was issued for a while. Hilary dissipated not long after weakening to a tropical storm on August 25.

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answers: Category 2

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answers: tropical wave

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answers: tropical Atlantic Ocean

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answers: mid-level

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answers: Mid-level circulation

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answers: The convention quickly diminished as the system moved across the eastern portion of the tropical Atlantic Ocean

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answers: It moved parallel to the Mexican coast

answers: NDQ_006461

answers: Mid-level circulation and convention organized

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: In fluid dynamics, the wave height of a surface wave is the difference between the elevations of a crest and a neighbouring trough. Wave height is a term used by mariners, as well as in coastal, ocean and naval engineering.

text: In

text: fluid dynamics

text: , the wave height of a

text: surface wave

text: is the difference between the

text: elevation

text: s of a

text: crest

text: and a neighbouring

text: trough

text: . Wave height is a term used by

text: mariner

text: s, as well as in

text: coastal

text: ocean

text: and

text: naval engineering

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answers: crest

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answers: crest

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answers: crest

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answers: fluid

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answers: Wave height

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answers: crest

answers: NDQ_006460

answers: shoreline

answers: NDQ_006461

answers: crest and a neighbouring trough

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: without being actively constraint by the boundary conditions at the two extremes of the string. The shape of the wave is constant, i.e. the curve is indeed of the form f(x−ct).

text: without being actively constraint by the boundary conditions at the two extremes of the string. The shape of the wave is constant, i.e. the curve is indeed of the form f(x−ct).

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answers: The shape of the wave is constant

answer: No

answer: No

answer: Yes

answer: No

answer: No

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text: Wind waves, as their name suggests, are generated by wind transferring energy from the atmosphere to the ocean's surface, and capillary-gravity waves play an essential role in this effect. There are two distinct mechanisms involved, called after their proponents, Phillips and Miles.

text: Wind waves, as their name suggests, are generated by wind transferring energy from the atmosphere to the ocean's surface, and

text: capillary-gravity waves

text: play an essential role in this effect. There are two distinct mechanisms involved, called after their proponents, Phillips and Miles.

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answers: capillary

answers: NDQ_006453

answers: Wind waves

answers: NDQ_006455

answers: wind transferring energy

answers: NDQ_006456

answers: gravity

answers: NDQ_006457

answers: surface

answers: NDQ_006458

answers: Gravity waves

answers: NDQ_006459

answers: wind

answers: NDQ_006460

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answers: NDQ_006461

answers: gravity

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: 2

text: Why couldn’t we just use a shorter runner so the delay is not so great? The answer lies at the end of the cycle when that big long runner now continues to flow at full speed disregarding the rising pressure in the cylinder and providing pressure to the cylinder when it is needed most. The runner length also controls the timing of the returning waves and cannot be altered. A shorter runner would flow earlier but also would die earlier while returning the positive waves much too quickly and those waves would be weaker. The key is to find the optimum balance of all the factors for the engine requirements.

text: Why couldn’t we just use a shorter runner so the delay is not so great? The answer lies at the end of the cycle when that big long runner now continues to flow at full speed disregarding the rising pressure in the cylinder and providing pressure to the cylinder when it is needed most. The runner length also controls the timing of the returning waves and cannot be altered. A shorter runner would flow earlier but also would die earlier while returning the positive waves much too quickly and those waves would be weaker. The key is to find the optimum balance of all the factors for the engine requirements.

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answers: The runner length also controls the timing of the returning waves

answers: NDQ_006453

answers: The runner length also controls the timing of the returning waves and cannot be altered

answers: NDQ_006455

answers: at the end of the cycle

answers: NDQ_006456

answers: positive waves

answers: NDQ_006457

answers: Wave energy is lowest at the surface and increases with depth

answers: NDQ_006458

answers: The runner length also controls the timing of the returning waves and cannot be altered

answers: NDQ_006459

answers: a shorter runner

answers: NDQ_006460

answers: The runner length also controls the timing

answers: NDQ_006461

answers: The runner length also controls the timing of the returning waves

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: In Nova Scotia, the high storm surge flooded the Cabot Trail in several locations, and in two cities coastal roads were washed out. Several days of persistent rainfall resulted in house flooding, sinkholes, and sewer backups. In neighboring New Brunswick, high winds left about 7,000 people without power along a 60 mi (100 km) portion of the coastline. High seas damaged wharves in Miramichi Bay. In Escuminac, New Brunswick, the surge reached 7.94 ft (2.43 m), just shy of the record set in November 1988. The nor'easter occurred ten months after a similarly powerful storm struck the region. The October storm produced record river flooding from the combination of strong waves and winds, and likewise damaged coastal structures. The provincial government paid about $2.4 million in insurance claims due to the storm.

text: In Nova Scotia, the high storm surge flooded the

text: Cabot Trail

text: in several locations, and in two cities coastal roads were washed out. Several days of persistent rainfall resulted in house flooding, sinkholes, and sewer backups. In neighboring New Brunswick, high winds left about 7,000 people without power along a 60 mi (100 km) portion of the coastline. High seas damaged wharves in

text: Miramichi Bay

text: . In

text: Escuminac, New Brunswick

text: , the surge reached 7.94 ft (2.43 m), just shy of the record set in November 1988. The nor'easter occurred ten months after a similarly powerful storm struck the region. The October storm produced record river flooding from the combination of strong waves and winds, and likewise damaged coastal structures. The provincial government paid about $2.4 million in insurance claims due to the storm.

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answer: Yes

answer: Yes

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text: The wind and waves create surface currents (designated as « drift currents »). These currents can decompose in one quasi permanent current (which varies within the hourly scale) and one movement of Stokes drift under the effect of rapid waves movement (at the echelon of a couple of seconds).). The quasi permanent current is accelerated by the breaking of waves, and in a lesser governing effect, by the friction of the wind on the surface.

text: The

text: wind

text: and

text: wave

text: s create surface currents (designated as « drift currents »). These currents can decompose in one quasi permanent current (which varies within the hourly scale) and one movement of

text: Stokes drift

text: under the effect of rapid waves movement (at the echelon of a couple of seconds).). The quasi permanent current is accelerated by the breaking of waves, and in a lesser governing effect, by the friction of the wind on the surface.

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answer: Yes

answer: Yes

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answer: 1

text: This effect operates similarly to the patterns made by sunlight on the bottom of a pool, the difference is that the light is bent at the contact point with the water while the shock wave is distorted by density variations (e.g. due to temperature variations) in the atmosphere. Variations of wind can cause a similar effect. This will disperse the shock wave at some places and focus it at others. For powerful shock waves this can cause damage farther than expected; the shock wave energy density will decrease beyond expected values based on uniform geometry  falloff for weak shock or acoustic waves, as expected at large distances).

text: This effect operates similarly to the patterns made by sunlight on the bottom of a pool, the difference is that the light is bent at the contact point with the water while the shock wave is distorted by

text: density

text: variations (e.g. due to temperature variations) in the atmosphere. Variations of

text: wind

text: can cause a similar effect. This will disperse the shock wave at some places and focus it at others. For powerful shock waves this can cause damage farther than expected; the shock wave energy density will decrease beyond expected values

text: based on uniform geometry

text: falloff for weak shock or acoustic waves, as expected at large distances).

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answers: Shock waves can cause damage farther than expected

answers: NDQ_006453

answers: Shock waves

answers: NDQ_006455

answers: shock wave

answers: NDQ_006456

answers: oscillating

answers: NDQ_006457

answers: This will disperse the shock wave at some places and focus it at others

answers: NDQ_006458

answers: This will disperse the shock wave at some places and focus it at others

answers: NDQ_006459

answers: wind

answers: NDQ_006460

answers: For powerful shock waves this can cause damage farther than expected

answers: NDQ_006461

answers: This will disperse the shock wave at some places and focus it at others

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: 1

text: When the source of the waves is moving towards the observer, each successive wave crest is emitted from a position closer to the observer than the previous wave. Therefore, each wave takes slightly less time to reach the observer than the previous wave. Hence, the time between the arrival of successive wave crests at the observer is reduced, causing an increase in the frequency. While they are travelling, the distance between successive wave fronts is reduced, so the waves "bunch together".  Conversely, if the source of waves is moving away from the observer, each wave is emitted from a position farther from the observer than the previous wave, so the arrival time between successive waves is increased, reducing the frequency. The distance between successive wave fronts is then increased, so the waves "spread out".

text: When the source of the waves is moving towards the observer, each successive wave

text: crest

text: is emitted from a position closer to the observer than the previous wave. Therefore, each wave takes slightly less time to reach the observer than the previous wave. Hence, the time between the arrival of successive wave crests at the observer is reduced, causing an increase in the frequency. While they are travelling, the distance between successive wave fronts is reduced, so the waves "bunch together".  Conversely, if the source of waves is moving away from the observer, each wave is emitted from a position farther from the observer than the previous wave, so the arrival time between successive waves is increased, reducing the frequency. The distance between successive wave fronts is then increased, so the waves "spread out".

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answers: NDQ_006452

answers: The distance between successive wave fronts is reduced, so the waves "bunch together"

answers: NDQ_006453

answers: Bunch together

answers: NDQ_006455

answers: When the source of the waves is moving

answers: NDQ_006456

answers: forward

answers: NDQ_006457

answers: Wave energy is lowest at the surface and increases with depth

answers: NDQ_006458

answers: The distance between successive wave fronts is reduced, so the waves "bunch together"

answers: NDQ_006459

answers: When the source of waves is moving towards the observer

answers: NDQ_006460

answers: Waves travel across the ocean to end up on a shoreline

answers: NDQ_006461

answers: each successive wave crest is emitted from a position closer to the observer than the previous wave

answer: No

answer: No

answer: No

answer: No

answer: Yes

answer: 1

text: In Washington, D.C., the storm produced wind gusts of up to 45 mph (75 km/h) which, in combination with heavy rainfall, resulted in a few downed tree branches and power lines. High tides left moderate damage in St. Mary's County, Maryland of about $4.4 million (2006 USD), with the damage to trees and power lines considered worse than the impact in Hurricane Isabel in 2003. In neighboring Charles County, storm surge flooding forced the evacuations of houses along the waterfront. The interaction between Ernesto and a high pressure area over eastern Canada produced high winds, heavy rainfall, tidal flooding, and high waves across the Mid-Atlantic and New England. In Delaware, the winds left 151,000 people without power, and the adverse conditions canceled several Labor Day Weekend events. A buoy in the Delaware Bay recorded a record-high wave height of . In southern New Jersey,  winds left over 200,000 buildings without power, while high waves flooded or closed several roads and bridges. Further north, between 2-4 inches (50–100 mm) of rain fell across Pennsylvania and New York. In Pennsylvania, there were two deaths. A seven-year-old boy died at a hospital, after a tree limb fell on him. A man was trying to rescue his golden retriever from a drainage steam, while he was sucked into an outflow pipe, and was found dead after being pulled out of a manhole. The rain in New York caused delays in the play at the 2006 US Open, and washed out a whole day's play.

text: In Washington, D.C., the storm produced wind gusts of up to 45 mph (75 km/h) which, in combination with heavy rainfall, resulted in a few downed tree branches and power lines. High tides left moderate damage in

text: St. Mary's County, Maryland

text: of about $4.4 million (2006 USD), with the damage to trees and power lines considered worse than the

entity_name: Effects of Hurricane Isabel in Maryland and Washington, D.C.

text: impact in Hurricane Isabel

text: in 2003. In neighboring

text: Charles County

text: , storm surge flooding forced the evacuations of houses along the waterfront. The interaction between Ernesto and a high pressure area over eastern Canada produced high winds, heavy rainfall, tidal flooding, and high waves across the Mid-Atlantic and New England. In Delaware, the winds left 151,000 people without power, and the adverse conditions canceled several

text: Labor Day Weekend

text: events. A buoy in the

text: Delaware Bay

text: recorded a record-high wave height of . In southern New Jersey,  winds left over 200,000 buildings without power, while high waves flooded or closed several roads and bridges. Further north, between 2-4 inches (50–100 mm) of rain fell across Pennsylvania and

text: New York

text: . In Pennsylvania, there were two deaths. A seven-year-old boy died at a hospital, after a tree limb fell on him. A man was trying to rescue his

text: golden retriever

text: from a drainage steam, while he was sucked into an outflow pipe, and was found dead after being pulled out of a manhole. The rain in New York caused delays in the play at the

text: 2006 US Open

text: , and washed out a whole day's play.

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answers: high wave height

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answers: High tides

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answers: high tides

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: 1

text: In a wave pool water is pushed out of an opening with enough force to create a wave-like shape.  Riders can ride this type of wave on a regular surfboard.

text: In a

text: wave pool

text: water is pushed out of an opening with enough force to create a wave-like shape.  Riders can ride this type of wave on a regular

text: surfboard

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answers: waves break when they become too tall

answers: NDQ_006453

answers: wave pool

answers: NDQ_006455

answers: water is pushed out

answers: NDQ_006456

answers: pushed

answers: NDQ_006457

answers: surface

answers: NDQ_006458

answers: Friction with the shore

answers: NDQ_006459

answers: water

answers: NDQ_006460

answers: yes

answers: NDQ_006461

answers: water is pushed out of an opening

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Three Willie action figures were created by Playmates Toys for the World of Springfield series: Willie depicted in his usual appearance, released in 2001 in wave 4; "Ripped Willie", released in 2002 as part of wave 8; and "Kilted Willie", released in 2003 in wave 14.

text: Three Willie action figures were created by

text: Playmates Toys

text: for the

text: World of Springfield

text: series: Willie depicted in his usual appearance, released in 2001 in wave 4; "Ripped Willie", released in 2002 as part of wave 8; and "Kilted Willie", released in 2003 in wave 14.

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answers: a bottle bobs in place

answer: No

answer: No

answer: No

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text: Beginning with the Big Bang he believes creation has continued through a series of waves, each one a factor of 20 times shorter in duration than the one preceding it. Each wave has driven the structure of the universe to a higher level.The first wave drove the creation of physical matter, the second living cells, the third multicellular life, the fourth organisms living in family groups, the fifth, saw humans in tribal groups, and the sixth in national groups. The seventh wave encompasses human awareness of the whole planet, and the eighth awareness of our place in the galactic structure. The final wave, the ninth and shortest of all, began on 8 March 2011 and will complete along with all the others on 28 October 2011 sees awareness of the whole of the cosmos achieved. Rather than the series ending with an Apocalypse he describes it as the completion of the creation process of the Universe. The way will then be open to the full realisation of consciousness at its highest level which he terms "Unity consciousness".

text: Beginning with the

text: Big Bang

text: he believes creation has continued through a series of waves, each one a factor of 20 times shorter in duration than the one preceding it. Each wave has driven the structure of the universe to a higher level.The first wave drove the creation of physical matter, the second living cells, the third multicellular life, the fourth organisms living in family groups, the fifth, saw humans in tribal groups, and the sixth in national groups. The seventh wave encompasses human awareness of the whole planet, and the eighth awareness of our place in the galactic structure. The final wave, the ninth and shortest of all, began on 8 March 2011 and will complete along with all the others on 28 October 2011 sees awareness of the whole of the cosmos achieved. Rather than the series ending with an Apocalypse he describes it as the completion of the creation process of the Universe. The way will then be open to the full realisation of consciousness at its highest level which he terms "Unity consciousness".

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answers: Apocalypse

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answers: Wave energy is lowest at the surface and increases with depth

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answers: Waves

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answers: Each wave has driven the structure of the universe to a higher level

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Within this third generation of models, the spectral wave transport equation is used to describe the change in wave spectrum over changing topography.  It simulates wave generation, wave movement (propagation within a fluid), wave shoaling, refraction, energy transfer between waves, and wave dissipation.  Since surface winds are the primary forcing mechanism in the spectral wave transport equation, ocean wave models use information produced by numerical weather prediction models as inputs to determine how much energy is transferred from the atmosphere into the layer at the surface of the ocean.  Along with dissipation of energy through whitecaps and resonance between waves, surface winds from numerical weather models allow for more accurate predictions of the state of the sea surface.

text: Within this third generation of models, the spectral wave transport equation is used to describe the change in wave spectrum over changing topography.  It simulates wave generation, wave movement (propagation within a fluid),

text: wave shoaling

text: refraction

text: , energy transfer between waves, and wave dissipation.  Since surface winds are the primary forcing mechanism in the spectral wave transport equation, ocean wave models use information produced by numerical weather prediction models as inputs to determine how much energy is transferred from the atmosphere into the layer at the surface of the ocean.  Along with dissipation of energy through

text: whitecaps

text: and

text: resonance

text: between waves, surface winds from numerical weather models allow for more accurate predictions of the state of the sea surface.

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answers: spectral wave transport equation

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answers: surface

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answers: wave shoaling

answer: Yes

answer: Yes

answer: Yes

answer: No

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answer: 1

text: Around one mile north of Shek O beach, after passing the Shek O Country Club, is Big Wave Bay.  As its name suggests, big waves roll on to the beach, propelled by the wind, making it a popular destination for surfers. Wind surfers can be found in the sea off Big Wave Bay and Shek O beaches. The Dragon's Back above Shek O is home to Hong Kong Island's only paragliding site. Paragliders can be seen riding the lift and landing at the nearby Rocky Bay. Big Wave Bay Beach is also the site of prehistoric rock carving similar to those found on Cheung Chau Island.

text: Around one mile north of Shek O beach, after passing the Shek O Country Club, is

text: Big Wave Bay

text: .  As its name suggests, big waves roll on to the beach, propelled by the wind, making it a popular destination for surfers. Wind surfers can be found in the sea off Big Wave Bay and Shek O beaches. The Dragon's Back above Shek O is home to Hong Kong Island's only paragliding site. Paragliders can be seen riding the lift and landing at the nearby Rocky Bay. Big Wave Bay Beach is also the site of prehistoric

text: rock carving

text: similar to those found on

text: Cheung Chau

text: Island.

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answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: 1

text: Due to the weak and disorganized structure of the storm, its effects upon landfall in Florida were minimal. Gusty winds damaged newly planted trees, and some power lines were downed; throughout the state, roughly 14,000 people lost power. A storm surge of  was measured at Virginia Key. Tropical storm-force winds were recorded in several areas, although sustained winds of over 40 mph (65 km/h) were confined to Virginia Key. Rainfall was also minimal, with a maximum of  falling in northern Miami-Dade County. Overall, monetary losses as a result of the storm in Florida amounted to $2,000 (2010 USD). In Pinellas County, one person was hospitalized after being struck by lightning at Fred Howard Park on July 24.

text: Due to the weak and disorganized structure of the storm, its effects upon landfall in Florida were minimal. Gusty winds damaged newly planted trees, and some power lines were downed; throughout the state, roughly 14,000 people lost power. A storm surge of  was measured at

text: Virginia Key

text: . Tropical storm-force winds were recorded in several areas, although sustained winds of over 40 mph (65 km/h) were confined to Virginia Key. Rainfall was also minimal, with a maximum of  falling in northern

text: Miami-Dade County

text: . Overall, monetary losses as a result of the storm in Florida amounted to $2,000 (2010 USD). In

text: Pinellas County

text: , one person was hospitalized after being struck by lightning at Fred Howard Park on July 24.

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answers: A storm surge

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answers: confined to Virginia Key

answer: Yes

answer: Yes

answer: Yes

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text: He examined wind and wave effects, and his analysis  is the first quantitative discussion of wave height as a (square root) function of fetch. His paper  is one of the first quantitative studies of windspeeds in the planetary boundary layer. Motivated by practical applications, these are fundamental contributions. He designed the Stevenson screen as a shelter to shield meteorological instruments, and this has been widely adopted.

text: He examined wind and wave effects, and his analysis  is the first quantitative discussion of wave height as a (square root) function of fetch. His paper  is one of the first quantitative studies of windspeeds in the planetary boundary layer. Motivated by practical applications, these are fundamental contributions. He designed the

text: Stevenson screen

text: as a shelter to shield

text: meteorological

text: instruments, and this has been widely adopted.

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answers: He examined wind and wave effects

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answer: Yes

answer: Yes

answer: Yes

answer: Yes

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text: Sea-floor maps released by the US National Oceanic and Atmospheric Administration in 2007 revealed the mechanisms behind Mavericks' waves. A long, sloping ramp leads to the surface. The ramp slows the propagation of the wave over it. The wave over the deep troughs on each side of the ramp continues at full speed forming two angles in the wavefront centered over the boundaries between the ramp and the troughs.  The result of this is a U-shaped or V-shaped wavefront on the ramp that contains the wave energy from the full width of the ramp.  This U-shaped or V-shaped wave then collapses into a small area at the top center of the ramp with tremendous force.

text: Sea-floor maps released by the US National Oceanic and Atmospheric Administration in 2007 revealed the mechanisms behind Mavericks' waves. A long, sloping ramp leads to the surface. The ramp slows the propagation of the wave over it. The wave over the deep troughs on each side of the ramp continues at full speed forming two angles in the wavefront centered over the boundaries between the ramp and the troughs.  The result of this is a U-shaped or V-shaped wavefront on the ramp that contains the wave energy from the full width of the ramp.  This U-shaped or V-shaped wave then collapses into a small area at the top center of the ramp with tremendous force.

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answers: Mavericks' waves

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answers: Mavericks' waves

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answers: Mavericks' waves

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answers: full speed

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answers: The ramp slows the propagation of the wave over it

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answers: Mavericks

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answers: surface

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answers: The ramp slows the propagation of the wave

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: In his 1966 account of the incident, The Wreck of the Memphis, Captain Beachs son, Edward L. Beach, Jr., ascribed her loss to an unexpected tsunami exceeding  in height, and this explanation has been carried forward by most sources discussing her loss. More recent research, however, has called this explanation into question. No record of any seismic event in the Caribbean on 29 August 1916 that could have triggered a tsunami has been found, and the rate of advance of the large wave Memphis reported — about an hour to cross the distance from the horizon to the ship — matches that of a wind-generated ocean wave (possibly a rogue wave); a tsunami, in contrast, would have covered the distance in only a few minutes. The periods of the three large waves that struck Memphis also are characteristic of large wind-generated waves rather than tsunamis.

text: In his 1966 account of the incident, The Wreck of the Memphis, Captain Beachs son,

text: Edward L. Beach, Jr.

text: , ascribed her loss to an unexpected

text: tsunami

text: exceeding  in height, and this explanation has been carried forward by most sources discussing her loss. More recent research, however, has called this explanation into question. No record of any seismic event in the Caribbean on 29 August 1916 that could have triggered a tsunami has been found, and the rate of advance of the large wave Memphis reported — about an hour to cross the distance from the horizon to the ship — matches that of a wind-generated ocean wave (possibly a

text: rogue wave

text: ); a tsunami, in contrast, would have covered the distance in only a few minutes. The periods of the three large waves that struck Memphis also are characteristic of large wind-generated waves rather than tsunamis.

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answers: an unexpected tsunami exceeding in height

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answers: The Wreck of the Memphis

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answer: Yes

answer: No

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text: Strong winds from Isabel extended from North Carolina to New England and westward to West Virginia. The winds, combined with previous rainfall which moistened the soil, downed many trees and power lines across its path, leaving about 6 million electricity customers without power at some point. Parts of coastal Virginia, especially in the Hampton Roads and Northeast North Carolina areas, were without electricity for almost a month. Coastal areas suffered from waves and its powerful storm surge, with areas in eastern North Carolina and southeast Virginia reporting severe damage from both winds and the storm surge. Throughout its path, Isabel resulted in $3.6 billion in damage (2003 USD, $

text: Strong winds from Isabel extended from

text: North Carolina

text: to

text: New England

text: and westward to

text: West Virginia

text: . The winds, combined with previous rainfall which moistened the soil, downed many trees and power lines across its path, leaving about 6 million electricity customers without power at some point. Parts of coastal

text: Virginia

text: , especially in the

text: Hampton Roads

text: and Northeast

text: North Carolina

text: areas, were without

text: electricity

text: for almost a month. Coastal areas suffered from waves and its powerful storm surge, with areas in eastern North Carolina and southeast

text: Virginia

text: reporting severe damage from both winds and the storm surge. Throughout its path, Isabel resulted in $3.6 billion in damage (2003 USD, $

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answers: Strong winds from Isabel

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answers: Storm surge

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answers: Strong winds

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answer: Yes

answer: Yes

answer: No

answer: Yes

answer: No

answer: 1

text: A tropical wave emerged into the Atlantic Ocean from the west coast of Africa near Dakar, Senegal on September 22. The wave traveled westward with minimal tropical cyclogenesis and reached the Lesser Antilles about a week later. While passing through the islands, heavy rainfall and strong winds were reported. Eventually, the system developed into a broad area of low pressure and acquired a low-level circulation. However, upper-level wind shear resulted in no immediate further organization. After crossing Puerto Rico and the Virgin Islands, wind shear decreased, since the low was moving in the same direction as the upper-level winds.

text: A tropical wave emerged into the Atlantic Ocean from the west coast of Africa near

text: Dakar, Senegal

text: on September 22. The wave traveled westward with minimal

text: tropical cyclogenesis

text: and reached the Lesser Antilles about a week later. While passing through the islands, heavy rainfall and strong winds were reported. Eventually, the system developed into a broad area of low pressure and acquired a low-level circulation. However, upper-level wind shear resulted in no immediate further organization. After crossing Puerto Rico and the Virgin Islands, wind shear decreased, since the low was moving in the same direction as the upper-level winds.

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answers: NDQ_006458

answers: While passing through the islands, heavy rainfall and strong winds

answers: NDQ_006459

answers: upper-level wind shear

answers: NDQ_006460

answers: The wave traveled westward

answers: NDQ_006461

answers: low-level circulation

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: No

answer: 1

text: Hurricane Gonzalo originated in a tropical wave that emerged from the western coast of Africa on October 4 and trekked across the Atlantic. Despite an attendant expanse of clouds and thunderstorms, hostile winds from an upper-level trough hindered cyclogenesis. On October 10, after encountering an eastward-propagating Kelvin wave, the system developed more concentrated convection. With conditions increasingly favorable for further development, the disturbance gradually became better organized, forming a small low pressure area by October 11. In turn, a tropical depression formed at 00:00 UTC on October 12, located approximately 390 mi (630 km) east of the Leeward Islands. Continued maturation amid warm waters and low wind shear yielded Tropical Storm Gonzalo 12 hours later. Operationally, the National Hurricane Center (NHC) did not begin issuing advisories on the cyclone until midday on October 12, after a Hurricane Hunter flight into the system reported surface winds of 40 mph (65 km/h).

text: Hurricane Gonzalo originated in a

text: tropical wave

text: that emerged from the western coast of Africa on October 4 and trekked across the Atlantic. Despite an attendant expanse of clouds and thunderstorms, hostile winds from an

text: upper-level trough

text: hindered

text: cyclogenesis

text: . On October 10, after encountering an eastward-propagating

text: Kelvin wave

text: , the system developed more concentrated

text: convection

text: . With conditions increasingly favorable for further development, the disturbance gradually became better organized, forming a small

text: low pressure area

text: by October 11. In turn, a tropical depression formed at 00:00

text: UTC

text: on October 12, located approximately 390 mi (630 km) east of the

text: Leeward Islands

text: . Continued maturation amid warm waters and low

text: wind shear

text: yielded Tropical Storm Gonzalo 12 hours later. Operationally, the

text: National Hurricane Center

text: (NHC) did not begin issuing advisories on the cyclone until midday on October 12, after a

text: Hurricane Hunter

text: flight into the system reported

text: surface winds

text: of 40 mph (65 km/h).

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answers: Kelvin wave

answers: NDQ_006453

answers: tropical wave

answers: NDQ_006455

answers: cyclogenesis

answers: NDQ_006456

answers: eastward

answers: NDQ_006457

answers: surface winds

answers: NDQ_006458

answers: Kelvin wave

answers: NDQ_006459

answers: Kelvin wave

answers: NDQ_006460

answers: It trekked across the Atlantic

answers: NDQ_006461

answers: Kelvin wave

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: Yes

answer: 1

text: The high pressure gas exiting the cylinder initially flows in the form of a "wavefront" as all disturbances in fluids do. The exhaust gas pushes its way into the pipe which is already occupied by gas from previous cycles, pushing that gas ahead and causing a wave front. Once the gas flow stops, the wave continues, passing the energy to the next gas down stream and so on to the end of the pipe. If this wave encounters any change in cross section or temperature it will reflect a portion of its strength in the opposite direction to its travel. For example, a strong acoustic wave encountering an increase in area will reflect a weaker acoustic wave in the opposite direction. A strong acoustic wave encountering a decrease in area will reflect a strong acoustic wave in the opposite direction. The basic principle is described in wave dynamics.An expansion chamber makes use of this phenomenon by varying its diameter (cross section) and length to cause these reflections to arrive back at the cylinder at the desired time in the cycle.

text: The high

text: pressure

text: gas exiting the cylinder initially flows in the form of a "

text: wave

text: front" as all disturbances in fluids do. The exhaust gas pushes its way into the pipe which is already occupied by gas from previous cycles, pushing that gas ahead and causing a wave front. Once the gas flow stops, the wave continues, passing the energy to the next gas down stream and so on to the end of the pipe. If this wave encounters any change in

text: cross section

text: or

text: temperature

text: it will reflect a portion of its strength in the opposite direction to its travel. For example, a strong acoustic wave encountering an increase in area will reflect a weaker acoustic wave in the opposite direction. A strong acoustic wave encountering a decrease in area will reflect a strong acoustic wave in the opposite direction. The basic principle is described in

text: wave dynamics

text: .An expansion chamber makes use of this phenomenon by varying its diameter (cross section) and length to cause these reflections to arrive back at the cylinder at the desired time in the cycle.

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answers: If this wave encounters any change in cross section or temperature

answers: NDQ_006453

answers: Sea level rise

answers: NDQ_006455

answers: The exhaust gas pushes its way into the pipe

answers: NDQ_006456

answers: opposite direction

answers: NDQ_006457

answers: The basic principle is described in wave dynamics

answers: NDQ_006458

answers: The basic principle is described in wave dynamics

answers: NDQ_006459

answers: high pressure gas

answers: NDQ_006460

answers: no

answers: NDQ_006461

answers: If this wave encounters any change in cross section or temperature it will reflect a portion of its strength in the opposite direction to its travel

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: In a big wave wipeout, a breaking wave can push surfers down 20 to 50 feet (6.2 m to 15.5 m) below the surface. Once they stop spinning around, they have to quickly regain their equilibrium and figure out which way is up. Surfers may have less than 20 seconds to get to the surface before the next wave hits them. Additionally, the water pressure at a depth of 20 to 50 feet can be strong enough to rupture one's eardrums. Strong currents and water action at those depths can also slam a surfer into a reef or the ocean floor, which can result in severe injuries or even death.

text: In a big wave wipeout, a breaking wave can push surfers down 20 to 50 feet (6.2 m to 15.5 m) below the surface. Once they stop spinning around, they have to quickly regain their equilibrium and figure out which way is up. Surfers may have less than 20 seconds to get to the surface before the next wave hits them. Additionally, the water pressure at a depth of 20 to 50 feet can be strong enough to rupture one's eardrums. Strong currents and water action at those depths can also slam a surfer into a reef or the ocean floor, which can result in severe injuries or even death.

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text: A European windstorm crosses over Scotland and plunges into the mouth of the North Sea, to the west of Norway, where its strong winds push large bodies of water Southeast, towards coastal regions in England and the Netherlands. The tidal surge puts both nations on red alert as the English evacuate some coastal villages and close the Thames Barrier. The Dutch close the Eastern Scheldt storm surge barrier and the enormous Maeslant barrier in order to prevent massive flooding as the storm mimics the situation that caused the devastating North Sea flood of 1953. For the first time since 1976, the entire Dutch coastline is put on alert and is closely monitored by officials. The tidal surge turned out to be too weak to cause any significant damage to the strong Dutch coastal defenses. In England, only minor flooding occurred.

text: A

text: European windstorm

text: crosses over Scotland and plunges into the mouth of the

text: North Sea

text: , to the west of Norway, where its strong winds push large bodies of water Southeast, towards coastal regions in England and the Netherlands. The tidal surge puts both nations on red alert as the English evacuate some coastal villages and close the

text: Thames Barrier

text: . The Dutch close the

text: Eastern Scheldt storm surge barrier

text: and the enormous

text: Maeslant barrier

text: in order to prevent massive flooding as the storm mimics the situation that caused the devastating

text: North Sea flood of 1953

text: . For the first time since 1976, the entire Dutch coastline is put on alert and is closely monitored by officials. The tidal surge turned out to be too weak to cause any significant damage to the strong Dutch coastal defenses. In England, only minor flooding occurred.

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answers: Tidal surge

answer: Yes

answer: Yes

answer: Yes

answer: No

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answer: 1

text: In advance of the storm, tropical cyclone watches and warnings were issued for coastal areas, while rescue teams and the U.S. Coast Guard were put on standby. The storm dropped heavy rainfall near its immediate landfall location but little precipitation elsewhere. Along the coast of North Carolina, high waves, rip currents, and storm surge were reported. Slight localized flooding was reported. Gusty winds also occurred, though no wind damage was reported. Along the coast of Florida, rough surf drowned one person. Overall damage was minor.

text: In advance of the storm,

text: tropical cyclone watches and warnings

text: were issued for coastal areas, while rescue teams and the U.S. Coast Guard were put on standby. The storm dropped heavy rainfall near its immediate landfall location but little precipitation elsewhere. Along the coast of North Carolina, high waves,

text: rip current

text: s, and

text: storm surge

text: were reported. Slight localized flooding was reported. Gusty winds also occurred, though no wind damage was reported. Along the coast of Florida, rough surf drowned one person. Overall damage was minor.

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answers: rip currents

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answer: Yes

answer: Yes

answer: Yes

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text: Almost periodic function – Amplitude modulation – Amplitude – Beat – Chaos theory – Cyclic group – Diffraction – Doppler effect – Eigenstate – Eigenvalue – Fibonacci sequence – Fourier series – Frequency domain – Frequency spectrum – Hamiltonian (quantum mechanics) – Harmonic oscillator – Huygens–Fresnel principle – Longitudinal wave – Mechanical wave – Navier–Stokes equations – Partial differential equation – Periodic function – Permutation – Phase (waves) – Physics of music – Power spectrum – Signal – Sine wave – Spectrum of an operator – Translational symmetry – Transverse wave – Wave equation – Wave–particle duality – Wave – Waveform

text: Almost periodic function

text: Amplitude modulation

text: Amplitude

text: Beat

text: Chaos theory

text: Cyclic group

text: Diffraction

text: Doppler effect

text: Eigenstate

text: Eigenvalue

text: Fibonacci sequence

text: Fourier series

text: Frequency domain

text: Frequency spectrum

text: Hamiltonian (quantum mechanics)

text: Harmonic oscillator

text: Huygens–Fresnel principle

text: Longitudinal wave

text: Mechanical wave

text: Navier–Stokes equations

text: Partial differential equation

text: Periodic function

text: Permutation

text: Phase (waves)

text: Physics of music

text: Power spectrum

text: Signal

text: Sine wave

text: Spectrum of an operator

text: Translational symmetry

text: Transverse wave

text: Wave equation

text: Wave–particle duality

text: Wave

text: Waveform

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answers: Wave equation – Wave–particle duality

answers: NDQ_006453

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answers: Phase

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answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Artificial reefs can also be placed into natural wave environments to enhance the quality of the incoming breaking wave for surfing. Wave focusing areas can build up wave power and height prior to breaking, and breaking surfaces then trip the wave up to make it break; the surfing surface then carries the breaking wave along an angle that maximises its value for surfing.

text: Artificial reef

text: s can also be placed into natural wave environments to enhance the quality of the incoming

text: breaking wave

text: for

text: surfing

text: . Wave focusing areas can build up wave power and height prior to

text: breaking

text: , and breaking surfaces then trip the wave up to make it break; the surfing surface then carries the breaking wave along an angle that maximises its value for surfing.

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text: ) have contributed to solve the riddles of wave breaking behaviors, unfortunately there hasn’t been a clear understanding for exact theories of the wind wave dissipation process still yet because of its non-linear behaviors. By past and present observations and derived theories, the physics of the ocean-wave dissipation can be categorized by its passing regions along to water depth. In deep water, wave dissipation occurs by the actions of friction or drag forces such as opposite-directed winds or viscous forces generated by turbulent flows—usually nonlinear forces. In shallow water, the behaviors of wave dissipations are mostly types of shore wave breaking (see Types of wave breaking). Some of simple general descriptions of wind-wave dissipation (defined by Luigi Cavaleri et al. ) were proposed when we consider only ocean surface waves such as wind waves. By means of the simple, the interactions of waves with the vertical structure of the upper layers of the ocean are ignored for simplified theory in many proposed mechanisms.

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answers: In shallow water, the behaviors of wave dissipations are mostly types of shore wave breaking

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answer: Yes

answer: Yes

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text: There are similarities to descriptions of the 1953 floods in East Anglia which were caused by a storm surge. Some of the original sources frequently referred to the high spring tide and strong winds from the southwest, classic conditions for a storm surge. Horsburgh and Horritt have shown that the tide and probable weather at the time were capable of generating a surge that is consistent with the observed inundation.

text: There are similarities to descriptions of the

text: 1953 floods in East Anglia

text: which were caused by a storm surge. Some of the original sources frequently referred to the high

text: spring tide

text: and strong winds from the southwest, classic conditions for a storm surge. Horsburgh and Horritt have shown that the tide and probable weather at the time were capable of generating a surge that is consistent with the observed inundation.

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answers: storm surge

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answers: Storm surge

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answer: No

answer: Yes

answer: No

answer: No

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text: In contrast to Delaware and Maryland, the strong northeast portion of the nor'easter affected New Jersey for several days, producing strong winds and record high tides. Wind gusts reached  in Cape May, which were the strongest winds in association with the storm. Sustained winds were around  in the region. High winds in Atlantic City destroyed the windows of storefronts. Along the Jersey coast, the nor'easter produced waves of up to  in height. About  offshore Long Branch, waves reached heights of . In South Jersey, the storm surge struck the coast near low tide, which restricted flooding. The highest tide in South Jersey was  in Ocean City, which broke the previous record of  set in 1984. Further north, the surge coincided with several days of high tides and a lunar tide, causing significant flooding and beach erosion. The highest tide was  in Perth Amboy along the Raritan River, which broke the record set in 1960. In many locations, the storm produced the highest tides since the Ash Wednesday Storm of 1962. The storm also dropped rainfall across the state, peaking at  in Morristown, along with gusts peaking at 58 mph (93 kph) at Morristown Municipal Airport. The rainfall caused higher discharge rates along rivers. The storm also produced high snowfall totals, including  in Sussex County. Throughout the coastline, the cost to replace the lost beach from erosion was estimated at $300 million (1992 USD).

text: In contrast to Delaware and Maryland, the strong northeast portion of the nor'easter affected New Jersey for several days, producing strong winds and record high tides. Wind gusts reached  in

text: Cape May

text: , which were the strongest winds in association with the storm.

text: Sustained

text: winds were around  in the region. High winds in Atlantic City destroyed the windows of storefronts. Along the Jersey coast, the nor'easter produced waves of up to  in height. About  offshore

text: Long Branch

text: , waves reached heights of . In

text: South Jersey

text: , the

text: storm surge

text: struck the coast near low tide, which restricted flooding. The highest tide in South Jersey was  in

text: Ocean City

text: , which broke the previous record of  set in 1984. Further north, the surge coincided with several days of high tides and a

text: lunar tide

text: , causing significant flooding and beach erosion. The highest tide was  in

text: Perth Amboy

text: along the

text: Raritan River

text: , which broke the record set in 1960. In many locations, the storm produced the highest tides since the

text: Ash Wednesday Storm of 1962

text: . The storm also dropped rainfall across the state, peaking at  in

text: Morristown

text: , along with gusts peaking at 58 mph (93 kph) at Morristown Municipal Airport. The rainfall caused higher discharge rates along rivers. The storm also produced high snowfall totals, including  in

text: Sussex County

text: . Throughout the coastline, the cost to replace the lost beach from erosion was estimated at $300 million (1992 USD).

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answers: Along the Jersey coast

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answer: Yes

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text: Sidi Kaouki is fast becoming one of the most popular surf and wind surfing destinations in Morocco. There a number of surf sports including beach breaks and reef breaks that produce punchy peaks and nice shaped waves. It is also a great spot for kite surfing as the wind is stronger than some other nearby spots including Essaouira.

text: Sidi Kaouki is fast becoming one of the most popular surf and wind surfing destinations in Morocco. There a number of surf sports including beach breaks and reef breaks that produce punchy peaks and nice shaped waves. It is also a great spot for kite surfing as the wind is stronger than some other nearby spots including Essaouira.

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text: East coasts also receive heavy winter swells when low-pressure cells form in the sub-tropics, where slow moving highs inhibit their movement. These lows produce a shorter fetch than polar fronts, however they can still generate heavy swells, since their slower movement increases the duration of a particular wind direction. The variables of fetch and duration both influence how long wind acts over a wave as it travels, since a wave reaching the end of a fetch behaves as if the wind died.

text: East coasts also receive heavy winter swells when low-pressure cells form in the sub-tropics, where slow moving

text: highs

text: inhibit their movement. These lows produce a shorter fetch than polar fronts, however they can still generate heavy swells, since their slower movement increases the duration of a particular wind direction. The variables of fetch and duration both influence how long wind acts over a wave as it travels, since a wave reaching the end of a fetch behaves as if the wind died.

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answers: swells when low-pressure cells form in the sub-tropics

answers: NDQ_006453

answers: fetch

answers: NDQ_006455

answers: low-pressure cells form

answers: NDQ_006456

answers: slow moving

answers: NDQ_006457

answers: highs inhibit their movement

answers: NDQ_006458

answers: swells when low-pressure cells form in the sub-tropics

answers: NDQ_006459

answers: lows

answers: NDQ_006460

answers: fetch

answers: NDQ_006461

answers: slow moving highs inhibit their movement

answer: No

answer: Yes

answer: No

answer: No

answer: No

answer: 1

text: Waves are disturbances that carry energy as they move. Mechanical waves propagate through a medium – air or water, making it oscillate as they pass by. Wind waves are surface waves that create the chaotic patterns of the sea. As they pass over sand, such waves create patterns of ripples; similarly, as the wind passes over sand, it creates patterns of dunes.

text: Wave

text: s are disturbances that carry energy as they move.

text: Mechanical wave

text: s propagate through a medium – air or water, making it

text: oscillate

text: as they pass by.

text: Wind wave

text: s are

text: surface wave

text: s that create the chaotic patterns of the sea. As they pass over sand, such waves create patterns of ripples; similarly, as the wind passes over sand, it creates patterns of

text: dune

text: s.

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answers: Waves are disturbances

answers: NDQ_006453

answers: dunes

answers: NDQ_006455

answers: mechanical waves propagate

answers: NDQ_006456

answers: oscillate

answers: NDQ_006457

answers: Surface waves

answers: NDQ_006458

answers: As they pass over sand

answers: NDQ_006459

answers: the sea

answers: NDQ_006460

answers: As they pass over sand

answers: NDQ_006461

answers: Mechanical waves propagate through a medium

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: 1

text: Wind power is affected by air temperature because colder air is more dense and therefore more effective at producing wind power.  As a result, wind power is affected seasonally (more output in winter than summer) and by daily temperature variations. During the 2006 California heat wave output from wind power in California significantly decreased to an average of 4% of capacity for seven days.  A similar result was seen during the 2003 European heat wave, when the output of wind power in France, Germany, and Spain fell below 10% during peak demand times.

text: Wind power is affected by air temperature because colder air is more dense and therefore more effective at producing wind power.  As a result, wind power is affected seasonally (more output in winter than summer) and by daily temperature variations. During the

text: 2006 California heat wave

text: output from

text: wind power in California

text: significantly decreased to an average of 4% of capacity for seven days.  A similar result was seen during the

text: 2003 European heat wave

text: , when the output of wind power in France, Germany, and Spain fell below 10% during peak demand times.

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answers: colder air is more dense

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answer: Yes

answer: No

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text: On August 30, 2010, the eye of Hurricane Earl passed just 15 to 20 miles north of Anegada at category 4, with winds in excess of 135 mph. The close passage led to significant damage on the island, with major flooding on the south side from the storm surge and breaking waves. The north side of the island experienced no storm surge, and Horseshoe Reef protected the north side of the island from breaking waves. 24 hours before the storm arrived, the forecast was for the storm to pass well to the north. By the time that it was apparent that the hurricane was going to have major impact, all transportation service from Anegada (air and ferry) had been suspended. Fortunately, there were no serious injuries to anyone on the island.

text: On August 30, 2010, the eye of

text: Hurricane Earl

text: passed just 15 to 20 miles north of Anegada at category 4, with winds in excess of 135 mph. The close passage led to significant damage on the island, with major flooding on the south side from the

text: storm surge

text: and breaking waves. The north side of the island experienced no storm surge, and Horseshoe Reef protected the north side of the island from breaking waves. 24 hours before the storm arrived, the forecast was for the storm to pass well to the north. By the time that it was apparent that the hurricane was going to have major impact, all transportation service from Anegada (air and ferry) had been suspended. Fortunately, there were no serious injuries to anyone on the island.

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text: A retrospective analysis, or reanalysis, combines all available observations with a physical model to describe the state of a system over a time period of decades.  Wind waves are a part of both the NCEP Reanalysis and the ERA-40 from the ECMWF. Such resources permit the creation of monthly wave climatologies, and can track the variation of wave activity on interannual and multi-decadal time scales.  During the northern hemisphere winter, the most intense wave activity is located in the central North Pacific south of the Aleutians, and in the central North Atlantic south of Iceland. During the southern hemisphere winter, intense wave activity circumscribes the pole at around 50°S, with 5 m significant wave heights typical in the southern Indian Ocean.

text: A retrospective analysis, or reanalysis, combines all available observations with a physical model to describe the state of a system over a time period of decades.  Wind waves are a part of both the NCEP Reanalysis and the

text: from the ECMWF. Such resources permit the creation of monthly wave climatologies, and can track the variation of wave activity on interannual and multi-decadal time scales.  During the northern hemisphere winter, the most intense wave activity is located in the central North Pacific south of the Aleutians, and in the central North Atlantic south of Iceland. During the southern hemisphere winter, intense wave activity circumscribes the pole at around 50°S, with 5 m significant wave heights typical in the southern Indian Ocean.

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answers: Wind waves

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answers: wind

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answers: lateral

answers: NDQ_006457

answers: Wave energy is lowest at the surface and increases with depth

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answers: 5 m significant wave heights typical in the southern Indian Ocean

answers: NDQ_006459

answers: physical model

answers: NDQ_006460

answers: shoreline

answers: NDQ_006461

answers: can track the variation of wave activity

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: 1

text: ACE focuses upon the most intense winds concentrated in a storm's center. Whereas, the actual destructive power of a storm depends upon the total area impacted with damaging winds, waves, and storm surge. The metric Integrated Kinetic Energy (IKE), developed in 2007, more accurately reflects the destructive potential.  It examines the kinetic energy that forces a storm surge and creates high waves as well as the horizontal wind loads over the full storm. This metric yields a time specific value for a storm and doesn't account for the destruction caused by a storm over its entire life.  Therefore, in 2013 the researchers at the University of Florida created a metric called Track Integrated Kinetic Energy (TIKE). TIKE expands the concept by accumulating IKE over the lifespan of an individual tropical cyclone and a total value for all named tropical cyclones in the season.

text: ACE focuses upon the most intense winds concentrated in a storm's center. Whereas, the actual destructive power of a storm depends upon the total area impacted with damaging winds, waves, and storm surge. The metric Integrated Kinetic Energy (IKE), developed in 2007, more accurately reflects the destructive potential.  It examines the kinetic energy that forces a storm surge and creates high waves as well as the horizontal wind loads over the full storm. This metric yields a time specific value for a storm and doesn't account for the destruction caused by a storm over its entire life.  Therefore, in 2013 the researchers at the University of Florida created a metric called Track Integrated Kinetic Energy (TIKE). TIKE expands the concept by accumulating IKE over the lifespan of an individual tropical cyclone and a total value for all named tropical cyclones in the season.

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answers: high waves

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answers: storm surge

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answers: a storm surge

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answers: kinetic

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answers: Integrated Kinetic Energy (IKE)

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answers: Integrated Kinetic Energy (IKE)

answers: NDQ_006459

answers: kinetic energy

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answers: Waves

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answers: Integrated Kinetic Energy (IKE)

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: Yes

answer: 1

text: 3. The interactions between the waves on the surface generate longer waves (Hasselmann et al., 1973) and the interaction will transfer wave energy from the shorter waves generated by the Miles mechanism to the waves have slightly lower frequencies than the frequency at the peak wave magnitudes, then finally the waves will be faster than the cross wind speed (Pierson & Moskowitz).

text: 3. The interactions between the waves on the surface generate longer waves (Hasselmann et al., 1973) and the interaction will transfer wave energy from the shorter waves generated by the Miles mechanism to the waves have slightly lower frequencies than the frequency at the peak wave magnitudes, then finally the waves will be faster than the cross wind speed (Pierson & Moskowitz).

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answers: The interactions between the waves on the surface generate longer waves

answers: NDQ_006453

answers: Hasselmann et al

answers: NDQ_006455

answers: interaction

answers: NDQ_006456

answers: cross wind

answers: NDQ_006457

answers: Wave energy is lowest at the surface

answers: NDQ_006458

answers: The interaction will transfer wave energy from the shorter waves generated by the Miles mechanism

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answers: interactions between the waves on the surface

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answers: surface

answers: NDQ_006461

answers: interaction will transfer wave energy from the shorter waves generated by the Miles mechanism

answer: No

answer: No

answer: Yes

answer: No

answer: No

answer: 1

text: The great majority of large breakers seen on a beach result from distant winds. Five factors influence the formation of the flow structures in wind waves:

text: The great majority of large breakers seen on a beach result from distant winds. Five factors influence the formation of the flow structures in wind waves:

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answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: 1

text: His research areas included both pure mathematics (projective geometry, polytopes, random functions and surfaces) and applied mathematics (fluid dynamics, microseisms, the generation of ocean waves by wind, the dynamics of bubbles, sonoluminescence, wave breaking, steep waves, and the exchange of heat and gases at the ocean surface).

text: His research areas included both

text: pure mathematics

text: projective geometry

text: polytopes

text: , random functions and surfaces) and applied mathematics (

text: fluid dynamics

text: , microseisms, the generation of ocean waves by wind, the dynamics of

text: bubbles

text: sonoluminescence

text: wave breaking

text: , steep waves, and the exchange of heat and gases at the ocean surface).

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answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: 1

text: In the Tahitian story of Rata 'Aremata-Popoto ("tidal wave") and 'Aremata-Roroa ("long wave") are two ocean-dwelling monsters that Rata must overcome.

text: In the Tahitian story of

text: Rata

text: 'Aremata-Popoto ("tidal wave") and 'Aremata-Roroa ("long wave") are two ocean-dwelling monsters that Rata must overcome.

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text: equations, as well as custom shapes and custom waves.

text: equations, as well as custom shapes and custom waves.

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text: A tropical wave moved off the western coast of Africa on October 21, briefly developing two weak low pressure areas before the wave crossed into the Pacific Ocean on November 1. Thunderstorm activity slowly increased as the wave interacted within the Intertropical Convergence Zone. After a curved band of convection developed, it is estimated the system formed into Tropical Depression Twenty-E around 0000 UTC on November 11, about 550 mi (1,050 km) southwest of Manzanillo. Throughout its duration, the depression never completely separated from the Intertropical Convergence Zone. When the NHC issued its first advisory on the depression, the agency predicted slight intensification to tropical storm status and for the depression to last at least two days. This was due to a forecast of gradually increasing wind shear after the first 24 hours. Instead, the circulation became very elongated; it is estimated the cyclone degenerated into a trough by late on November 11.

text: A tropical wave moved off the western coast of Africa on October 21, briefly developing two weak low pressure areas before the wave crossed into the Pacific Ocean on November 1. Thunderstorm activity slowly increased as the wave interacted within the Intertropical Convergence Zone. After a curved band of convection developed, it is estimated the system formed into Tropical Depression Twenty-E around 0000 UTC on November 11, about 550 mi (1,050 km) southwest of Manzanillo. Throughout its duration, the depression never completely separated from the Intertropical Convergence Zone. When the NHC issued its first advisory on the depression, the agency predicted slight intensification to tropical storm status and for the depression to last at least two days. This was due to a forecast of gradually increasing wind shear after the first 24 hours. Instead, the circulation became very elongated; it is estimated the cyclone degenerated into a trough by late on November 11.

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answers: Tropical Depression Twenty-E

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answers: Tropical Depression Twenty-E

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text: Note that h is the depth of the fluid (similar to the equivalent depth and analoguous to H in the primitive equations listed above for Rossby-gravity and Kelvin waves), K is temperature diffusion, K is eddy diffusivity, and τ is the wind stress in either the x or y directions.

text: Note that h is the depth of the fluid (similar to the equivalent depth and analoguous to H in the primitive equations listed above for Rossby-gravity and Kelvin waves), K is temperature diffusion, K is eddy diffusivity, and τ is the wind stress in either the x or y directions.

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answer: No

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text: Kruskal's most widely known work was the discovery in the 1960s of the integrability of certain nonlinear partial differential equations involving functions of one spatial variable as well as time.  These developments began with a pioneering computer simulation by Kruskal and Norman Zabusky (with some assistance from Gary Deem) of a nonlinear equation known as the Korteweg–de Vries equation (KdV).  The KdV equation is an asymptotic model of the propagation of nonlinear dispersive waves. But Kruskal and Zabusky  made the startling discovery of a  "solitary wave" solution of the KdV equation that propagates nondispersively and even regains its shape after a collision with other such waves.  Because of the particle-like properties of such a wave, they named it a "soliton," a term that caught on almost immediately.

text: Kruskal's most widely known work was the discovery in the 1960s of the integrability of certain nonlinear partial differential equations involving functions of one spatial variable as well as time.  These developments began with a pioneering computer simulation by Kruskal and

text: Norman Zabusky

text: (with some assistance from Gary Deem) of a nonlinear equation known as the

text: Korteweg–de Vries equation

text: (KdV).  The KdV equation is an asymptotic model of the propagation of nonlinear

text: dispersive

text: waves. But Kruskal and Zabusky  made the startling discovery of a  "solitary wave" solution of the KdV equation that propagates nondispersively and even regains its shape after a collision with other such waves.  Because of the particle-like properties of such a wave, they named it a "

text: soliton

text: ," a term that caught on almost immediately.

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answers: NDQ_006457

answers: The KdV equation is an asymptotic model

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answers: NDQ_006459

answers: nonlinear partial differential equations

answers: NDQ_006460

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answers: NDQ_006461

answers: particle-like properties of such a wave

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The local surfers have forced the wave to break more cleanly, with increased height, by attaching ropes to the bridge which trail submerged planks, creating two large "U"-shapes. Such a shape makes the wave easier to surf for river surfers (playboating makes fewer demands of the wave shape).

text: The local surfers have forced the wave to break more cleanly, with increased height, by attaching ropes to the bridge which trail submerged planks, creating two large "U"-shapes. Such a shape makes the wave easier to surf for river surfers (playboating makes fewer demands of the wave shape).

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answer: No

answer: No

answer: No

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text: The storm affected Marshall Islands around November 28, producing winds as high as . The storm impacted islands of Kwajalein, Majuro, Lae, Wotho, and Eniwetok. Kwajalein Missile Range caught stronger winds than expected from the storm, and operations in the missile range were affected severely. Zelda also produced a pressure of , which was the lowest pressure ever recorded on Kwajalein. Later, In Ebeye, 60 percent of homes were destroyed, and 6,000 people were left homeless. Food and water supplies were contaminated from salt in surge waves, and the water desalination plant became inoperable. Fresh water production records since 1989 were lost during the storm. The local hospital was still intact, but a few power lines were cut. There were no deaths or significant injuries. Other islands in the nation had their water contaminated by saltwater, and 95 percent of the crops were destroyed by the storm surge.  Coral reefs were also damaged when the storm came nearby.

text: The storm affected Marshall Islands around November 28, producing winds as high as . The storm impacted islands of Kwajalein,

text: Majuro

text: Lae

text: Wotho

text: , and

text: Eniwetok

entity_name: Ronald Reagan Ballistic Missile Defense Test Site

text: Kwajalein Missile Range

text: caught stronger winds than expected from the storm, and operations in the missile range were affected severely. Zelda also produced a pressure of , which was the lowest pressure ever recorded on Kwajalein. Later, In

text: Ebeye

text: , 60 percent of homes were destroyed, and 6,000 people were left homeless. Food and water supplies were contaminated from salt in

text: surge waves

text: , and the water desalination plant became inoperable. Fresh water production records since 1989 were lost during the storm. The local hospital was still intact, but a few power lines were cut. There were no deaths or significant injuries. Other islands in the nation had their water contaminated by saltwater, and 95 percent of the crops were destroyed by the storm surge.

text: Coral reefs

text: were also damaged when the storm came nearby.

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answers: waves break when they become too tall to be supported by their base

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answers: Zelda also produced a pressure of

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answer: Yes

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text: The sand deposit may extend well inland from the berm crest, where there may be evidence of one or more older crests (the storm beach) resulting from very large storm waves and beyond the influence of the normal waves. At some point the influence of the waves (even storm waves) on the material comprising the beach stops, and if the particles are small enough (sand size or smaller), winds shape the feature. Where wind is the force distributing the grains inland, the deposit behind the beach becomes a dune.

text: The sand deposit may extend well inland from the berm crest, where there may be evidence of one or more older crests (the storm beach) resulting from very large storm waves and beyond the influence of the normal waves. At some point the influence of the waves (even storm waves) on the material comprising the beach stops, and if the particles are small enough (sand size or smaller), winds shape the feature. Where wind is the force distributing the grains inland, the deposit behind the beach becomes a

text: dune

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text: Cape Fear experienced minor beach erosion. The erosion, combined with high waves, washed out a portion of a roadway. The heavy rainfall in the Outer Banks disabled over 200 cars and flooded nearly 500. Strong wind gusts left around 10,000 buildings without power. Many places were not restored for two to three days after the storm. Wind and storm surge damaged over 100 houses and buildings. Damage amounted to about $7.5 million (2004 USD). Two days after the storm passed, a man drowned off of Nags Head from strong rip currents and waves. This was the only direct casualty from the storm.

text: Cape Fear

text: experienced minor beach erosion. The erosion, combined with high waves, washed out a portion of a roadway. The heavy rainfall in the Outer Banks disabled over 200 cars and flooded nearly 500. Strong wind gusts left around 10,000 buildings without power. Many places were not restored for two to three days after the storm. Wind and storm surge damaged over 100 houses and buildings. Damage amounted to about $7.5 million (2004 USD). Two days after the storm passed, a man drowned off of

text: Nags Head

text: from strong rip currents and waves. This was the only direct casualty from the storm.

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text: According to the superposition principle of quantum mechanics, wave functions can be added together and multiplied by complex numbers to form new wave functions and form a Hilbert space. The inner product between two wave functions is a measure of the overlap between the corresponding physical states and is used in the foundational probabilistic interpretation of quantum mechanics, the Born rule, relating transition probabilities to inner products.   The Schrödinger equation determines how wave functions evolve over time. A wave function behaves qualitatively like other waves, such as water waves or waves on a string, because the Schrödinger equation is mathematically a type of wave equation. This explains the name "wave function", and gives rise to wave–particle duality. However, the wave function in quantum mechanics describes a kind of physical phenomenon, still open to different interpretations, which fundamentally differs from that of classic mechanical waves.

text: According to the

text: superposition principle

text: of quantum mechanics, wave functions can be added together and multiplied by complex numbers to form new wave functions and form a

text: Hilbert space

text: . The inner product between two wave functions is a measure of the overlap between the corresponding physical states and is used in the foundational probabilistic interpretation of quantum mechanics, the

text: Born rule

text: , relating transition probabilities to inner products.   The Schrödinger equation determines how wave functions evolve over time. A wave function behaves qualitatively like other

text: wave

text: s, such as

text: water wave

text: s or waves on a string, because the Schrödinger equation is mathematically a type of

text: wave equation

text: . This explains the name "wave function", and gives rise to

text: wave–particle duality

text: . However, the wave function in quantum mechanics describes a kind of physical phenomenon, still open to different

text: interpretations

text: , which fundamentally differs from that of classic mechanical waves.

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answer: No

answer: No

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answer: No

answer: 1

text: The rules of right-a-way vary slightly with the type of break. Point Breaks will always have a consistent direct of what is inside, that is the person further up the line will have right-away. In a single peak situation where there is both a left and a right two people are able to be on the wave at the same time provided that one goes left and one goes right and that neither crosses the path of the other to go one direction. If this does happen then the surfer who stood up first will get the right-a-way. On a multi peaked wave where the wave eventually comes together both peaks can be surfed until the surfers come together, when they do the surfer who stood up first has right-a-way and the other must maneuver to get off the wave without interrupting the other surfer.

text: The rules of right-a-way vary slightly with the type of break. Point Breaks will always have a consistent direct of what is inside, that is the person further up the line will have right-away. In a single peak situation where there is both a left and a right two people are able to be on the wave at the same time provided that one goes left and one goes right and that neither crosses the path of the other to go one direction. If this does happen then the surfer who stood up first will get the right-a-way. On a multi peaked wave where the wave eventually comes together both peaks can be surfed until the surfers come together, when they do the surfer who stood up first has right-a-way and the other must maneuver to get off the wave without interrupting the other surfer.

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answers: 4

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answers: NDQ_006452

answers: Point Breaks

answers: NDQ_006453

answers: Wave

answers: NDQ_006455

answers: break

answers: NDQ_006456

answers: one direction

answers: NDQ_006457

answers: Wave energy is lowest at the surface

answers: NDQ_006458

answers: Point Breaks will always have a consistent direct of what is inside

answers: NDQ_006459

answers: surfer

answers: NDQ_006460

answers: Point Breaks

answers: NDQ_006461

answers: a consistent direct of what is inside

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: To produce a shock wave, an object in a given medium (such as air or water) must travel faster than the local speed of sound. In the case of an aircraft travelling at high subsonic speed, regions of air around the aircraft may be travelling at exactly the speed of sound, so that the sound waves leaving the aircraft pile up on one another, similar to a traffic jam on a motorway. When a shock wave forms, the local air pressure increases and then spreads out sideways. Because of this amplification effect, a shock wave can be very intense, more like an explosion when heard at a distance (not coincidentally, since explosions create shock waves).

text: To produce a shock wave, an object in a given medium (such as air or water) must travel faster than the local speed of sound. In the case of an aircraft travelling at high subsonic speed, regions of air around the aircraft may be travelling at exactly the speed of sound, so that the sound waves leaving the aircraft pile up on one another, similar to a traffic jam on a motorway. When a shock wave forms, the local air pressure increases and then spreads out sideways. Because of this amplification effect, a shock wave can be very intense, more like an explosion when heard at a distance (not coincidentally, since explosions create shock waves).

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answers: When a shock wave forms

answers: NDQ_006453

answers: Shock wave

answers: NDQ_006455

answers: When a shock wave forms

answers: NDQ_006456

answers: subsonic

answers: NDQ_006457

answers: Because of this amplification effect, a shock wave can be very intense

answers: NDQ_006458

answers: The local air pressure increases and then spreads out sideways

answers: NDQ_006459

answers: explosions

answers: NDQ_006460

answers: It is impossible to say

answers: NDQ_006461

answers: must travel faster than the local speed of sound

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: A storm surge is an onshore gush of water associated with a low pressure weather system—storms.  Storm surges can cause beach accretion and erosion. Historically notable storm surges occurred during the North Sea Flood of 1953, Hurricane Katrina, and the 1970 Bhola cyclone.

text: A

text: storm surge

text: is an onshore gush of water associated with a

text: low pressure

text: weather system—storms.  Storm surges can cause

text: beach accretion

text: and erosion. Historically notable storm surges occurred during the

text: North Sea Flood of 1953

text: Hurricane Katrina

text: , and the

text: 1970 Bhola cyclone

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text: Even before Chaba passed over the Pacific islands, the typhoon generated rough surf. On August 21 on Marpi Point Field in Saipan, a large wave resulted in a fatality and caused another person to become hospitalized. As the typhoon moved through the Northern Mariana Islands, tropical storm conditions were felt in Saipan while typhoon-force winds were felt in Rota and Tinian. Rota was positioned beneath Chaba's eyewall for several hours, resulting in extremely heavy rain and strong winds. The highest recorded wind gust there peaked at 219 km/h (136 mph), and gusts in excess of 160 km/h (100 mph) were documented for ten consecutive hours. Total rainfall measurements at Rota International Airport reached 528 mm (20.80 in). Extensive damage resulted on Rota, with the complete destruction of 50 homes. An additional 175 homes sustained minor damage. At the coast, the storm surge from Chaba caused coastal inundation up to 3.4 m (11 ft) inland, resulting in beach erosion. The toppling of electrical infrastructure resulted in island-wide power outages. Similar effects occurred on Tinian and Saipan, which also experienced widespread power outages and coastal inundation. Across both islands 270 homes were destroyed and 700 others were at least partially damaged. Telephone services were also cut in Tinian. Overall, 13 people were injured and damage costs totaled to approximately US$18 million in the Northern Mariana Islands.

text: Even before Chaba passed over the Pacific islands, the typhoon generated rough surf. On August 21 on

text: Marpi Point Field

text: in

text: Saipan

text: , a large wave resulted in a fatality and caused another person to become hospitalized. As the typhoon moved through the Northern Mariana Islands, tropical storm conditions were felt in Saipan while typhoon-force winds were felt in Rota and

text: Tinian

text: . Rota was positioned beneath Chaba's eyewall for several hours, resulting in extremely heavy rain and strong winds. The highest recorded wind gust there peaked at 219 km/h (136 mph), and gusts in excess of 160 km/h (100 mph) were documented for ten consecutive hours. Total rainfall measurements at

text: Rota International Airport

text: reached 528 mm (20.80 in). Extensive damage resulted on Rota, with the complete destruction of 50 homes. An additional 175 homes sustained minor damage. At the coast, the

text: storm surge

text: from Chaba caused coastal inundation up to 3.4 m (11 ft) inland, resulting in

text: beach erosion

text: . The toppling of electrical infrastructure resulted in island-wide

text: power outage

text: s. Similar effects occurred on Tinian and Saipan, which also experienced widespread power outages and coastal inundation. Across both islands 270 homes were destroyed and 700 others were at least partially damaged. Telephone services were also cut in Tinian. Overall, 13 people were injured and damage costs totaled to approximately

text: US

text: $18 million in the Northern Mariana Islands.

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text: Storm tides threaten, in particular, the coasts of the Netherlands, Belgium, Germany, and Denmark and low lying areas of eastern England particularly around The Wash and Fens.Storm surges are caused by changes in barometric pressure combined with strong wind created wave action.

text: Storm tide

text: s threaten, in particular, the coasts of the Netherlands, Belgium, Germany, and Denmark and low lying areas of eastern England particularly around

text: The Wash

text: and

text: Fens

text: .Storm surges are caused by changes in

text: barometric pressure

text: combined with strong wind created

text: wave action

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answers: Storm surges

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text: Roughly paralleling the North Carolina coast beginning on September 26, Helene's slow movement and strong intensity resulted in moderate to heavy impacts in coastal areas of the state. Despite the hurricane's Category 4 hurricane intensity, due to its closest approach to land remaining offshore, its storm surge remained less than initially forecast. The hurricane's track also placed its strongest storm surge in the eastern hemisphere of the storm, away from any landmasses. Surge heights peaked at 6 ft (1.8 m) near Marine Corps Air Station Cherry Point. In Wilmington, Helene produced ocean swells at the coast 2.5 – 3 times per minute, indicative of a strong hurricane. There, the cumulative sea level was roughly 9 ft (2.7 m) above normal. However, as a result of the storm striking at low tide, damage caused by storm surge was mostly mitigated. Despite this, sand dunes in southern areas of Fort Fisher, were mostly destroyed by waves. On Cedar Island, strong winds produced by the hurricane pushed waves inland, inundating homes. Elsewhere, minor beach erosion occurred.

text: Roughly paralleling the North Carolina coast beginning on September 26, Helene's slow movement and strong intensity resulted in moderate to heavy impacts in coastal areas of the state. Despite the hurricane's Category 4 hurricane intensity, due to its closest approach to land remaining offshore, its

text: storm surge

text: remained less than initially forecast. The hurricane's track also placed its strongest storm surge in the eastern hemisphere of the storm, away from any landmasses. Surge heights peaked at 6 ft (1.8 m) near

text: Marine Corps Air Station Cherry Point

text: . In

text: Wilmington

text: , Helene produced

text: ocean swells

text: at the coast 2.5 – 3 times per minute, indicative of a strong hurricane. There, the cumulative sea level was roughly 9 ft (2.7 m) above normal. However, as a result of the storm striking at

text: low tide

text: , damage caused by storm surge was mostly mitigated. Despite this,

text: sand dune

text: s in southern areas of

text: Fort Fisher

text: , were mostly destroyed by waves. On

text: Cedar Island

text: , strong winds produced by the hurricane pushed waves inland, inundating homes. Elsewhere, minor

text: beach erosion

text: occurred.

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answer: Yes

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text: However, further offshore several breaking seas hit the lifeboat as the swell became larger and the wind increased to a severe gale force 9. At one point, the lifeboat fell 10m from the crest of a wave. Soon afterwards, another huge wave knocked her on her side, but she was able to self right.

text: However, further offshore several breaking seas hit the lifeboat as the swell became larger and the wind increased to a severe gale force 9. At one point, the lifeboat fell 10m from the crest of a wave. Soon afterwards, another huge wave knocked her on her side, but she was able to self right.

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answers: buoyancy

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: 1

text: Winds blowing in an onshore direction (from the sea towards the land) can cause the water to 'pile up' against the coast. This is known as wind set up. Low atmospheric pressure is associated with storm systems and this tends to increase the surface sea level, this is barometric set up. Finally increased wave break height results in a higher water level in the surf zone which is wave set up. Theses three processes interact to create waves that can overtop natural and engineered coastal protection structures thus penetrating seawater further inland than normal.

text: Winds blowing in an onshore direction (from the sea towards the land) can cause the water to 'pile up' against the coast. This is known as wind set up. Low

text: atmospheric pressure

text: is associated with storm systems and this tends to increase the surface sea level, this is barometric set up. Finally increased

text: wave

text: break height results in a higher water level in the

text: surf zone

text: which is wave set up. Theses three processes interact to create waves that can overtop natural and engineered coastal protection structures thus penetrating seawater further inland than normal.

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answers: higher water level

answers: NDQ_006453

answers: barometric set up

answers: NDQ_006455

answers: higher water level in the surf zone

answers: NDQ_006456

answers: onshore

answers: NDQ_006457

answers: surface

answers: NDQ_006458

answers: higher water level in the surf zone

answers: NDQ_006459

answers: storm systems

answers: NDQ_006460

answers: from the sea towards the land

answers: NDQ_006461

answers: barometric set up

answer: Yes

answer: Yes

answer: No

answer: No

answer: No

answer: 1

text: In a similar way, a surface nepheloid layer may be created, due to particle flotation, while intermediate nepheloid layers may be formed at the slopes of the ocean bed due to the dynamics of internal waves.

text: In a similar way, a surface nepheloid layer may be created, due to particle flotation, while intermediate nepheloid layers may be formed at the slopes of the ocean bed due to the dynamics of

text: internal wave

text: s.

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answers: NDQ_006452

answers: slopes

answers: NDQ_006453

answers: nepheloid layer

answers: NDQ_006455

answers: due to particle flotation

answers: NDQ_006456

answers: internal waves

answers: NDQ_006457

answers: surface

answers: NDQ_006458

answers: surface nepheloid layer

answers: NDQ_006459

answers: the slopes of the ocean bed

answers: NDQ_006460

answers: surface

answers: NDQ_006461

answers: particle flotation

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Upon making landfall, Tropical Storm Grace produced a light storm surge of 3.5 feet (1 m) in Matagorda and North Jetty, Texas. Wind gusts peaked at 53 mph (85 km/h) with sustained winds of 40 mph (64 km/h) at Sea Rim State Park. Locations closer to where the storm made landfall reported below tropical storm force winds, with the exception of Galveston which recorded a 40 mph (64 km/h) wind gust. Rainfall was moderate to heavy across eastern Texas, peaking at 10.36 inches (263 mm) in Spindletop Bayou. The outer bands of Grace spawned a waterspout just south of the western tip of Galveston Island, prompting the issuance of a tornado warning. The waterspout dissipated before moving onshore. The storm also caused light beach erosion, though little occurred beyond the erosion caused by Hurricane Claudette one month prior. Near the coast, high tides from the storm flooded piers, bulkheads, and low-lying areas. Further inland, heavy rainfall lead to flash flooding, covering roads and entering a few houses. Overall, damage was minor, and totaled to $113,000 (2003 USD, $132,400 2008 USD).

text: Upon making landfall, Tropical Storm Grace produced a light storm surge of 3.5 feet (1 m) in

text: Matagorda

text: and

text: North Jetty

text: Texas

text: . Wind gusts peaked at 53 mph (85 km/h) with sustained winds of 40 mph (64 km/h) at

text: Sea Rim State Park

text: . Locations closer to where the storm made landfall reported below tropical storm force winds, with the exception of

text: Galveston

text: which recorded a 40 mph (64 km/h) wind gust. Rainfall was moderate to heavy across eastern

text: Texas

text: , peaking at 10.36 inches (263 mm) in

text: Spindletop Bayou

text: . The outer bands of Grace spawned a

text: waterspout

text: just south of the western tip of

text: Galveston Island

text: , prompting the issuance of a

text: tornado warning

text: . The waterspout dissipated before moving onshore. The storm also caused light beach erosion, though little occurred beyond the erosion caused by

text: Hurricane Claudette

text: one month prior. Near the coast, high tides from the storm flooded piers, bulkheads, and low-lying areas. Further inland, heavy rainfall lead to flash flooding, covering roads and entering a few houses. Overall, damage was minor, and totaled to $113,000 (2003 USD, $132,400 2008 USD).

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answers: high tides from the storm

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answers: high tides

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: 1

text: A reef break happens when a wave breaks over a coral reef or a rocky seabed. Examples are Cloudbreak in Fiji and Jaws in Maui.

text: A

text: reef break

text: happens when a wave breaks over a

text: coral reef

text: or a rocky seabed. Examples are

text: Cloudbreak

text: in

text: Fiji

text: and

text: Jaws

text: in Maui.

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answers: NDQ_006452

answers: A reef break

answers: NDQ_006453

answers: Cloudbreak

answers: NDQ_006455

answers: breaks

answers: NDQ_006456

answers: fast

answers: NDQ_006457

answers: Wave energy is lowest at the surface

answers: NDQ_006458

answers: reef break

answers: NDQ_006459

answers: coral reef

answers: NDQ_006460

answers: Shoreline

answers: NDQ_006461

answers: reef break

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The "Waving Song" is one of the fight songs for Oklahoma State. At Oklahoma State football games, the song is played by the Cowboy Marching Band during the pregame traditions, following touchdowns, and after victories against the Cowboys' opponents. For other athletic events, the Waving Song is played after an OSU victory as the start of the fight song trilogy.  While the song is played, fans wave their right arms in the air; the effect is similar to wheat waving in the wind.

text: The "Waving Song" is one of the

text: fight songs

text: for Oklahoma State. At Oklahoma State football games, the song is played by the

entity_name: Oklahoma State University Cowboy Marching Band

text: Cowboy Marching Band

text: during the pregame traditions, following touchdowns, and after victories against the Cowboys' opponents. For other athletic events, the Waving Song is played after an OSU victory as the start of the fight song trilogy.  While the song is played, fans wave their right arms in the air; the effect is similar to wheat waving in the wind.

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answers: The effect is similar to wheat waving in the wind

answers: NDQ_006453

answers: Wheat waving in the wind

answers: NDQ_006455

answers: While the song is played

answers: NDQ_006456

answers: wind

answers: NDQ_006457

answers: Wave energy is lowest at the surface

answers: NDQ_006458

answers: The effect is similar to wheat waving in the wind

answers: NDQ_006459

answers: fans

answers: NDQ_006460

answers: Wave

answers: NDQ_006461

answers: effect is similar to wheat waving in the wind

answer: No

answer: Yes

answer: No

answer: No

answer: No

answer: 1

text: Waves are frequently found at Pampa Grande, primarily on ceramics/pottery. The waves have two different interpretations. Often waves appear in conjunction with right triangles or “stairs”. These geometric shapes would have served as an abbreviated version of earlier and more complex motifs. The first way this geometric motif has been interpreted is symbolizing marine life and its importance. Expert, Ilana Johnson, explains one way the waves can be interpreted. They “…could have been an abbreviated version of the stylized catfish or double-headed serpent motif found in panels on the murals at Huaca de la Luna and Huaca El Brujo [other Moche sites]”. The second way these wave motifs are interpreted are as the Temple of the Stairway and Wave. This is said to have been a ceremonial place where ritual human sacrifice took place. The wave motif is often found in several places on one piece of pottery.

text: Waves are frequently found at Pampa Grande, primarily on ceramics/pottery. The waves have two different interpretations. Often waves appear in conjunction with right triangles or “stairs”. These geometric shapes would have served as an abbreviated version of earlier and more complex motifs. The first way this geometric motif has been interpreted is symbolizing marine life and its importance. Expert, Ilana Johnson, explains one way the waves can be interpreted. They “…could have been an abbreviated version of the stylized catfish or double-headed serpent motif found in panels on the murals at Huaca de la Luna and Huaca El Brujo [other Moche sites]”. The second way these wave motifs are interpreted are as the Temple of the Stairway and Wave. This is said to have been a ceremonial place where ritual human sacrifice took place. The wave motif is often found in several places on one piece of pottery.

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answers: Waves break when they become too tall to be supported by their base

answers: NDQ_006453

answers: Pampa Grande

answers: NDQ_006455

answers: ceramics/pottery

answers: NDQ_006456

answers: Waves

answers: NDQ_006457

answers: Wave energy is lowest at the surface and increases with depth

answers: NDQ_006458

answers: Wave motif is often found in several places on one piece of pottery

answers: NDQ_006459

answers: Moche

answers: NDQ_006460

answers: Waves

answers: NDQ_006461

answers: symbolizing marine life and its importance

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: General: The effects of a hurricane can be scattered across a large area, because hurricanes are large complex storms which spawn smaller thunderstorms, tornadoes, storm surges, and sea waves.  Wind speeds east of the eye can be 40-50 mph (64–80 km/h) higher than winds west of the eye. Wind gusts can be scattered, so boats or debris can ram one house but not another.  One building can seem untouched, while others nearby are flattened; also trees can be partly weakened: tree limbs can fall months later, crashing onto a roof, automobile, fence, etc.

text: General: The effects of a hurricane can be scattered across a large area, because hurricanes are large complex storms which spawn smaller thunderstorms, tornadoes, storm surges, and sea waves.  Wind speeds east of the eye can be 40-50 mph (64–80 km/h) higher than winds west of the eye. Wind gusts can be scattered, so boats or debris can ram one house but not another.  One building can seem untouched, while others nearby are flattened; also trees can be partly weakened: tree limbs can fall months later, crashing onto a roof, automobile, fence, etc.

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answers: Tree limbs

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answers: Wind gusts can be scattered

answer: No

answer: No

answer: Yes

answer: No

answer: No

answer: 1

text: A low-pressure area developed within the monsoon trough on February 1, while located about 250 km (155 mi) south of the Indonesian island of Bali. The low formed due to a surge of energy within the monsoon that had crossed the equator from the northwest. Associated convection was initially sparse, and over the subsequent few days the system tracked west-southwestward without much development, moving around a large ridge over northwestern Australia. There was initially moderate wind shear in the region, although an anticyclone was developing aloft, which allowed the convection was able to persist over the center and gradually develop outflow. Late on February 3, the Perth Tropical Cyclone Warning Center (PTCWC) upgraded the tropical low to a Category 1 on the Australian tropical cyclone scale, estimating 10 minute sustained winds of 65 km/h (40 mph). At 04:00 UTC the next day, the PTCWC named the storm Tropical Cyclone Leon. An hour prior, the Joint Typhoon Warning Center (JTWC) initiated advisories on Tropical Cyclone 11S, while the storm was located about 215 km (130 mi) south-southeast of Christmas Island.

text: A

text: low-pressure area

text: developed within the

text: monsoon trough

text: on February 1, while located about 250 km (155 mi) south of the

text: Indonesia

text: n island of

text: Bali

text: . The low formed due to a surge of energy within the monsoon that had crossed the

text: equator

text: from the northwest. Associated convection was initially sparse, and over the subsequent few days the system tracked west-southwestward without much development, moving around a large

text: ridge

text: over northwestern Australia. There was initially moderate

text: wind shear

text: in the region, although an

text: anticyclone

text: was developing aloft, which allowed the convection was able to persist over the center and gradually develop

text: outflow

text: . Late on February 3, the Perth Tropical Cyclone Warning Center (PTCWC) upgraded the tropical low to a Category 1 on the

text: Australian tropical cyclone scale

text: , estimating 10 minute

text: sustained winds

text: of 65 km/h (40 mph). At 04:00 UTC the next day, the PTCWC

text: named

text: the storm Tropical Cyclone Leon. An hour prior, the

text: Joint Typhoon Warning Center

text: (JTWC) initiated advisories on Tropical Cyclone 11S, while the storm was located about 215 km (130 mi) south-southeast of

text: Christmas Island

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answers: waves break when they become too tall to be supported by their base

answers: NDQ_006453

answers: Cyclone

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answers: surge of energy within the monsoon

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answers: lateral

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answers: Surface wave energy is lowest at the surface and increases with depth

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answers: The low formed due to a surge of energy within the monsoon that had crossed the equator

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answers: 10 minute sustained winds

answers: NDQ_006460

answers: The low-pressure area developed

answers: NDQ_006461

answers: there was initially moderate wind shear in the region

answer: Yes

answer: Yes

answer: No

answer: Yes

answer: No

answer: 1

text: Other phasing adjustments can increase the downward radiation in the far field without tilting the main lobe, creating null fill to compensate for extremely high mountaintop locations, or decrease it in the near field, to prevent excessive exposure to those workers or even nearby homeowners on the ground.  The latter effect is also achieved by half-wave spacing – inserting additional elements halfway between existing elements with full-wave spacing.  This phasing achieves roughly the same horizontal gain as the full-wave spacing; that is, a five-element full-wave-spaced array equals a nine- or ten-element half-wave-spaced array.

text: Other phasing adjustments can increase the downward radiation in the

text: far field

text: without tilting the main

text: lobe

text: , creating

text: null fill

text: to compensate for extremely high

text: mountain

text: top locations, or decrease it in the

text: near field

text: , to prevent excessive exposure to those workers or even nearby homeowners on the ground.  The latter effect is also achieved by half-wave spacing – inserting additional elements halfway between existing elements with full-wave spacing.  This phasing achieves roughly the same horizontal gain as the full-wave spacing; that is, a five-element full-wave-spaced array equals a nine- or ten-element half-wave-spaced array.

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answers: mountaintop locations

answers: NDQ_006453

answers: null fill

answers: NDQ_006455

answers: half-wave spacing

answers: NDQ_006456

answers: horizontal

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answers: phasing

answers: NDQ_006460

answers: Wave

answers: NDQ_006461

answers: half-wave spacing

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Nelscott Reef is an ocean reef near Lincoln City, Oregon, United States, that creates a reef break (a surf-break created by the presence of a rock or coral reef) that is known as the only place on the Oregon Coast with the right conditions for big wave surfing. It is named for the former community of Nelscott, which is now a part of Lincoln City. After watching the perfect big wave a half mile offshore since ’89 and knowing there was no way of paddling a conventional big wave gun through the huge beachbreak to get to it, in 1995 Nelscott Reef pioneer John Forse took an underpowered zodiac out in the 17 feet at 20 second swell and after several tries was able to penetrate the Siletz rivermouth and got outside. Feeling insignificant and vulnerable floating around in the huge open ocean swells he was able to work his way to the channel on the north side of the reef, unpack his gun and paddle to where he thought the take off zone was. With no bearings or landmarks with which to triangulate the wide ranging take off zone he was lucky enough to be in the spot and paddle for his life for the set wave headed his way. The speed of the wave combined with the wind keeping him on the peak prevented him from getting down the face and felt like the “Jay Moriarty stuck in the lip at Mavericks” famous wipeout and got blown out the back only to find the wave’s “big brother” bearing down on him. Scrambling for his life he was able to claw up and over the north shoulder and get out of the impact zone. After that “up close and personal” experience John realized that this was a different kind of wave, and was Great for towsurfing and SUP Surfing.

text: Nelscott Reef is an ocean

text: reef

text: near

text: Lincoln City, Oregon

text: United States

text: , that creates a reef break (a surf-break created by the presence of a rock or coral reef) that is known as the only place on the

text: Oregon Coast

text: with the right conditions for

text: big wave surfing

text: . It is named for the former community of

text: Nelscott

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answers: big wave

answers: NDQ_006453

answers: rivermouth

answers: NDQ_006455

answers: ocean swells

answers: NDQ_006456

answers: forward

answers: NDQ_006457

answers: The speed of the wave

answers: NDQ_006458

answers: impact zone

answers: NDQ_006459

answers: ocean reef

answers: NDQ_006460

answers: A surf-break

answers: NDQ_006461

answers: swell

answer: Yes

answer: Yes

answer: No

answer: No

answer: No

answer: 1

text: Satellite experiments have found evidence of positrons and a few antiprotons in primary cosmic rays, amounting to less than 1% of the particles in primary cosmic rays. This antimatter cannot all have been created in the Big Bang, but is instead attributed to have been produced by cyclic processes at high energies.  For instance, electron-positron pairs may be formed in pulsars, as a magnetized neutron star rotation cycle shears electron-positron pairs from the star surface.  Therein the antimatter forms a wind which crashes upon the ejecta of the progenitor supernovae.  This weathering takes place as "the cold, magnetized relativistic wind launched by the star hits the non-relativistically expanding ejecta, a shock wave system forms in the impact: the outer one propagates in the ejecta, while a reverse shock propagates back towards the star." The former ejection of matter in the outer shock wave and the latter production of antimatter in the reverse shock wave are steps in a space weather cycle.

text: Satellite experiments have found evidence of

text: positron

text: s and a few antiprotons in primary cosmic rays, amounting to less than 1% of the particles in primary cosmic rays. This antimatter cannot all have been created in the Big Bang, but is instead attributed to have been produced by cyclic processes at high energies.  For instance, electron-positron pairs may be formed in

text: pulsar

text: s, as a magnetized neutron star rotation cycle shears electron-positron pairs from the star surface.  Therein the antimatter forms a wind which crashes upon the ejecta of the progenitor supernovae.  This weathering takes place as "the cold, magnetized relativistic wind launched by the star hits the non-relativistically expanding ejecta, a shock wave system forms in the impact: the outer one propagates in the ejecta, while a reverse shock propagates back towards the star." The former ejection of matter in the outer shock wave and the latter production of antimatter in the reverse shock wave are steps in a space weather cycle.

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answers: shock wave

answers: NDQ_006453

answers: Weathering

answers: NDQ_006455

answers: hit the non-relativistically expanding ejecta

answers: NDQ_006456

answers: cyclic

answers: NDQ_006457

answers: The outer one propagates in the ejecta, while a reverse shock propagates back towards the star

answers: NDQ_006458

answers: shock wave

answers: NDQ_006459

answers: supernovae

answers: NDQ_006460

answers: This antimatter cannot all have been created in the Big Bang

answers: NDQ_006461

answers: shock wave

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Built into the cavity is an array of ultrasonic transducers, which are used to create the separate standing-wave patterns at ultrasonic frequencies. As wind passes through the cavity, a change in the wave’s property occurs (phase shift). By measuring the amount of phase shift in the received signals by each transducer, and then by mathematically processing the data, the sensor is able to provide an accurate horizontal measurement of wind speed and direction.

text: Built into the cavity is an array of ultrasonic transducers, which are used to create the separate standing-wave patterns at ultrasonic frequencies. As wind passes through the cavity, a change in the wave’s property occurs (phase shift). By measuring the amount of phase shift in the received signals by each transducer, and then by mathematically processing the data, the sensor is able to provide an accurate horizontal measurement of wind speed and direction.

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answers: standing-wave patterns

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answers: standing-wave patterns

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answers: wind passes through the cavity

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answers: horizontal

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answers: As wind passes through the cavity

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answers: standing-wave patterns at ultrasonic frequencies

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answers: NDQ_006460

answers: As wind passes through the cavity

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answers: a change in the wave’s property occurs

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: Yes

answer: 1

text: A series of surface waves can be generated due to large-scale displacement of the ocean water. These can be caused by sub-marine landslides, seafloor deformations due to earthquakes, or the impact of a large meteorite.

text: A series of surface waves can be generated due to large-scale displacement of the ocean water. These can be caused by sub-marine

text: landslide

text: s, seafloor deformations due to

text: earthquake

text: s, or the impact of a large

text: meteorite

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answers: surface waves

answers: NDQ_006453

answers: surface waves

answers: NDQ_006455

answers: large-scale displacement of the ocean water

answers: NDQ_006456

answers: sub-marine

answers: NDQ_006457

answers: sub-marine

answers: NDQ_006458

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answers: NDQ_006459

answers: a large meteorite

answers: NDQ_006460

answers: surface waves

answers: NDQ_006461

answers: displacement of the ocean water

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The Billabong Pro Teahupo'o's reputation for wave riding is partly due to its unique form. An extremely shallow coral reef which ranges up to 20 inches beneath the waters surface is responsible for a very hollow-breaking wave. The wave's unique shape, with an effect of almost breaking below sea level, is due to the specific shape of the reef beneath the wave. Its semi circular nature which drops down sharply creates a 'below water' effect and the extreme angles in descent create an instant instability to the wave. A steep wall of reef causes the entire mass to fold onto a scalloped semi circle breaking arc. The wave bends and races along into a dry reef closeout and the lip of the wave is often as thick as it is tall. Therefore, resulting in the "Billabong Pro Teahupo’o being one of the deadliest big wave competitions in the world to this present date".

text: The Billabong Pro Teahupo'o's reputation for wave riding is partly due to its unique form. An extremely shallow coral reef which ranges up to 20 inches beneath the waters surface is responsible for a very hollow-breaking wave. The wave's unique shape, with an effect of almost breaking below sea level, is due to the specific shape of the reef beneath the wave. Its semi circular nature which drops down sharply creates a 'below water' effect and the extreme angles in descent create an instant instability to the wave. A steep wall of reef causes the entire mass to fold onto a scalloped semi circle breaking arc. The wave bends and races along into a dry reef closeout and the lip of the wave is often as thick as it is tall. Therefore, resulting in the "Billabong Pro Teahupo’o being one of the deadliest big wave competitions in the world to this present date".

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answers: An extremely shallow coral reef which ranges up to 20 inches beneath the waters surface

answers: NDQ_006453

answers: Teahupo'o

answers: NDQ_006455

answers: An extremely shallow coral reef

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answers: below water

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answers: The Billabong Pro Teahupo'o

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answers: The Billabong Pro Teahupo'o

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answers: reef

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answers: The wave's unique shape

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answers: shallow coral reef which ranges up to 20 inches beneath the waters surface

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The primary food sources of the waved albatross are fish, squid, and crustaceans, as well as smaller birds. But they have also been observed to scavenge for other food sources, including the regurgitated food of other birds. When foraging, the waved albatross finds places in the ocean where prey will be near this surface; this is the most effective way for the albatross to get its food. The waved albatrosses will forage  away from the place where the chicks are nesting to get food for them.

text: The primary food sources of the waved albatross are

text: fish

text: squid

text: , and

text: crustacean

text: s, as well as smaller birds. But they have also been observed to scavenge for other food sources, including the regurgitated food of other birds. When foraging, the waved albatross finds places in the ocean where prey will be near this surface; this is the most effective way for the albatross to get its food. The waved albatrosses will forage  away from the place where the chicks are nesting to get food for them.

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answers: waved albatross

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answers: scavenge

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answers: albatross

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answers: slow

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answers: surface

answers: NDQ_006458

answers: Waved albatross find places in the ocean where prey will be near this surface

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answers: albatross

answers: NDQ_006460

answers: shoreline

answers: NDQ_006461

answers: prey will be near this surface

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: A lineatus uses the shape of the waveform to determine distance by analyzing how much the waveform has changed since it was generated; this amount of change is extremely predictable and regular. The surface waveform has high frequencies near source, and lower frequencies farther away due to the dampening effect of the water surface; the amount of decrease diminishes with distance. A lineatus’ possible use of the wavefront’s curvature can be excluded since fish are still able to judge the distance of a wave’s source with only a single functioning neuromast when all others have been ablated. When presented with single-frequency or upward frequency-modulated waves, fish underestimate the distance of the wave source; this suggests the normal downward FM of capillary waves, which arises almost immediately in wave dispersion, is necessary for A lineatus to judge distance.  This was confirmed in 1982 by presenting fish with waves  with an artificially generated waveform so that at 7 cm the wave had the downward FM sweep of a wave 15 cm away, and fish responded to these by swimming 15 cm.

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answers: Waves break when they become too tall to be supported by their base

answers: NDQ_006453

answers: A lineatus uses the shape of the waveform

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answers: it was generated

answers: NDQ_006456

answers: downward

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answers: surface waveform has high frequencies near source, and lower frequencies farther away

answers: NDQ_006458

answers: The surface waveform has high frequencies near source

answers: NDQ_006459

answers: A lineatus

answers: NDQ_006460

answers: Wave dispersion

answers: NDQ_006461

answers: the normal downward FM of capillary waves, which arises almost immediately in wave dispersion

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: These waves break along or near a jetty. They are also called 'groynes' in some places. Examples include Long Beach in New York,  The Wedge in California, and Duranbah Groyne in Australia.

text: These waves break along or near a jetty. They are also called 'groynes' in some places. Examples include Long Beach in New York,

text: The Wedge

text: in California, and Duranbah Groyne in Australia.

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answers: 4

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answers: NDQ_006452

answers: The Wedge

answers: NDQ_006453

answers: Groyne

answers: NDQ_006455

answers: break

answers: NDQ_006456

answers: unsteady

answers: NDQ_006457

answers: surface

answers: NDQ_006458

answers: The Wedge

answers: NDQ_006459

answers: The Wedge

answers: NDQ_006460

answers: Groyne

answers: NDQ_006461

answers: groynes

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: An implosion shock wave might be of such short duration that only part of the pit is compressed at any instant as the wave passes through it. To prevent this, a pusher shell may be needed. The pusher is located between the explosive lens and the tamper. It works by reflecting some of the shock wave backwards, thereby having the effect of lengthening its duration. It is made out of a low density metal—such as aluminium, beryllium, or an alloy of the two metals (aluminium being easier and safer to shape, and is two orders of magnitude cheaper; beryllium for its high-neutron-reflective capability). Fat Man used an aluminium pusher.

text: An implosion shock wave might be of such short duration that only part of the pit is compressed at any instant as the wave passes through it. To prevent this, a pusher shell may be needed. The pusher is located between the explosive lens and the tamper. It works by reflecting some of the shock wave backwards, thereby having the effect of lengthening its duration. It is made out of a low

text: density

text: metal

text: —such as

text: aluminium

text: beryllium

text: , or an

text: alloy

text: of the two metals (aluminium being easier and safer to shape, and is two orders of magnitude cheaper; beryllium for its high-neutron-reflective capability). Fat Man used an aluminium pusher.

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answers: It is made out of a low density metal

answers: NDQ_006453

answers: pusher

answers: NDQ_006455

answers: implosion shock wave

answers: NDQ_006456

answers: forward

answers: NDQ_006457

answers: It is made out of a low density metal

answers: NDQ_006458

answers: It works by reflecting some of the shock wave backwards, thereby having the effect of lengthening its duration

answers: NDQ_006459

answers: tamper

answers: NDQ_006460

answers: It is made out of a low density metal

answers: NDQ_006461

answers: reflecting some of the shock wave backwards

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The effect of waves, while directly powered by the wind, is distinct from a storm's wind-powered currents. Powerful wind whips up large, strong waves in the direction of its movement. Although these surface waves are responsible for very little water transport in open water, they may be responsible for significant transport near the shore. When waves are breaking on a line more or less parallel to the beach, they carry considerable water shoreward. As they break, the water particles moving toward the shore have considerable momentum and may run up a sloping beach to an elevation above the mean water line which may exceed twice the wave height before breaking.

text: The effect of waves, while directly powered by the wind, is distinct from a storm's wind-powered currents. Powerful wind whips up large, strong waves in the direction of its movement. Although these surface waves are responsible for very little water transport in open water, they may be responsible for significant transport near the shore. When waves are breaking on a line more or less parallel to the beach, they carry considerable water shoreward. As they break, the water particles moving toward the shore have considerable momentum and may run up a sloping beach to an elevation above the mean water line which may exceed twice the wave height before breaking.

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answers: waves break when they become too tall to be supported by their base

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answers: surface waves

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answers: Powerful wind

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answers: momentum

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answers: As they break, the water particles moving toward the shore have considerable momentum

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answers: Powerful wind

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answers: shoreward

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answers: surface waves are responsible for very little water transport

answer: Yes

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answer: Yes

answer: Yes

answer: Yes

answer: 1

text: The first ocean wave models were developed in the 1960s and 1970s.  These models had the tendency to overestimate the role of wind in wave development and underplayed wave interactions.  A lack of knowledge concerning how waves interacted among each other, assumptions regarding a maximum wave height, and deficiencies in computer power limited the performance of the models.  After experiments were performed in 1968, 1969, and 1973, wind input from the Earth's atmosphere was weighted more accurately in the predictions.  A second generation of models was developed in the 1980s, but they could not realistically model swell nor depict wind-driven waves (also known as wind waves) caused by rapidly changing wind fields, such as those within tropical cyclones.  This caused the development of a third generation of wave models from 1988 onward.

text: The first

text: ocean wave models

text: were developed in the 1960s and 1970s.  These models had the tendency to overestimate the role of wind in wave development and underplayed wave interactions.  A lack of knowledge concerning how waves interacted among each other, assumptions regarding a maximum wave height, and deficiencies in computer power limited the performance of the models.  After experiments were performed in 1968, 1969, and 1973, wind input from the Earth's atmosphere was weighted more accurately in the predictions.  A second generation of models was developed in the 1980s, but they could not realistically model

text: swell

text: nor depict

text: wind-driven waves

text: (also known as wind waves) caused by rapidly changing wind fields, such as those within tropical cyclones.  This caused the development of a third generation of wave models from 1988 onward.

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answers: assumptions regarding a maximum wave height

answers: NDQ_006453

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answers: NDQ_006455

answers: wind

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answers: fast

answers: NDQ_006457

answers: Wave energy is lowest at the surface and increases with depth

answers: NDQ_006458

answers: Waves interacted among each other

answers: NDQ_006459

answers: rapidly changing wind fields

answers: NDQ_006460

answers: The first ocean wave models

answers: NDQ_006461

answers: wind input from the Earth's atmosphere

answer: Yes

answer: Yes

answer: No

answer: Yes

answer: Yes

answer: 1

text: Breaking the Waves was received as mainstream cinema, but in reality it was a kind of high budget experimental film. It had elaborated the chapter shots and used handheld camera in a sketchy raw style that followed the actors closely. Breaking the Waves marked an important change in focus. In von Trier's early films, the protagonist is a man, typically a disillusioned idealist whose downfall is furthered by a deceitful, fatal woman.  In this film, for the first time the protagonist is a woman, emotional and naive. This will continues in the following films: with the only exception of the comedy, The Boss of It All, all Trier's subsequent films have a female protagonist. Breaking the Waves controversially connects religion with eroticism. The film focuses on sexual perversity and female martyrdom, issues that will continue in Trier's later work and that have challenged critics and commentators, who see the self-sacrificing submissive heroine as basically a misogynist cliche.

text: Breaking the Waves was received as mainstream cinema, but in reality it was a kind of high budget experimental film. It had elaborated the chapter shots and used handheld camera in a sketchy raw style that followed the actors closely. Breaking the Waves marked an important change in focus. In von Trier's early films, the protagonist is a man, typically a disillusioned idealist whose downfall is furthered by a deceitful, fatal woman.  In this film, for the first time the protagonist is a woman, emotional and naive. This will continues in the following films: with the only exception of the comedy,

text: The Boss of It All

text: , all Trier's subsequent films have a female protagonist. Breaking the Waves controversially connects religion with eroticism. The film focuses on sexual perversity and female martyrdom, issues that will continue in Trier's later work and that have challenged critics and commentators, who see the self-sacrificing submissive heroine as basically a misogynist cliche.

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answers: breaking the waves

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answers: Waves

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answers: Breaking

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answers: high budget

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answers: Shoreline

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answers: handheld camera in a sketchy raw style

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: A shore break is a wave that breaks directly on, or very close to the shore. This happens when the beach is very steep at the shoreline. These waves are really just a form of beach or reef break, but breaking very close to the shore.

text: A shore break is a wave that breaks directly on, or very close to the

text: shore

text: . This happens when the beach is very steep at the shoreline. These waves are really just a form of beach or reef break, but breaking very close to the shore.

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answers: Shore break

answers: NDQ_006453

answers: reef break

answers: NDQ_006455

answers: beach is very steep

answers: NDQ_006456

answers: fast

answers: NDQ_006457

answers: Shore break

answers: NDQ_006458

answers: Shore break

answers: NDQ_006459

answers: reef

answers: NDQ_006460

answers: Shore break

answers: NDQ_006461

answers: steep at the shoreline

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Many wind instruments have some kind of flaring bell shape. These are generally not exponential in configuration, and are used to modify the standing wave patterns of the instrument, and thereby the musical notes which can be produced.

text: Many wind instruments have some kind of flaring bell shape. These are generally not exponential in configuration, and are used to modify the

text: standing wave

text: patterns of the instrument, and thereby the

text: musical note

text: s which can be produced.

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answers: exponential

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answers: bell shape

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answer: Yes

answer: Yes

answer: Yes

answer: No

answer: No

answer: 1

text: Jet streams are typically continuous over long distances, but discontinuities are common. The path of the jet typically has a meandering shape, and these meanders themselves propagate eastward, at lower speeds than that of the actual wind within the flow. Each large meander, or wave, within the jet stream is known as a Rossby wave (planetary wave). Rossby waves are caused by changes in the Coriolis effect with latitude. Shortwave troughs, are smaller scale waves superimposed on the Rossby waves, with a scale of  long, that move along through the flow pattern around large scale, or longwave, "ridges" and "troughs" within Rossby waves. Jet streams can split into two when it encounters an upper-level low, that diverts a portion of the jet stream under its base, while the remainder of the jet moves by to its north.

text: Jet streams are typically continuous over long distances, but discontinuities are common. The path of the jet typically has a meandering shape, and these meanders themselves propagate eastward, at lower speeds than that of the actual wind within the flow. Each large meander, or wave, within the jet stream is known as a

text: Rossby wave

text: (planetary wave). Rossby waves are caused by changes in the

text: Coriolis effect

text: with latitude.

text: Shortwave troughs

text: , are smaller scale waves superimposed on the Rossby waves, with a scale of  long, that move along through the flow pattern around large scale, or longwave, "ridges" and "troughs" within Rossby waves. Jet streams can split into two when it encounters an upper-level low, that diverts a portion of the jet stream under its base, while the remainder of the jet moves by to its north.

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answers: "ridges" and "troughs"

answers: NDQ_006453

answers: Jet streams

answers: NDQ_006455

answers: changes in the Coriolis effect

answers: NDQ_006456

answers: longwave

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answers: Coriolis effect with latitude

answers: NDQ_006459

answers: changes in the Coriolis effect

answers: NDQ_006460

answers: The path of the jet typically has a meandering shape

answers: NDQ_006461

answers: changes in the Coriolis effect with latitude

answer: No

answer: No

answer: Yes

answer: No

answer: No

answer: 1

text: When generated by light wind in open water, a nautical name for them is cat's paw waves, since they may resemble paw prints. Light breezes which stir up such small ripples are also sometimes referred to as cat's paws. On the open ocean, much larger ocean surface waves (seas and swells) may result from coalescence of smaller wind-caused ripple-waves.

text: When generated by light wind in open water, a nautical name for them is cat's paw waves, since they may resemble paw prints. Light breezes which stir up such small ripples are also sometimes referred to as cat's paws. On the open ocean, much larger

text: ocean surface wave

text: s (

text: seas

text: and

text: swell

text: s) may result from coalescence of smaller wind-caused ripple-waves.

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answers: larger ocean surface waves

answers: NDQ_006453

answers: swells

answers: NDQ_006455

answers: light breezes

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answers: unsteady

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answers: NDQ_006458

answers: Cat's paw waves

answers: NDQ_006459

answers: larger ocean surface waves

answers: NDQ_006460

answers: surface waves

answers: NDQ_006461

answers: cat's paw waves

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: 1

text: Storm surges caused by extratropical cyclones have been recorded along the coastal areas. These storm surges are formed from strong winds that blow towards the land. They are formed due to the interaction between the semi-permanent South Pacific High and a low pressure system over the Atlantic, southeast of Argentina, creating strong winds from the south or southwest. The sudestada, which brings the worst storm surges, occurs when there is a high pressure system over southern Argentina in the Atlantic Ocean that interacts with a low pressure over Uruguay and southern Brazil, causing strong winds from the southeast. Storm surges have caused flooding of coastal areas, leading to extensive property loss and other damage. It is also the main natural factor in the erosion of coastlines. The flooding as a result of storm surges are particularly destructive in flat coastal areas such as the Rio de La Plata shores, and the Salado Basin.

text: Storm surges caused by

text: extratropical cyclones

text: have been recorded along the coastal areas. These storm surges are formed from strong winds that blow towards the land. They are formed due to the interaction between the semi-permanent South Pacific High and a low pressure system over the Atlantic, southeast of Argentina, creating strong winds from the south or southwest. The sudestada, which brings the worst storm surges, occurs when there is a high pressure system over southern Argentina in the Atlantic Ocean that interacts with a low pressure over

text: Uruguay

text: and southern Brazil, causing strong winds from the southeast. Storm surges have caused flooding of coastal areas, leading to extensive property loss and other damage. It is also the main natural factor in the

text: erosion of coastlines

text: . The flooding as a result of storm surges are particularly destructive in flat coastal areas such as the

text: Rio de La Plata

text: shores, and the

text: Salado Basin

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answers: It is also the main natural factor in the erosion of coastlines

answers: NDQ_006453

answers: Storm surge

answers: NDQ_006455

answers: strong winds that blow towards the land

answers: NDQ_006456

answers: south or southwest

answers: NDQ_006457

answers: Surface wave energy is lowest at the surface and increases with depth

answers: NDQ_006458

answers: It is also the main natural factor in the erosion of coastlines

answers: NDQ_006459

answers: The sudestada

answers: NDQ_006460

answers: Storm surges caused by extratropical cyclones

answers: NDQ_006461

answers: low pressure

answer: Yes

answer: Yes

answer: No

answer: No

answer: No

answer: 1

text: In mid-June a change in the jet stream over a large part of the Pacific Ocean caused an increase in tropical wave frequency. One of these waves would become the precursor to Olga. The wave was first noticed near the Marshall Islands, particularly the Island of Majuro on June 24. As it moved west weather satellites depicted the wave had begun to organize with considerable convection and spiraling storm bands as it neared the Central Caroline Islands. Due to the waves close proximity to a high pressure area to the north, strong easterlies accelerated it to the west. The increased forward speed inhibited the establishment of a circulation until it was south of Guam early on June 29, though the JMA had classified it a tropical depression two days earlier. Later that day reconnaissance had detected a closed center and gale force winds and the low was upgraded to a tropical storm and was given the name Olga. As it entered the Philippine Sea the ridge that had kept it to the south began to weaken allowing Olga to move in a northwestward direction. Moving into an increasingly favorable environment, the storm slowed in its forward speed, and strengthened into a typhoon late on June 29. Rapid intensification followed as the system bottomed out at a pressure of  and winds of 160 mph (260 km/h) on July 1. The strengthening happened within a little over a day brought it to a super typhoon, the first of the season. The 62 millibar drop with the day of June 30 and July 1 caused a very high wind profile around the six mile radius eye. The storm followed a break in the ridge and moved northward while weakening gradually. While passing to the east of Taiwan a short wave from the Chinese mainland caused a sharp direction change in Olga's path. A low developed in the wake of the short wave, dominated Olga causing the typhoon to greatly weaken. Dry air soon entered the circulation caused a shallowing in the systems overall convection. By July 5 Olga made landfall on the Kansai region, south of Osaka, as a tropical storm. The system continued into the Sea of Japan, and became merged within a cold front. The remaining low tracked over South Korea before completely dissipating on July 7.

text: In mid-June a change in the jet stream over a large part of the Pacific Ocean caused an increase in tropical wave frequency. One of these waves would become the precursor to Olga. The wave was first noticed near the

text: Marshall Islands

text: , particularly the Island of

text: Majuro

text: Kansai region

text: , south of

text: Osaka

text: , as a tropical storm. The system continued into the Sea of Japan, and became merged within a cold front. The remaining low tracked over South Korea before completely dissipating on July 7.

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answers: 0

answers: NDQ_006452

answers: Taiwan

answers: NDQ_006453

answers: Guam

answers: NDQ_006455

answers: a change in the jet stream

answers: NDQ_006456

answers: forward

answers: NDQ_006457

answers: Taiwan

answers: NDQ_006458

answers: Taiwan

answers: NDQ_006459

answers: typhoon

answers: NDQ_006460

answers: Philippine Sea

answers: NDQ_006461

answers: Taiwan

answer: No

answer: No

answer: Yes

answer: No

answer: No

answer: 1

text: As Ike crossed Cuba on September 8 it weakened to Category 1 and emerged into the Caribbean Sea, where it moved along the southern coast.  Ike killed 7 people in Cuba, having traversed nearly the entirety of the island nation.  It crossed into the Gulf of Mexico on September 9 and ballooned in size. Ike maintained a double eyewall structure across most of the Gulf of Mexico and continued to expand in size. It made landfall on Galveston Island on September 13 as a strong Category 2 hurricane, but its large size brought a storm surge of over  from Galveston Island eastward into southern Louisiana. The Bolivar Peninsula was worst affected by the surge, while Galveston Island (where waves topped the seawall) and the Port Arthur areas also saw extensive damage. Power was knocked out to most of the Houston area and windows were blown out of skyscrapers in downtown Houston. As Ike moved inland, it brought extensive flooding and wind damage throughout the Midwest and as far north as Pennsylvania. Ike was categorized extratropical on September 14.

text: As Ike crossed Cuba on September 8 it weakened to Category 1 and emerged into the

text: Caribbean Sea

text: , where it moved along the southern coast.  Ike killed 7 people in Cuba, having traversed nearly the entirety of the island nation.  It crossed into the Gulf of Mexico on September 9 and ballooned in size. Ike maintained a double

text: eyewall

text: structure across most of the Gulf of Mexico and continued to expand in size. It made landfall on

text: Galveston Island

text: on September 13 as a strong Category 2 hurricane, but its large size brought a storm surge of over  from Galveston Island eastward into southern

text: Louisiana

text: . The

text: Bolivar Peninsula

text: was worst affected by the surge, while Galveston Island (where waves topped the

text: seawall

text: ) and the

text: Port Arthur

text: areas also saw extensive damage. Power was knocked out to most of the

text: Houston

text: area and windows were blown out of skyscrapers in

text: downtown Houston

text: . As Ike moved inland, it brought extensive flooding and wind damage throughout the

text: Midwest

text: and as far north as

text: Pennsylvania

text: . Ike was categorized extratropical on September 14.

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answers: 3: The answer has limited relevance and completeness, with noticeable gaps or inaccuracies.

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answers: NDQ_006452

answers: waves topped the seawall

answers: NDQ_006453

answers: storm surge

answers: NDQ_006455

answers: Category 2 hurricane

answers: NDQ_006456

answers: slow

answers: NDQ_006457

answers: Ike maintained a double eyewall structure across most of the Gulf of Mexico and continued to expand in size

answers: NDQ_006458

answers: The Bolivar Peninsula

answers: NDQ_006459

answers: storm surge

answers: NDQ_006460

answers: Waves topped the seawall

answers: NDQ_006461

answers: Because the bottle is floating on top of the water.

answer: No

answer: Yes

answer: No

answer: No

answer: No

answer: 1

text: A swell, in the context of an ocean, sea or lake, is a series of mechanical waves that propagate along the interface between water and air and so they are often referred to as surface gravity waves. These series of surface gravity waves are not generated by the immediate local wind, instead by distant weather systems, where wind blows for a duration of time over a fetch of water. This is the primary definition of a swell as opposed to a locally generated wind wave, which is still under the influence of the mechanisms that created it e.g. wind blowing over a puddle. More generally, a swell consists of wind-generated waves that are not—or are hardly—affected by the local wind at that time. Swell waves often have a long wavelength but this varies due to the size,  strength and duration of the weather system responsible for the swell and the size of the water body e.g. wavelengths are rarely more than 150 m in the Mediterranean . Swell wavelength, also, varies from event to event. Occasionally, swells which are longer than 700 m occur as a result of the most severe storms. Swells have a narrower range of  frequencies and directions than locally generated wind waves, because swell waves have dispersed from their generation area, have dissipated and therefore lost an amount of randomness, taking on a more defined shape and direction. Swell direction is the direction from which the swell is coming. It is measured in degrees (as on a compass), and often referred to in general directions, such as a NNW or SW swell.

text: A swell, in the context of an ocean, sea or lake, is a series of

text: mechanical waves

text: that propagate along the interface between water and air and so they are often referred to as

text: surface gravity waves

text: . These series of surface gravity waves are not generated by the immediate

text: local wind

text: , instead by distant weather systems, where wind blows for a duration of time over a

text: fetch

text: of water. This is the primary definition of a swell as opposed to a locally generated wind wave, which is still under the influence of the mechanisms that created it e.g. wind blowing over a puddle. More generally, a swell consists of wind-generated waves that are not—or are hardly—affected by the local wind at that time. Swell waves often have a long

text: wavelength

text: but this varies due to the size,  strength and duration of the weather system responsible for the swell and the size of the water body e.g. wavelengths are rarely more than 150 m in the Mediterranean . Swell wavelength, also, varies from event to event. Occasionally, swells which are longer than 700 m occur as a result of the most severe storms. Swells have a narrower range of

text: frequencies

text: and directions than locally generated wind waves, because swell waves have dispersed from their generation area, have

text: dissipated

text: and therefore lost an amount of randomness, taking on a more defined shape and direction. Swell direction is the direction from which the swell is coming. It is measured in degrees (as on a compass), and often referred to in general directions, such as a NNW or SW swell.

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answers: surface gravity waves

answers: NDQ_006453

answers: puddle

answers: NDQ_006455

answers: wind blows

answers: NDQ_006456

answers: gravity

answers: NDQ_006457

answers: surface gravity waves

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answers: surface gravity waves

answers: NDQ_006459

answers: severe storms

answers: NDQ_006460

answers: surface gravity waves

answers: NDQ_006461

answers: surface gravity waves

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: It doesn't break often, requiring huge swells from the Southern Ocean, but these can produce very large waves often in excess of 40 ft with some contending for the biggest wave in Australia at over 60 ft.

text: It doesn't break often, requiring huge swells from the

text: Southern Ocean

text: , but these can produce very large waves often in excess of 40 ft with some contending for the biggest wave in Australia at over 60 ft.

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answers: Wave energy is lowest at the surface

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answers: Australia

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answers: swells

answer: No

answer: No

answer: No

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answer: 1

text: The storm surge, or the increase in sea level due to the cyclone, is typically the worst effect from landfalling tropical cyclones, historically resulting in 90% of tropical cyclone deaths.  The relatively quick surge in sea level can move miles/kilometers inland, flooding homes and cutting off escape routes.  The storm surges and winds of hurricanes may be destructive to human-made structures, but they also stir up the waters of coastal estuaries, which are typically important fish breeding locales.

text: The

text: storm surge

text: , or the increase in sea level due to the cyclone, is typically the worst effect from landfalling tropical cyclones, historically resulting in 90% of tropical cyclone deaths.  The relatively quick surge in sea level can move miles/kilometers inland, flooding homes and cutting off escape routes.  The storm surges and winds of hurricanes may be destructive to human-made structures, but they also stir up the waters of coastal estuaries, which are typically important fish breeding locales.

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answers: NDQ_006452

answers: The storm surge

answers: NDQ_006453

answers: storm surge

answers: NDQ_006455

answers: hurricanes

answers: NDQ_006456

answers: fast

answers: NDQ_006457

answers: The relatively quick surge in sea level

answers: NDQ_006458

answers: Friction with the shore

answers: NDQ_006459

answers: hurricanes

answers: NDQ_006460

answers: land

answers: NDQ_006461

answers: stir up the waters

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: On August 15, 2011, a tropical wave exited the west African coast, and emerged into the Atlantic, characterized by distinct low-level cyclonic rotation and deep tropical humidity. It remained well-defined while moving steadily westward for several days to the south of the Cape Verde Islands, although at the time any notable convection occurred well to the southwest of its axis. As the wave distanced itself from the islands, development of thunderstorms and showers in its proximity continued to remain scarce, and it became rather broad in appearance. On August 19, the convective structure began to show signs of organization as the associated atmospheric pressure lowered, and with a progressively favorable environment situated ahead of the wave its chances of undergoing tropical cyclogenesis markedly increased. The strong thunderstorm activity continued to become more pronounced around the main low-pressure feature. By August 20, the National Hurricane Center noted that tropical cyclone formation was imminent as the wave neared the Lesser Antilles, and a reconnaissance aircraft confirmed the presence of a small surface circulation center just southwest of a burst of vigorous convection and unusually high sustained winds, indicating sufficient organization for the cyclone to be upgraded into Tropical Storm Irene at 23:00 UTC that day.

text: On August 15, 2011, a

text: tropical wave

text: exited the west African coast, and emerged into the

text: Atlantic

text: , characterized by distinct low-level

text: cyclonic rotation

text: and deep tropical humidity. It remained well-defined while moving steadily westward for several days to the south of the

text: Cape Verde Islands

text: , although at the time any notable

text: convection

text: occurred well to the southwest of its axis. As the wave distanced itself from the islands, development of thunderstorms and showers in its proximity continued to remain scarce, and it became rather broad in appearance. On August 19, the convective structure began to show signs of organization as the associated

text: atmospheric pressure

text: lowered, and with a progressively favorable environment situated ahead of the wave its chances of undergoing

text: tropical cyclogenesis

text: markedly increased. The strong thunderstorm activity continued to become more pronounced around the main

text: low-pressure feature

text: . By August 20, the

text: National Hurricane Center

text: noted that

text: tropical cyclone

text: formation was imminent as the wave neared the

text: Lesser Antilles

text: , and a

text: reconnaissance aircraft

text: confirmed the presence of a small surface circulation center just southwest of a burst of vigorous convection and unusually high

text: sustained winds

text: , indicating sufficient organization for the cyclone to be upgraded into Tropical Storm Irene at 23:00

text: UTC

text: that day.

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text: Surfing waves break along a sand bank that extends from Snapper Rocks through Rainbow Bay, past Greenmount point and Coolangatta, then to Kirra. This region has been called the Superbank.

text: Surfing waves break along a sand bank that extends from

text: Snapper Rocks

text: through

text: Rainbow Bay

text: , past Greenmount point and

text: Coolangatta

text: , then to Kirra. This region has been called the Superbank.

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answer: No

answer: No

answer: No

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text: Dolphins sometimes ride on the bow waves created by boats or surf on naturally breaking waves.

text: Dolphins sometimes ride on the

text: bow wave

text: s created by boats or surf on naturally breaking waves.

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answers: naturally

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answers: bow waves

answers: NDQ_006455

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answers: NDQ_006456

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answers: NDQ_006457

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answers: NDQ_006458

answers: Bow waves

answers: NDQ_006459

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answers: NDQ_006460

answers: shoreline

answers: NDQ_006461

answers: naturally breaking waves

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: In continuum mechanics, wave turbulence is a set of nonlinear waves deviated far from thermal equilibrium. Such a state is usually accompanied by dissipation. It is either decaying turbulence or requires an external source of energy to sustain it. Examples are waves on a fluid surface excited by winds or ships, and waves in plasma excited by electromagnetic waves etc.

text: In

text: continuum mechanics

text: , wave turbulence is a set of

text: nonlinear

text: wave

text: s deviated far from

text: thermal equilibrium

text: . Such a state is usually accompanied by

text: dissipation

text: . It is either

text: decaying turbulence

text: or requires an external source of

text: energy

text: to sustain it. Examples are waves on a

text: fluid surface

text: excited by

text: wind

text: s or

text: ship

text: s, and waves in

text: plasma

text: excited by

text: electromagnetic waves

text: etc.

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answers: NDQ_006459

answers: 0

answers: NDQ_006460

answers: 0

answers: NDQ_006461

answers: 0

answers: NDQ_006452

answers: dissipation

answers: NDQ_006453

answers: turbulence

answers: NDQ_006455

answers: an external source of energy

answers: NDQ_006456

answers: fluid

answers: NDQ_006457

answers: Wave turbulence

answers: NDQ_006458

answers: dissipation

answers: NDQ_006459

answers: winds or ships

answers: NDQ_006460

answers: waves on a fluid surface

answers: NDQ_006461

answers: requires an external source of energy to sustain it

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: 1

text: Since the late 1960s when Gordon Clark found the optimum formulation of urethane foam, many of the surfboards in common use have been of the shortboard variety between 6 feet and 7 feet in length with a pointed nose and a rounded or squarish tail, typically with three "skegs" (fins) but sometimes with two or as many as five. Surfers generally find a shortboard quick to maneuver compared with other types of surfboards, but because of a lack of flotation due to the smaller size, the shortboard is harder to catch waves with, often requiring steeper, larger and more powerful waves and very late takeoffs, where the surfer catches the wave at the critical moment before it breaks.

text: Since the late 1960s when Gordon Clark found the optimum formulation of urethane foam, many of the surfboards in common use have been of the shortboard variety between 6 feet and 7 feet in length with a pointed nose and a rounded or squarish tail, typically with three "skegs" (fins) but sometimes with two or as many as five. Surfers generally find a shortboard quick to maneuver compared with other types of surfboards, but because of a lack of flotation due to the smaller size, the shortboard is harder to catch waves with, often requiring steeper, larger and more powerful waves and very late takeoffs, where the surfer catches the wave at the critical moment before it breaks.

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answers: larger and more powerful waves

answers: NDQ_006453

answers: Waves

answers: NDQ_006455

answers: at the critical moment before it breaks

answers: NDQ_006456

answers: steeper

answers: NDQ_006457

answers: steeper, larger and more powerful waves

answers: NDQ_006458

answers: lack of flotation

answers: NDQ_006459

answers: Surfers

answers: NDQ_006460

answers: Waves

answers: NDQ_006461

answers: lack of flotation

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: When waves travel into areas of shallow water, they begin to be affected by the ocean bottom.  The free orbital motion of the water is disrupted, and water particles in orbital motion no longer return to their original position.  As the water becomes shallower, the swell becomes higher and steeper, ultimately assuming the familiar sharp-crested wave shape.  After the wave breaks, it becomes a wave of translation and erosion of the ocean bottom intensifies.

text: When

text: waves

text: travel into areas of shallow water, they begin to be affected by the

text: ocean

text: bottom.  The free

text: orbital motion

text: of the water is disrupted, and water particles in orbital motion no longer return to their original position.  As the water becomes shallower, the swell becomes higher and steeper, ultimately assuming the familiar sharp-crested wave shape.  After the

text: wave breaks

text: , it becomes a wave of translation and erosion of the ocean bottom intensifies.

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answers: When waves travel into areas of shallow water

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answers: shallow water

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answers: When waves travel into areas of shallow water

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answers: orbital

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answers: As the water becomes shallower

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answers: After the wave breaks, it becomes a wave of translation

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answers: shallow water

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answers: After the wave breaks

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answers: water particles in orbital motion no longer return to their original position

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The Wave-dancers are a tribe of elves who took refuge in the oceans of the World of Two Moons.  Thanks to elfin flesh-shaping magic, the Wave-dancers have in some cases undergone physical alterations such as fins and fish-like tails to help them adapt to an aquatic life.

text: The Wave-dancers are a tribe of elves who took refuge in the oceans of the World of Two Moons.  Thanks to elfin flesh-shaping magic, the Wave-dancers have in some cases undergone physical alterations such as fins and fish-like tails to help them adapt to an aquatic life.

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answers: Wave-dancers

answers: NDQ_006453

answers: Wave

answers: NDQ_006455

answers: oceans

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answers: oceans

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answers: Wave-dancers

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answers: Wave-dancers

answers: NDQ_006460

answers: aquatic

answers: NDQ_006461

answers: fins

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: In physics, the wavelength of a sinusoidal wave is the spatial period of the wave—the distance over which the wave's shape repeats, and thus the inverse of the spatial frequency. It is usually determined by considering the distance between consecutive corresponding points of the same phase, such as crests, troughs, or zero crossings and is a characteristic of both traveling waves and standing waves, as well as other spatial wave patterns. Wavelength is commonly designated by the Greek letter lambda (λ). The concept can also be applied to periodic waves of non-sinusoidal shape. The term wavelength is also sometimes applied to modulated waves, and to the sinusoidal envelopes of modulated waves or waves formed by interference of several sinusoids.

text: In

text: physics

text: , the wavelength of a

text: sinusoidal wave

text: is the spatial period of the wave—the distance over which the wave's shape repeats, and thus the

text: inverse

text: of the

text: spatial frequency

text: . It is usually determined by considering the distance between consecutive corresponding points of the same

text: phase

text: , such as crests, troughs, or

text: zero crossing

text: s and is a characteristic of both traveling waves and

text: standing wave

text: s, as well as other spatial wave patterns. Wavelength is commonly designated by the

text: Greek letter

text: lambda

text: (λ). The concept can also be applied to periodic waves of non-sinusoidal shape. The term wavelength is also sometimes applied to

text: modulated

text: waves, and to the sinusoidal

text: envelopes

text: of modulated waves or waves formed by

text: interference

text: of several sinusoids.

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answers: standing waves

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answers: standing waves

answers: NDQ_006455

answers: interference of several sinusoids

answers: NDQ_006456

answers: traveling

answers: NDQ_006457

answers: The term wavelength is also sometimes applied to modulated waves

answers: NDQ_006458

answers: standing waves

answers: NDQ_006459

answers: interference of several sinusoids

answers: NDQ_006460

answers: is a characteristic of both traveling waves and standing waves

answers: NDQ_006461

answers: inverse of the spatial frequency

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Kelvin waves have been connected to El Niño (beginning in the Northern Hemisphere winter months) in recent years in terms of precursors to this atmospheric and oceanic phenomenon.  Many scientists have utilized coupled atmosphere–ocean models to simulate an El Niño Southern Oscillation (ENSO) event and have stated that the Madden–Julian oscillation (MJO) can trigger oceanic Kelvin waves throughout its 30- to 60-day cycle or the latent heat of condensation can be released (from intense convection) resulting in Kelvin waves as well; this process can then signal the onset of an El Niño event.  The weak low pressure in the Indian Ocean (due to the MJO) typically propagates eastward into the North Pacific Ocean and can produce easterly winds.  These easterly winds can transfer West Pacific warm water toward the east, thereby exciting a Kelvin wave, which in this sense can be thought of as a warm-water anomaly that travels under the ocean’s surface at a depth of about 150 meters.  This wave can be observed at the surface by a slight rise in sea surface height of about 8 cm (associated with  a depression of the thermocline) and an SST increase that covers hundreds of square miles across the surface of the ocean.

text: Kelvin waves have been connected to El Niño (beginning in the Northern Hemisphere winter months) in recent years in terms of precursors to this atmospheric and oceanic phenomenon.  Many scientists have utilized coupled atmosphere–ocean models to simulate an

text: El Niño Southern Oscillation

text: (ENSO) event and have stated that the

text: Madden–Julian oscillation

text: (MJO) can trigger oceanic Kelvin waves throughout its 30- to 60-day cycle or the latent heat of condensation can be released (from intense convection) resulting in Kelvin waves as well; this process can then signal the onset of an El Niño event.  The weak low pressure in the

text: Indian Ocean

text: (due to the MJO) typically propagates eastward into the

text: North Pacific Ocean

text: and can produce easterly winds.  These easterly winds can transfer

text: West Pacific

text: warm water toward the east, thereby exciting a Kelvin wave, which in this sense can be thought of as a warm-water anomaly that travels under the ocean’s surface at a depth of about 150 meters.  This wave can be observed at the surface by a slight rise in sea surface height of about 8 cm (associated with  a depression of the thermocline) and an

text: SST

text: increase that covers hundreds of square miles across the surface of the ocean.

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answers: Kelvin waves

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answers: Kelvin wave

answers: NDQ_006455

answers: the Madden–Julian oscillation

answers: NDQ_006456

answers: Kelvin

answers: NDQ_006457

answers: Kelvin waves

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answers: Kelvin waves

answers: NDQ_006459

answers: latent heat of condensation

answers: NDQ_006460

answers: Kelvin waves

answers: NDQ_006461

answers: Kelvin waves

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Ocean swells form from the longer term amalgamation of wind-generated waves on the surface. The stronger the wind and the longer the area over which it blows, generally the larger the swell.

text: Ocean swells form from the longer term amalgamation of wind-generated waves on the surface. The stronger the wind and the longer the area over which it blows, generally the larger the swell.

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answers: NDQ_006453

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answers: 0

answers: NDQ_006457

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answers: NDQ_006459

answers: 4

answers: NDQ_006460

answers: 4

answers: NDQ_006461

answers: 0

answers: NDQ_006452

answers: The stronger the wind

answers: NDQ_006453

answers: swell

answers: NDQ_006455

answers: wind

answers: NDQ_006456

answers: faster

answers: NDQ_006457

answers: surface

answers: NDQ_006458

answers: Wind-generated waves

answers: NDQ_006459

answers: wind

answers: NDQ_006460

answers: surface

answers: NDQ_006461

answers: wind-generated waves

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: 1

text: The wave characteristics of "the Point" have long been considered world-class, and include: a remarkably easy paddle out; a machine-like, jacking, perfect almond-shaped tube (particularly when >4 feet) and which has reportedly held waves up to 15 feet (Hawaiian scale-that's ~30 feet wave faces) since the earthquake; and a sculptured wave face which is partially smoothed out by a weak 'reverse current'- which sucks water from the bay into the wave and acts to 'smooths out' the breaking wave face, even under light onshore wind conditions.

text: The wave characteristics of "the Point" have long been considered world-class, and include: a remarkably easy paddle out; a machine-like, jacking, perfect almond-shaped tube (particularly when >4 feet) and which has reportedly held waves up to 15 feet (Hawaiian scale-that's ~30 feet wave faces) since the earthquake; and a sculptured wave face which is partially smoothed out by a weak 'reverse current'- which sucks water from the bay into the wave and acts to 'smooths out' the breaking wave face, even under light onshore wind conditions.

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answers: NDQ_006460

answers: 4

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answers: NDQ_006452

answers: breaking wave face

answers: NDQ_006453

answers: reverse current

answers: NDQ_006455

answers: breaking

answers: NDQ_006456

answers: reverse

answers: NDQ_006457

answers: Wave energy is lowest at the surface

answers: NDQ_006458

answers: "the Point" have long been considered world-class

answers: NDQ_006459

answers: earthquake

answers: NDQ_006460

answers: onshore

answers: NDQ_006461

answers: sucks water from the bay into the wave

answer: Yes

answer: Yes

answer: No

answer: No

answer: Yes

answer: 1

text: About 2.6 million Cubans, a fourth of the population was evacuated ahead of Ike. In Baracoa, 200 homes were reported to be destroyed and waves were running  high and peaked at  in different areas of Cuba. The Category 4 hurricane made landfall on September 8 on the north coast of eastern Cuba in the province of Holguín near Puerto de Sama, with sustained winds of about , causing widespread flooding and damage to the eastern provinces. It passed across the central provinces of Holguín, Las Tunas, and Camagüey, emerging over the sea to the south of Cuba during the day. Ike dropped to Category One intensity by the time it crossed the island. It then followed the southern coast of Cuba and crossed the western end of the island in Pinar del Río Province, close to the path taken by Hurricane Gustav ten days previously. The western areas of Cuba, already devastated by just 10 days before Ike hit, suffered additional major flooding from the rain and storm surge. The sugar cane crop was devastated, with over  destroyed. The banana, yucca, coffee and corn crop also suffered significant damage. Alongside Gustav, they were described as the "worst ever" storms by Cuban officials.

text: About 2.6 million Cubans, a fourth of the population was evacuated ahead of Ike. In

text: Baracoa

text: , 200 homes were reported to be destroyed and waves were running  high and peaked at  in different areas of Cuba. The Category 4 hurricane made landfall on September 8 on the north coast of eastern Cuba in the province of

text: Holguín

text: near Puerto de Sama, with sustained winds of about , causing widespread flooding and damage to the eastern provinces. It passed across the central provinces of Holguín, Las Tunas, and Camagüey, emerging over the sea to the south of Cuba during the day. Ike dropped to Category One intensity by the time it crossed the island. It then followed the southern coast of Cuba and crossed the western end of the island in

text: Pinar del Río Province

text: , close to the path taken by

text: Hurricane Gustav

text: ten days previously. The western areas of Cuba, already devastated by just 10 days before Ike hit, suffered additional major flooding from the rain and storm surge. The

text: sugar cane

text: crop was devastated, with over  destroyed. The

text: banana

text: yucca

text: coffee

text: and

text: corn

text: crop also suffered significant damage. Alongside Gustav, they were described as the "worst ever" storms by Cuban officials.

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answers: NDQ_006452

answers: Category 4 hurricane

answers: NDQ_006453

answers: storm surge

answers: NDQ_006455

answers: Category 4 hurricane

answers: NDQ_006456

answers: fast

answers: NDQ_006457

answers: waves are running high and peaked at in different areas of Cuba

answers: NDQ_006458

answers: waves are running high and peaked at in different areas of Cuba

answers: NDQ_006459

answers: Category 4 hurricane

answers: NDQ_006460

answers: landfall

answers: NDQ_006461

answers: Category 4 hurricane

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: 1

text: For the specific case of predicting wind wave statistics on the ocean, the term ocean surface wave model is used.

text: For the specific case of predicting wind wave statistics on the ocean, the term ocean surface wave model is used.

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text: In many cases the medium in which the wave propagates does not permit a direct observation of the true form. In these cases, the term "waveform" refers to the shape of a graph of the varying quantity against time. An instrument called an oscilloscope can be used to pictorially represent a wave as a repeating image on a screen.

text: In many cases the medium in which the wave propagates does not permit a direct

text: observation

text: of the true form. In these cases, the term "waveform" refers to the shape of a graph of the varying quantity against time. An instrument called an

text: oscilloscope

text: can be used to pictorially represent a wave as a repeating image on a

text: screen

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answers: Waves do not permit a direct observation of the true form

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answer: No

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answer: 1

text: A Kelvin wave is any progressive wave that is channeled between two boundaries or opposing forces (usually between the Coriolis force and a coastline or the equator). There are two types, coastal and equatorial. Kelvin waves are gravity driven and non-dispersive. This means that Kelvin waves can retain their shape and direction over long periods of time. They are usually created by a sudden shift in the wind, such as the change of the trade winds at the beginning of the El Niño-Southern Oscillation.

text: A

text: Kelvin wave

text: is any

text: progressive wave

text: that is channeled between two boundaries or opposing forces (usually between the

text: Coriolis force

text: and a

text: coastline

text: or the

text: equator

text: ). There are two types, coastal and equatorial. Kelvin waves are

text: gravity

text: driven and

text: non-dispersive

text: . This means that Kelvin waves can retain their shape and direction over long periods of time. They are usually created by a sudden shift in the wind, such as the change of the

text: trade wind

text: s at the beginning of the

text: El Niño-Southern Oscillation

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answers: Kelvin waves

answers: NDQ_006453

answers: Kelvin waves are gravity driven and non-dispersive

answers: NDQ_006455

answers: Kelvin waves are gravity driven and non-dispersive

answers: NDQ_006456

answers: gravity driven

answers: NDQ_006457

answers: Kelvin waves

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answers: Kelvin waves are gravity driven

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answers: a sudden shift in the wind

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answers: Kelvin wave

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answers: gravity driven and non-dispersive

answer: Yes

answer: Yes

answer: No

answer: No

answer: No

answer: 1

text: The term marine energy encompasses both wave power i.e. power from surface waves, and tidal power i.e. obtained from the kinetic energy of large bodies of moving water. Offshore wind power is not a form of marine energy, as wind power is derived from the wind, even if the wind turbines are placed over water.The oceans have a tremendous amount of energy and are close to many if not most concentrated populations. Ocean energy has the potential of providing a substantial amount of new renewable energy around the world.

text: The term marine energy encompasses both

text: wave power

text: i.e. power from surface waves, and

text: tidal power

text: i.e. obtained from the kinetic energy of large bodies of moving water.

text: Offshore wind power

text: is not a form of marine energy, as wind power is derived from the wind, even if the

text: wind turbine

text: s are placed over water.The oceans have a tremendous amount of energy and are close to many if not most concentrated populations. Ocean energy has the potential of providing a substantial amount of new

text: renewable energy

text: around the world.

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answers: surface waves

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answers: Tidal power

answers: NDQ_006455

answers: kinetic energy

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answers: kinetic energy

answers: NDQ_006457

answers: surface waves

answers: NDQ_006458

answers: Tidal power

answers: NDQ_006459

answers: surface waves

answers: NDQ_006460

answers: surface waves

answers: NDQ_006461

answers: surface waves

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The interaction of two trains of surface waves of different frequencies and directions generates wave groups. For wave propagating almost in the same direction, this gives the usual sets of waves that travel at the group speed, which is slower than phase speed of water waves (see animation). For typical ocean waves with a period around 10 seconds, this group speed is close to 10 m/s.

text: The interaction of two trains of

text: surface waves

text: of different frequencies and directions generates

text: wave group

text: s. For wave propagating almost in the same direction, this gives the usual sets of waves that travel at the group speed, which is slower than phase speed of water waves (see animation). For typical ocean waves with a period around 10 seconds, this

text: group speed

text: is close to 10 m/s.

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text: Wind-wave dissipation or "swell dissipation" is process in which a wave generated via a weather system loses its mechanical energy transferred from the atmosphere via wind. Wind waves, as their name suggests, are generated by wind transferring energy from the atmosphere to the ocean's surface, capillary gravity waves play an essential role in this effect, "wind waves" or "swell" are also known as surface gravity waves.

text: Wind-wave dissipation or "

text: swell dissipation

text: " is process in which a wave generated via a weather system loses its

text: mechanical

text: energy transferred from the atmosphere via wind. Wind waves, as their name suggests, are generated by wind transferring energy from the atmosphere to the ocean's surface,

text: capillary gravity waves

text: play an essential role in this effect, "wind waves" or "swell" are also known as

text: surface gravity wave

text: s.

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answer: Yes

answer: Yes

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answer: 1

text: The Storm of the Century, also known as the Great Blizzard of 1993, was a large cyclonic storm that formed over the Gulf of Mexico on March 12, 1993, and dissipated in the North Atlantic Ocean on March 15. It is unique for its intensity, massive size and wide-reaching effect. At its height, the storm stretched from Canada towards Central America, but its main impact was on the Eastern United States and Cuba. The cyclone moved through the Gulf of Mexico, and then through the Eastern United States before moving into Canada. Areas as far south as central Alabama and Georgia received  of snow and areas such as Birmingham, Alabama, received up to  with isolated reports of . Even the Florida Panhandle reported up to , with hurricane-force wind gusts and record low barometric pressures. Between Louisiana and Cuba, hurricane-force winds produced high storm surges across northwestern Florida, which along with scattered tornadoes killed dozens of people. Record cold temperatures were seen across portions of the South and East in the wake of this storm. In the United States, the storm was responsible for the loss of electric power to over 10 million customers. It is purported to have been directly experienced by nearly 40 percent of the country's population at that time. A total of 310 people, including 10 from Cuba, perished during this storm.

text: The

text: Storm of the Century

text: , also known as the Great Blizzard of 1993, was a large

text: cyclonic

text: storm that formed over the

text: Gulf of Mexico

text: on March 12, 1993, and dissipated in the North Atlantic Ocean on March 15. It is unique for its intensity, massive size and wide-reaching effect. At its height, the storm stretched from Canada towards Central America, but its main impact was on the Eastern United States and Cuba. The cyclone moved through the Gulf of Mexico, and then through the Eastern United States before moving into Canada. Areas as far south as central Alabama and Georgia received  of snow and areas such as

text: Birmingham, Alabama

text: , received up to  with isolated reports of . Even the

text: Florida Panhandle

text: reported up to , with

text: hurricane-force

text: wind gusts and record low

text: barometric pressure

text: s. Between Louisiana and Cuba, hurricane-force winds produced high storm surges across northwestern Florida, which along with scattered

text: tornado

text: es killed dozens of people. Record cold temperatures were seen across portions of the South and East in the wake of this storm. In the United States, the storm was responsible for the loss of

text: electric power

text: to over 10 million customers. It is purported to have been directly experienced by nearly 40 percent of the country's population at that time. A total of 310 people, including 10 from Cuba, perished during this storm.

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answers: The Storm of the Century

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answer: Yes

answer: Yes

answer: No

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answer: 1

text: Most people think of waves as a surface phenomenon, which acts between water (as in lakes or oceans) and the air. Where low density water overlies high density water in the ocean, internal waves propagate along the boundary. They are especially common over the continental shelf regions of the world oceans and where brackish water overlies salt water at the outlet of large rivers. There is typically little surface expression of the waves, aside from slick bands that can form over the trough of the waves.

text: Most people think of waves as a surface phenomenon, which acts between water (as in lakes or oceans) and the air. Where low density water overlies high density water in the

text: ocean

text: , internal waves propagate along the boundary. They are especially common over the

text: continental shelf

text: regions of the world oceans and where

text: brackish

text: water overlies salt water at the outlet of large rivers. There is typically little surface expression of the waves, aside from slick bands that can form over the trough of the waves.

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answers: There is typically little surface expression of the waves

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answers: brackish water

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answers: low density water overlies high density water

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answers: trough

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answers: There is typically little surface expression

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answers: There is typically little surface expression

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answers: rivers

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answers: Where low density water overlies high density water in the ocean

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answers: There is typically little surface expression of the waves

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: While everyday wind waves have a wavelength (from crest to crest) of about  and a height of roughly , a tsunami in the deep ocean has a much larger wavelength of up to . Such a wave travels at well over , but owing to the enormous wavelength the wave oscillation at any given point takes 20 or 30 minutes to complete a cycle and has an amplitude of only about . This makes tsunamis difficult to detect over deep water, where ships are unable to feel their passage.

text: While everyday

text: wind wave

text: s have a

text: wavelength

text: (from crest to crest) of about  and a height of roughly , a tsunami in the deep ocean has a much larger wavelength of up to . Such a wave travels at well over , but owing to the enormous wavelength the wave oscillation at any given point takes 20 or 30 minutes to complete a cycle and has an amplitude of only about . This makes tsunamis difficult to detect over deep water, where ships are unable to feel their passage.

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answers: crest

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answers: tsunami

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answers: wind

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answers: well over

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answers: waves travels at well over

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answers: has an amplitude of only about

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answers: deep ocean

answers: NDQ_006460

answers: Wave travels at well over

answers: NDQ_006461

answers: waves have a wavelength

answer: Yes

answer: No

answer: Yes

answer: Yes

answer: Yes

answer: 1

text: Once every five or six years, a tropical storm, accompanied by very high and potentially damaging winds and heavy rain, will strike the region. About once every 11 or 12 years a hurricane brings damaging winds and storm surges to the region. Several Category 3 storms have struck Cape Cod since record-keeping began, such as the Long Island Express of 1938 and the 1944 Great Atlantic hurricane. Strong Category 2 storms, such as Hurricane Carol of 1954 and Hurricane Bob of 1991 also caused considerable damage. Notable Category 1 storms include Hurricane Edna of 1954 (shortly following Hurricane Carol) and Hurricane Donna of 1960, also Hurricane Irene in 2011, and Hurricane Sandy in 2012. Other notable storms include the Gale of 1815, which would likely have been rated a strong hurricane on the Saffir-Simpson scale, and the so-called "Perfect Storm" of October 31, 1991. The February 2013 nor'easter produced winds in excess of  and dropped over  of snow on some parts of Cape Cod. The storm knocked out power to tens of thousands of Cape Cod residents, some for up to two weeks.

text: Once every five or six years, a

text: tropical storm

text: , accompanied by very high and potentially damaging winds and heavy rain, will strike the region. About once every 11 or 12 years a

text: hurricane

text: brings damaging winds and

text: storm surge

text: s to the region. Several

text: Category 3

text: storms have struck Cape Cod since record-keeping began, such as the

text: Long Island Express

text: of 1938 and the

text: 1944 Great Atlantic hurricane

text: . Strong

text: Category 2

text: storms, such as

text: Hurricane Carol

text: of 1954 and

text: Hurricane Bob

text: of 1991 also caused considerable damage. Notable

text: Category 1

text: storms include

text: Hurricane Edna

text: of 1954 (shortly following

text: Hurricane Carol

text: ) and

text: Hurricane Donna

text: of 1960, also

text: Hurricane Irene

text: in 2011, and

text: Hurricane Sandy

text: in 2012. Other notable storms include the

text: Gale of 1815

text: , which would likely have been rated a strong hurricane on the Saffir-Simpson scale, and the so-called "

text: Perfect Storm

text: " of October 31, 1991. The

text: February 2013 nor'easter

text: produced winds in excess of  and dropped over  of snow on some parts of Cape Cod. The storm knocked out power to tens of thousands of Cape Cod residents, some for up to two weeks.

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text: The surf zone is place of convergence of multiple waves types creating complex wave patterns. A wave suitable for surfing results from maximum speeds of 5 meters per second. This speed is relative because local onshore winds can cause waves to break. In the surf zone, shallow water waves are carried by global winds to the beach and interact with local winds to make surfing waves.

text: The surf zone is place of convergence of multiple waves types creating complex wave patterns. A wave suitable for surfing results from maximum speeds of 5 meters per second. This speed is relative because local onshore winds can cause waves to break. In the surf zone, shallow water waves are carried by global winds to the beach and interact with local winds to make surfing waves.

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answers: local onshore winds

answers: NDQ_006453

answers: shallow water

answers: NDQ_006455

answers: local onshore winds

answers: NDQ_006456

answers: relative

answers: NDQ_006457

answers: shallow water waves

answers: NDQ_006458

answers: Break

answers: NDQ_006459

answers: global winds

answers: NDQ_006460

answers: global winds

answers: NDQ_006461

answers: shallow water waves are carried by global winds

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: Yes

answer: 1

text: Since the demonstrations of wave-like properties in photons and electrons, similar experiments have been conducted with neutrons and protons. Among the most famous experiments are those of Estermann and Otto Stern in 1929.Authors of similar recent experiments with atoms and molecules, described below, claim that these larger particles also act like waves. A wave is basically a group of particles which moves in a particular form of motion, i.e. to and fro. If we break that flow by an object it will convert into radiants.

text: Since the demonstrations of wave-like properties in

text: photon

text: s and

text: electron

text: s, similar experiments have been conducted with

text: neutron

text: s and

text: proton

text: s. Among the most famous experiments are those of

text: Estermann

text: and

text: Otto Stern

text: in 1929.Authors of similar recent experiments with atoms and molecules, described below, claim that these larger particles also act like waves. A wave is basically a group of particles which moves in a particular form of motion, i.e. to and fro. If we break that flow by an object it will convert into radiants.

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answers: larger particles also act like waves

answers: NDQ_006453

answers: Sea level rise

answers: NDQ_006455

answers: If we break that flow by an object

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answers: It will convert into radiants

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answers: Break that flow by an object it will convert into radiants

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answers: It will convert into radiants

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answers: break that flow by an object

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Surfing waves can be analyzed using the following parameters: breaking wave height, wave peel angle (α), wave breaking intensity, and wave section length. The breaking wave height has two measurements, the relative heights estimated by surfers and the exact measurements done by physical oceanographers. Measurements done by surfers were 1.36 to 2.58 times higher than the measurements done by scientists. The scientifically concluded wave heights that are physically possible to surf are 1 to 20 meters.

text: Surfing waves can be analyzed using the following parameters: breaking wave height, wave peel angle (α), wave breaking intensity, and wave section length. The breaking wave height has two measurements, the relative heights estimated by surfers and the exact measurements done by physical oceanographers. Measurements done by surfers were 1.36 to 2.58 times higher than the measurements done by scientists. The scientifically concluded wave heights that are physically possible to surf are 1 to 20 meters.

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answers: Surfing

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answers: wave peel angle

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Three main types of breaking waves are identified by surfers or surf lifesavers. Their varying characteristics make them more or less suitable for surfing, and present different dangers.

text: Three main types of breaking waves are identified by

text: surfer

text: s or

text: surf lifesavers

text: . Their varying characteristics make them more or less suitable for surfing, and present different dangers.

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answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The Blizzard of ‘88 was one of the worst storm to ever strike the eastern seaboard. It started on Sunday morning, March 11, 1888 and the storm continued to rage until Monday midnight. Although there was only about two or three feet of snow, gale force winds that reached 60 MPH left snowdrifts as high as 10’ to 20’. During the storm, a rare “blowout tide,” (extreme ebbs caused by strong offshore winds which drain inshore shallows - the opposite of a storm-surge), drained the Rondout Creek enough that boats were grounded on the creek bottom. The ferry boat was hard aground and the Norwich was keeled over to one side. The stage to Ellenville left the Rondout at the usual time but nothing was heard from the stage the next day. The only thing authorities could do was assume that the stage was stuck in the snow someplace and that the passengers were safe. The stage from Ellenville reached Hurley that Monday and stayed until the next day when the driver returned to Rondout with only one sleigh bob.

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answers: NDQ_006452

answers: “blowout tide”

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answers: “blowout tide”

answers: NDQ_006455

answers: Sunday morning

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answers: blowout

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answers: Blizzard of ‘88

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answers: Blizzard of ‘88

answers: NDQ_006459

answers: gale force winds

answers: NDQ_006460

answers: “blowout tide”

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answers: extreme ebbs

answer: No

answer: Yes

answer: No

answer: No

answer: No

answer: 1

text: In the Atlantic, a tropical wave spawned Tropical Depression Six. Twenty four hours later, wind shear degenerated the depression back into a wave. The wave continued westward, and in the southern Caribbean Sea, split in two on August 21. The southern part crossed Central America and emerged into the Pacific Ocean. Banding and convection steadily organized, and Tropical Depression Fifteen-E formed on August 27. It strengthened into Tropical Storm Lorena the next day. At this time, three systems were active and in close proximity. Lorena and a weakening Kiko started a Fujiwhara interaction. Lorena eventually became the dominate system, and absorbed the remnants of Kiko on August 29. Moving slowly out to sea, Lorena reached minimal hurricane strength on the September 1 as the convection became more concentrated. Lorena was a hurricane for less than a day. It weakened quickly to a depression on September 3. The cyclone was devoid of convection by September 7, and was thus declared a remnant low. The system never affected land.

text: In the

text: Atlantic

text: , a

text: tropical wave

text: spawned Tropical Depression Six. Twenty four hours later,

text: wind shear

text: degenerated the depression back into a wave. The wave continued westward, and in the southern

text: Caribbean Sea

text: , split in two on August 21. The southern part crossed Central America and emerged into the Pacific Ocean. Banding and convection steadily organized, and Tropical Depression Fifteen-E formed on August 27. It strengthened into Tropical Storm Lorena the next day. At this time, three systems were active and in close proximity. Lorena and a weakening Kiko started a

text: Fujiwhara interaction

text: . Lorena eventually became the dominate system, and absorbed the remnants of Kiko on August 29. Moving slowly out to sea, Lorena reached minimal hurricane strength on the September 1 as the convection became more concentrated. Lorena was a hurricane for less than a day. It weakened quickly to a depression on September 3. The cyclone was devoid of convection by September 7, and was thus declared a remnant low. The system never affected land.

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answers: NDQ_006452

answers: split in two

answers: NDQ_006453

answers: Tropical Depression

answers: NDQ_006455

answers: tropical wave

answers: NDQ_006456

answers: slow

answers: NDQ_006457

answers: surface

answers: NDQ_006458

answers: degenerated the depression

answers: NDQ_006459

answers: tropical depression

answers: NDQ_006460

answers: never affected land

answers: NDQ_006461

answers: wind shear

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: No

answer: 1

text: Hurricane Howard began as a tropical wave that moved off the west coast of Africa on August 18. The wave moved across the Atlantic Ocean and Caribbean Sea with little associated convection. By August 26, the wave produced disorganized convection as it moved through the western Caribbean, across Central America, and entered the eastern Pacific Ocean. Paralleling the southern coast of Mexico, the wave became increasingly organized and it was estimated that the tropical wave spawned a tropical depression around 1200 UTC on August 30 about 400 mi (645 km) south-southwest of Acapulco, Mexico. Classified as Tropical Depression Eleven-E, the system tracked west-northwestward under the steering currents of a weak mid-level ridge. In the hours after formation, the depression lacked a concentration of deep convection near the center. However, conditions favored eventual development, including warm sea surface temperatures and low amounts of wind shear.

text: Hurricane Howard began as a

text: tropical wave

text: that moved off the west coast of Africa on August 18. The wave moved across the Atlantic Ocean and

text: Caribbean Sea

text: with little associated

text: convection

text: . By August 26, the wave produced disorganized convection as it moved through the western Caribbean, across Central America, and entered the eastern Pacific Ocean. Paralleling the southern coast of Mexico, the wave became increasingly organized and it was estimated that the tropical wave spawned a

text: tropical depression

text: around 1200

text: UTC

text: on August 30 about 400 mi (645 km) south-southwest of

text: Acapulco

text: , Mexico. Classified as Tropical Depression Eleven-E, the system tracked west-northwestward under the steering currents of a weak mid-level

text: ridge

text: . In the hours after formation, the depression lacked a concentration of deep convection near the center. However, conditions favored eventual

text: development

text: , including warm

text: sea surface temperatures

text: and low amounts of

text: wind shear

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answers: Deep convection

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answers: low amounts of wind shear

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answers: It moved across the Atlantic Ocean

answers: NDQ_006461

answers: low amounts of wind shear

answer: No

answer: Yes

answer: No

answer: No

answer: No

answer: 1

text: Wind speed is affected by a number of factors and situations, operating on varying scales (from micro to macro scales). These include the pressure gradient, Rossby waves and jet streams, and local weather conditions. There are also links to be found between wind speed and wind direction, notably with the pressure gradient and terrain conditions.

text: Wind speed is affected by a number of factors and situations, operating on varying scales (from micro to macro scales). These include the pressure gradient, Rossby waves and

text: jet stream

text: s, and local weather conditions. There are also links to be found between wind speed and

text: wind direction

text: , notably with the pressure gradient and terrain conditions.

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answers: Rossby waves

answers: NDQ_006453

answers: Rossby waves

answers: NDQ_006455

answers: pressure gradient

answers: NDQ_006456

answers: jet streams

answers: NDQ_006457

answers: surface

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answers: Rossby waves

answers: NDQ_006459

answers: jet streams

answers: NDQ_006460

answers: Rossby

answers: NDQ_006461

answers: Rossby waves

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: 1

text: This type of structure can be used to create a metamaterial surface with the intended application of artificial magnetic conductors or applications for boundary conditions. Another application is as stop band device for surface wave propagation along the interface. This is because surface waves are a created as a consequence of an interface between two media having dissimilar refractive indices. Depending on the application of the system that includes the two media, there may be a need to attenuate surface waves or utilize them.

text: This type of structure can be used to create a metamaterial surface with the intended application of artificial magnetic conductors or applications for

text: boundary conditions

text: . Another application is as

text: stop band

text: device for

text: surface wave

text: propagation along the interface. This is because surface waves are a created as a consequence of an interface between two media having dissimilar

text: refractive indices

text: . Depending on the application of the system that includes the two media, there may be a need to attenuate surface waves or utilize them.

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text: Most surfboards intended for larger waves are longer (to increase hull speed for paddling, wave-catching, and surfing), and as most shapers orient the rail fins toward the nose of the board, a longer board inherently results in reduced toe-in of rail fins, therefore less negative angle of attack, less oscillation, greater stability, and higher speeds. Rail fins also typically have some degree of "cant," that is, are tilted out toward the rail they are adjacent to. This is a significant additional factor in lift at various attitudes, drag, and performance, as are the variables of other foils - including flexibility, thickness, and planform.  Rail fins evolved into being and surged into popularity as riders (Simon Anderson, most famously) sought a solution to two major performance issues of a central "single" fin - both related to engagement of the foil: For one, a centrally-mounted fin is tilted up out of the water as the board is leaned over, and thus it loses more and more of its lift as the lean angle increases - if the lean angle is acute enough, the fin's tip can be the only area left in the water; the tip may then rapidly stall and, having lost its lift, become disengaged from the water, leaving the board's bottom as the only control surface still operating. Before rail fins became (extremely) popular, this tendency of "single fins" led to riders "nursing" turns - this tendency was a significant limiting factor on performance. The enhanced hold offered by rail fins during turning led to more types of maneuvers being possible. The other major issue leading to rail fins' use is the fact that a rider can use the lift near the rail to increase speed and performance on smaller waves due to the above effects and abilities of these foils.

text: Most surfboards intended for larger waves are longer (to increase hull speed for paddling, wave-catching, and surfing), and as most shapers orient the rail fins toward the nose of the board, a longer board inherently results in reduced toe-in of rail fins, therefore less negative

text: angle of attack

text: , less oscillation, greater stability, and higher speeds. Rail fins also typically have some degree of "cant," that is, are tilted out toward the rail they are adjacent to. This is a significant additional factor in lift at various attitudes, drag, and performance, as are the variables of other foils - including flexibility, thickness, and

text: planform

text: .  Rail fins evolved into being and surged into popularity as riders (

text: Simon Anderson

text: , most famously) sought a solution to two major performance issues of a central "single" fin - both related to engagement of the foil: For one, a centrally-mounted fin is tilted up out of the water as the board is leaned over, and thus it loses more and more of its lift as the lean angle increases - if the lean angle is acute enough, the fin's tip can be the only area left in the water; the tip may then rapidly

text: stall

text: and, having lost its lift, become disengaged from the water, leaving the board's bottom as the only control surface still operating. Before rail fins became (extremely) popular, this tendency of "single fins" led to riders "nursing" turns - this tendency was a significant limiting factor on performance. The enhanced hold offered by rail fins during turning led to more types of maneuvers being possible. The other major issue leading to rail fins' use is the fact that a rider can use the lift near the rail to increase speed and performance on smaller waves due to the above effects and abilities of these foils.

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text: Ride the Winds, Break the Waves (Chinese: 乘风破浪) is a 2017 Chinese drama film directed by Han Han and starring Deng Chao, Eddie Peng, Zhao Liying and Dong Zijian.

text: Ride the Winds, Break the Waves (

text: Chinese

text: : 乘风破浪) is a 2017 Chinese

text: drama film

text: directed by

text: Han Han

text: and starring

text: Deng Chao

text: Eddie Peng

text: Zhao Liying

text: and Dong Zijian.

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text: where the atomic scattering factor in a partial wave expansion with partial wave phase-shifts δ is given by

text: where the atomic scattering factor in a partial wave expansion with partial wave phase-shifts δ is given by

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text: Ombak Tujuh (meaning "Seven Waves") is a "big-wave" spot. It is more closely related to Western Australia's Margaret River than other machine-like Indonesian waves. It's left-hand reef with a feathering, shifting, barreling take-off and a long reeling wall. It's considered to be the best wave along the Ujung Genteng peninsula, primarily because it's a wave magnet. Local geography cycles predominant winds around to blow offshore, too. But the wave's raw exposure to several swell directions makes for shifty conditions. Bigger boards are recommended just to ease yourself into these things. One of the most difficult aspects of the wave is reaching it, either by boat or by a long and winding road.

text: Ombak Tujuh (meaning "Seven Waves") is a "big-wave" spot. It is more closely related to

text: Western Australia

text: 's

text: Margaret River

text: than other machine-like Indonesian waves. It's left-hand

text: reef

text: with a feathering, shifting, barreling take-off and a long reeling wall. It's considered to be the best wave along the Ujung Genteng

text: peninsula

text: , primarily because it's a wave magnet. Local geography cycles predominant winds around to blow offshore, too. But the wave's raw exposure to several swell directions makes for shifty conditions. Bigger boards are recommended just to ease yourself into these things. One of the most difficult aspects of the wave is reaching it, either by boat or by a long and winding road.

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text: Last in the series of break, the Peak is found. It is located right at the base of the cave, making this the entry and exit point of Uluwatu. The Peak operates well at every tide stage. Coming in best at high tide this wave makes for many hallow barreling waves. Unlike high tide, low tide at the Peak is known for closing out. The peak has a reef break. Winds from the southeast make the most ideal waves. It is key to have a board the size of 6’8-7’4 while surfing this wave.

text: Last in the series of break, the Peak is found. It is located right at the base of the cave, making this the entry and exit point of Uluwatu. The Peak operates well at every tide stage. Coming in best at high tide this wave makes for many hallow barreling waves. Unlike high tide, low tide at the Peak is known for closing out. The peak has a reef break. Winds from the southeast make the most ideal waves. It is key to have a board the size of 6’8-7’4 while surfing this wave.

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answers: low tide

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answers: tide

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answers: slow

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answers: high tide

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answers: Shoreline

answers: NDQ_006461

answers: low tide

answer: Yes

answer: Yes

answer: No

answer: Yes

answer: No

answer: 1

text: Bombie is the first of the five breaks in the Uluwatu series, located on the outer reef. Well known for breaking boards and snapping leashes, Bombie is an extremely powerful wave. On bigger swell days the wave can reach up to 20 feet. With fairly consistent surf year round, the best time is from May to October. This is the dry season with southeast winds. The typical surf arises from groundswells, coming in with a southwest swell direction. Bombie has a left breaking reef.

text: Bombie is the first of the five breaks in the Uluwatu series, located on the outer

text: reef

text: . Well known for breaking boards and snapping leashes, Bombie is an extremely powerful wave. On bigger swell days the wave can reach up to 20 feet. With fairly consistent surf year round, the best time is from May to October. This is the

text: dry season

text: with southeast winds. The typical surf arises from groundswells, coming in with a southwest swell direction. Bombie has a left breaking reef.

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answers: NDQ_006452

answers: On bigger swell days

answers: NDQ_006453

answers: groundswells

answers: NDQ_006455

answers: groundswells

answers: NDQ_006456

answers: southwest

answers: NDQ_006457

answers: The typical surf arises from groundswells

answers: NDQ_006458

answers: Groundswells

answers: NDQ_006459

answers: groundswells

answers: NDQ_006460

answers: Wave

answers: NDQ_006461

answers: swell direction

answer: No

answer: Yes

answer: No

answer: No

answer: No

answer: 1

text: Three different types of wind waves develop over time:

text: Three different types of wind waves develop over time:

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answers: 2: The answer has limited relevance and completeness, with significant gaps or inaccuracies.

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answers: 2: The answer has limited relevance and completeness, with significant gaps or inaccuracies.

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answers: 4

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answers: NDQ_006452

answers: They break when they become too tall.

answers: NDQ_006453

answers: Sea level rise

answers: NDQ_006455

answers: wind

answers: NDQ_006456

answers: unsteady

answers: NDQ_006457

answers: Surface waves have less energy.

answers: NDQ_006458

answers: Friction with the shore

answers: NDQ_006459

answers: wind

answers: NDQ_006460

answers: Waves travel across the ocean

answers: NDQ_006461

answers: wind waves develop over time

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: Yes

answer: 1

text: The atmosphere and ocean are continuously stratified: potential density generally increases steadily downward. Internal waves in a continuously stratified medium may propagate vertically as well as horizontally. The dispersion relation for such waves is curious: For a freely-propagating internal wave packet, the direction of propagation of energy (group velocity) is perpendicular to the direction of propagation of wave crests and troughs (phase velocity). An internal wave may also become confined to a finite region of altitude or depth, as a result of varying stratification or wind. Here, the wave is said to be ducted or trapped, and a vertically standing wave may form, where the vertical component of group velocity approaches zero. A ducted internal wave mode may propagate horizontally, with parallel group and phase velocity vectors, analogous to propagation within a waveguide.

text: The atmosphere and ocean are continuously stratified:

text: potential density

text: generally increases steadily downward. Internal waves in a continuously stratified medium may propagate vertically as well as horizontally. The

text: dispersion relation

text: for such waves is curious: For a freely-propagating internal wave

text: packet

text: , the direction of propagation of energy (

text: group velocity

text: ) is perpendicular to the direction of propagation of wave crests and troughs (

text: phase velocity

text: ). An internal wave may also become confined to a finite region of

text: altitude

text: or depth, as a result of varying stratification or

text: wind

text: . Here, the wave is said to be ducted or trapped, and a vertically

text: standing wave

text: may form, where the vertical component of

text: group velocity

text: approaches zero. A ducted internal wave mode may

text: propagate

text: horizontally, with parallel

text: group

text: and

text: phase velocity

text: vectors

text: , analogous to

text: propagation

text: within a

text: waveguide

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answers: vertically standing wave may form

answers: NDQ_006453

answers: stratification or wind

answers: NDQ_006455

answers: potential density generally increases steadily downward

answers: NDQ_006456

answers: horizontally

answers: NDQ_006457

answers: potential density generally increases steadily downward

answers: NDQ_006458

answers: The vertical component of group velocity approaches zero

answers: NDQ_006459

answers: ducting

answers: NDQ_006460

answers: The atmosphere and ocean are continuously stratified

answers: NDQ_006461

answers: potential density generally increases steadily downward

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: There is now general agreement that the annual component of polar motion is a forced motion excited predominantly by atmospheric dynamics. There exist two external forces to excite polar motion: atmospheric winds, and pressure loading. The main component is pressure forcing, which is a standing wave of the form:

text: There is now general agreement that the annual component of polar motion is a forced motion excited predominantly by atmospheric dynamics. There exist two external forces to excite polar motion: atmospheric winds, and pressure loading. The main component is pressure forcing, which is a standing wave of the form:

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answers: standing wave

answer: No

answer: No

answer: No

answer: No

answer: No

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text: The cold wave that merged with Hurricane Sandy at the end of October, 2012 brought strong winds and high waves across the Great Lakes. Lake Michigan recorded wave heights of 20 to 22 feet and wind gusts of 60 to 70 mph. The southern end of Lake Michigan experienced a lake level rise of 15 inches as the winds pushed water down the lake.  Lake Huron experienced 23-foot waves and a wind gust of 74 mph was recorded at Fort Gratiot at the southern end of the lake. Most freighters stayed in harbor instead of trying to run through the storm.

text: The cold wave that merged with

text: Hurricane Sandy

text: at the end of October, 2012 brought strong winds and high waves across the Great Lakes. Lake Michigan recorded wave heights of 20 to 22 feet and wind gusts of 60 to 70 mph. The southern end of Lake Michigan experienced a lake level rise of 15 inches as the winds pushed water down the lake.  Lake Huron experienced 23-foot waves and a wind gust of 74 mph was recorded at Fort Gratiot at the southern end of the lake. Most freighters stayed in harbor instead of trying to run through the storm.

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answers: Lake Michigan

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answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: 1

text: Hawaiians would carefully select one of three types of trees. The trees included the koa (Acacia koa), ulu (Artocarpus altilis), and wiliwili (Erythrina sandwicensis) trees. Once selected, the surfer would dig the tree out and place fish in the hole as an offering to the gods. Selected craftsmen of the community were then hired to shape, stain, and prepare the board for the surfer. There were three primary shapes: the olo, kikoo, and the alaia. The olo is thick in the middle and gradually gets thinner towards the edges. The kikoo ranges in length from  and requires great skill to maneuver. The alaia board is around  long and requires great skill to ride and master. Aside from the preparatory stages prior to entering the water, the most skilled surfers were and pastors,[please clarify] including chiefs and warriors that surfed amongst the best waves on the island. These upper class Hawaiians gained respect through their enduring ability to master the waves and this art the Hawaiians referred to as surfing.Some ancient sites still popular today include Kahaluu Bay and Holualoa Bay.

text: Hawaiians would carefully select one of three types of trees. The trees included the koa (

text: Acacia koa

text: ), ulu (

text: Artocarpus altilis

text: ), and

text: wiliwili

text: (Erythrina sandwicensis) trees. Once selected, the surfer would dig the tree out and place fish in the hole as an offering to the gods. Selected craftsmen of the community were then hired to shape, stain, and prepare the board for the surfer. There were three primary shapes: the olo, kikoo, and the

text: alaia

text: . The olo is thick in the middle and gradually gets thinner towards the edges. The kikoo ranges in length from  and requires great skill to maneuver. The alaia board is around  long and requires great skill to ride and master. Aside from the preparatory stages prior to entering the water, the most skilled surfers were and pastors,[please clarify] including chiefs and warriors that surfed amongst the best waves on the island. These upper class Hawaiians gained respect through their enduring ability to master the waves and this art the Hawaiians referred to as surfing.Some ancient sites still popular today include

text: Kahaluu Bay

text: and

text: Holualoa Bay

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answers: the alaia board

answers: NDQ_006453

answers: waves

answers: NDQ_006455

answers: water

answers: NDQ_006456

answers: slow

answers: NDQ_006457

answers: The olo

answers: NDQ_006458

answers: The kikoo ranges in length from and requires great skill to maneuver

answers: NDQ_006459

answers: chiefs and warriors

answers: NDQ_006460

answers: The olo

answers: NDQ_006461

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answer: No

answer: No

answer: No

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answer: 1

text: Two different measures are used for storm tide and storm surge measurements. Storm tide is measured using a geodetic vertical datum (NGVD 29 or NAVD 88). Since storm surge is defined as the rise of water beyond what would be expected by the normal movement due to tides, storm surge is measured using tidal predictions, with the assumption that the tide prediction is well-known and only slowly varying in the region subject to the surge. Since tides are a localized phenomenon, storm surge can only be measured in relationship to a nearby tidal station. Tidal bench mark information at a station provides a translation from the geodetic vertical datum to mean sea level (MSL) at that location, then subtracting the tidal prediction yields a surge height above the normal water height.

text: Two different measures are used for storm tide and storm surge measurements. Storm tide is measured using a

text: geodetic

text: vertical datum (

text: NGVD 29

text: or

text: NAVD 88

text: ). Since storm surge is defined as the rise of water beyond what would be expected by the normal movement due to tides, storm surge is measured using tidal predictions, with the assumption that the tide prediction is well-known and only slowly varying in the region subject to the surge. Since tides are a localized phenomenon, storm surge can only be measured in relationship to a nearby tidal station. Tidal bench mark information at a station provides a translation from the geodetic vertical datum to

text: mean sea level (MSL)

text: at that location, then subtracting the tidal prediction yields a surge height above the normal water height.

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answers: NDQ_006459

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answers: NDQ_006460

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answers: NDQ_006461

answers: 0

answers: NDQ_006452

answers: surge height above the normal water height

answers: NDQ_006453

answers: storm surge

answers: NDQ_006455

answers: Tides

answers: NDQ_006456

answers: vertical

answers: NDQ_006457

answers: Tides are a localized phenomenon

answers: NDQ_006458

answers: Tidal prediction

answers: NDQ_006459

answers: storm surge

answers: NDQ_006460

answers: Tides

answers: NDQ_006461

answers: normal movement due to tides

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The Bolivar Peninsula was just to the right of landfall, placing it on the strong side of the hurricane. H Wind reconstructions (Powell et al., 1998) show winds blowing strongly from offshore-to-onshore for most of the storm, which acted to increase both surge and waves. Surge is extremely important for the particular case of the Bolivar Peninsula, as it allowed large waves to penetrate inland into areas they could not otherwise have reached. Shoreline erosion was around 75 m, which undermined the piled foundations of oceanfront buildings. Most other houses in this area were reduced to either piles or slabs by large waves riding on surge, with only a very few remaining more or less intact. Peak coastal surges reached . Water depths of at least  covered all of the Bolivar Peninsula, with most areas covered by at least  of water (not including wave action). Much of the southern part of Chambers County was also inundated by at least  of water. According to post-storm analyses by both the National Oceanic and Atmospheric Administration’s (NOAA) Hurricane Research Division and Applied Research Associates (ARA), a research and engineering company, the best estimates of 3-second peak wind gusts along the eastern portion of the peninsula were between 110 mph and 115 mph. Research observations also suggest most of eastern and southeastern Texas was subjected to tropical storm and hurricane-force winds for ten hours, and possibly longer.

text: The Bolivar Peninsula was just to the right of landfall, placing it on the strong side of the hurricane. H Wind reconstructions (Powell et al., 1998) show winds blowing strongly from offshore-to-onshore for most of the

text: storm

text: , which acted to increase both

text: surge

text: and

text: wave

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answers: NDQ_006452

answers: Waves break when they become too tall to be supported by their base

answers: NDQ_006453

answers: Surge

answers: NDQ_006455

answers: waves riding on surge

answers: NDQ_006456

answers: offshore

answers: NDQ_006457

answers: Water depths

answers: NDQ_006458

answers: Shoreline erosion

answers: NDQ_006459

answers: Surge

answers: NDQ_006460

answers: Shoreline erosion

answers: NDQ_006461

answers: small waves

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: 1

text: When the rail line to Point Richmond was complete, Ocean Wave began service as a ferry.  The first trip occurred on July 6, 1900, when Ocean Wave departed from the Ferry Building in San Francisco, and reached Point Richmond 40 minutes later, where passengers and baggage were transferred to an eastbound Santa Fe train, which would be the first ever to reachnChicago over an entirely Santa Fe-owned right of way.  In charge of Ocean Wave on this trip were Capt. John Lauritzen as master and Chief Engineer Ed Mahoney.

text: When the rail line to Point Richmond was complete, Ocean Wave began service as a ferry.  The first trip occurred on July 6, 1900, when Ocean Wave departed from the

text: Ferry Building

text: in San Francisco, and reached Point Richmond 40 minutes later, where passengers and baggage were transferred to an eastbound Santa Fe train, which would be the first ever to reachn

text: Chicago

text: over an entirely Santa Fe-owned right of way.  In charge of Ocean Wave on this trip were Capt. John Lauritzen as master and Chief Engineer Ed Mahoney.

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text: On the offshore Guanaja island, waters rose about  during the storm. The combination of storm surge and high winds severely damaged offshore islands. High waves eroded northern coastlines and damaged lagoons. Most of the Bay Islands had damage to their water facilities. Two days of winds exceeding  destroyed nearly all of the plants and trees on Guanaja, uprooting or knocking down almost the entire mangrove forest. Most mangrove trees were an average of  in height before they fell. Those remaining standing were damaged internally and unable to regrow. All trees lost their leaves on the island, and 70% of conifer trees were knocked down. Montane trees likewise experienced severe damage, although they made a recovery within a year. However, no mangrove trees had regrown there by three years after the storm struck, indicating the level of destruction. Tree damage also occurred on nearby Roatán island, although to a much lesser degree, and occurring on the eastern end. Winds there were generally less than 185 km/h (115 mph), and the tree damage was more random.

text: On the offshore Guanaja island, waters rose about  during the storm. The combination of

text: storm surge

text: and high winds severely damaged offshore islands. High waves eroded northern coastlines and damaged lagoons. Most of the

text: Bay Islands

text: had damage to their water facilities. Two days of winds exceeding  destroyed nearly all of the plants and trees on Guanaja, uprooting or knocking down almost the entire

text: mangrove

text: forest. Most mangrove trees were an average of  in height before they fell. Those remaining standing were damaged internally and unable to regrow. All trees lost their leaves on the island, and 70% of

text: conifer

text: trees were knocked down.

text: Montane trees

text: likewise experienced severe damage, although they made a recovery within a year. However, no mangrove trees had regrown there by three years after the storm struck, indicating the level of destruction. Tree damage also occurred on nearby

text: Roatán

text: island, although to a much lesser degree, and occurring on the eastern end. Winds there were generally less than 185 km/h (115 mph), and the tree damage was more random.

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answer: 1

text: On August 19, 2014, a tropical wave emerged off the west coast of Africa. The system traversed the Atlantic over the next week with no signs of development. Convection finally increased once the wave entered the Caribbean Sea on August 27; however, it was not until August 30 when interaction with a Kelvin wave spurred organization. An area of low pressure consolidated within the system as it crossed the Yucatán Peninsula on August 31. Formation of a banding feature along the southeastern portion of the circulation on September 1 marked the system's transition into a tropical depression by 18:00 UTC while over the Bay of Campeche. Although situated over warm waters of , strong wind shear created an unfavorable environment and hindered intensification. During this formative stage, the depression tracked northward as its center relocated before turning to the northwest and later west. It was uncertain if a closed circulation truly existed due to conflicting data and the depression could have remained a trough until the afternoon of September 2.

text: On August 19, 2014, a

text: tropical wave

text: emerged off the west coast of Africa. The system traversed the Atlantic over the next week with no signs of

text: development

text: Convection

text: finally increased once the wave entered the

text: Caribbean Sea

text: on August 27; however, it was not until August 30 when interaction with a

text: Kelvin wave

text: spurred organization. An

text: area of low pressure

text: consolidated within the system as it crossed the

text: Yucatán Peninsula

text: on August 31. Formation of a

text: banding feature

text: along the southeastern portion of the circulation on September 1 marked the system's transition into a tropical depression by 18:00

text: UTC

text: while over the

text: Bay of Campeche

text: . Although situated over warm waters of , strong

text: wind shear

text: created an unfavorable environment and hindered intensification. During this formative stage, the depression tracked northward as its center relocated before turning to the northwest and later west. It was uncertain if a closed circulation truly existed due to conflicting data and the depression could have remained a

text: trough

text: until the afternoon of September 2.

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answers: Kelvin wave

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answers: Tropical depression

answers: NDQ_006455

answers: interaction with a Kelvin wave

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answers: northward

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answers: Kelvin wave

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answers: Kelvin wave

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answers: Kelvin wave

answers: NDQ_006460

answers: Waves travel across the ocean to end up on a shoreline

answers: NDQ_006461

answers: Kelvin wave

answer: Yes

answer: Yes

answer: No

answer: No

answer: No

answer: 1

text: In physics, a wave packet (or wave train) is a short "burst" or "envelope" of localized wave action that travels as a unit.  A wave packet can be analyzed into, or can be synthesized from, an infinite set of component sinusoidal waves of different wavenumbers, with phases and amplitudes such that they interfere constructively only over a small region of space, and destructively elsewhere. Each component wave function, and hence the wave packet, are solutions of a wave equation. Depending on the wave equation, the wave packet's profile may remain constant (no dispersion, see figure) or it may change (dispersion) while propagating.

text: In physics, a wave packet (or wave train) is a short "burst" or "

text: envelope

text: " of localized wave action that travels as a unit.  A wave packet can be analyzed into, or can be synthesized from, an infinite set of component

text: sinusoidal wave

text: s of different

text: wavenumber

text: s, with phases and amplitudes such that they interfere constructively only over a small region of space, and destructively elsewhere. Each component

text: wave function

text: , and hence the wave packet, are solutions of a

text: wave equation

text: . Depending on the wave equation, the wave packet's profile may remain constant (no

text: dispersion

text: , see figure) or it may change (dispersion) while propagating.

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answers: destructively

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answers: localized wave action

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answers: propagating

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answers: localized

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answers: waves interfere constructively only over a small region of space

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answers: dispersion

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answers: wave equation

answers: NDQ_006460

answers: propagating

answers: NDQ_006461

answers: they interfere constructively only over a small region of space

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The two main meteorological factors contributing to a storm surge are a long fetch of winds spiraling inward toward the storm, and a low-pressure-induced dome of water drawn up under and trailing the storm's center.

text: The two main

text: meteorological

text: factors contributing to a storm surge are a long

text: fetch

text: of winds spiraling inward toward the storm, and a low-pressure-induced dome of water drawn up under and trailing the storm's center.

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answers: low-pressure

answers: NDQ_006453

answers: storm surge

answers: NDQ_006455

answers: winds spiraling

answers: NDQ_006456

answers: spiraling

answers: NDQ_006457

answers: low-pressure

answers: NDQ_006458

answers: low-pressure-induced dome

answers: NDQ_006459

answers: winds spiraling inward toward the storm

answers: NDQ_006460

answers: storm surge

answers: NDQ_006461

answers: low-pressure-induced dome of water

answer: Yes

answer: Yes

answer: No

answer: No

answer: No

answer: 1

text: Second-wave development strategies have their roots in the increase of worldwide competition, the descent of American manufacturing, and the critical evaluations of first-wave techniques of the late 1960s. These critiques labeled first-wave development as a zero-sum game between elites that instead of creating jobs merely transferred opportunities from one area to another at the benefit of "land-based" elites. The first use of second-wave strategies was in the late 1960s and early 70s. In second-wave economic development, practitioners began to use strategies to retain and expand existing firms. They also included a focus on small business development through entrepreneurial tools like loans and enterprise zones.

text: Second-wave development strategies have their roots in the increase of worldwide competition, the descent of American manufacturing, and the critical evaluations of first-wave techniques of the late 1960s. These critiques labeled first-wave development as a

text: zero-sum

text: game between elites that instead of creating jobs merely transferred opportunities from one area to another at the benefit of "land-based" elites. The first use of second-wave strategies was in the late 1960s and early 70s. In second-wave economic development, practitioners began to use strategies to retain and expand existing firms. They also included a focus on small business development through entrepreneurial tools like loans and enterprise zones.

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answers: Waves

answers: NDQ_006453

answers: Wave

answers: NDQ_006455

answers: increase of worldwide competition, the descent of American manufacturing

answers: NDQ_006456

answers: slow

answers: NDQ_006457

answers: Wave energy is lowest at the surface and increases with depth

answers: NDQ_006458

answers: second-wave

answers: NDQ_006459

answers: elites

answers: NDQ_006460

answers: Wave

answers: NDQ_006461

answers: second-wave economic development

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: There are a few other, smaller waves further down and within the bay, which include "Chickens," "20/20," "Tiger Tracks" and a few unnamed others. These waves generally only work on larger swells, but are surprisingly good alternatives when the main point is big. All of these waves can barrel in the right conditions, which generally require higher tides. There are also some right hand waves on the other side of the peninsula at G-Land, but they are fickle, requiring large swells, and no wind or off-season winds.

text: There are a few other, smaller waves further down and within the bay, which include "Chickens," "20/20," "Tiger Tracks" and a few unnamed others. These waves generally only work on larger swells, but are surprisingly good alternatives when the main point is big. All of these waves can barrel in the right conditions, which generally require higher tides. There are also some right hand waves on the other side of the peninsula at G-Land, but they are fickle, requiring large swells, and no wind or off-season winds.

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answers: barrel

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answers: higher tides

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answers: larger swells

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answers: Smaller waves

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answers: 20/20

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answers: higher tides

answers: NDQ_006460

answers: Bay

answers: NDQ_006461

answers: higher tides

answer: No

answer: No

answer: No

answer: No

answer: Yes

answer: 1

text: On 24 November 1824 strong winds and a storm surge caused waves to breach Chesil Beach, and many of the buildings in the village were destroyed. Seventy-three years later an old man of the village described the events he had witnessed on that day as a boy:

text: On 24 November 1824 strong winds and a storm surge caused waves to breach Chesil Beach, and many of the buildings in the village were destroyed. Seventy-three years later an old man of the village described the events he had witnessed on that day as a boy:

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text: Hurricane Emily originated from an African tropical wave that passed through the Cape Verde Islands on August 17, 1993. The wave traversed the tropical Atlantic and developed a closed cyclonic circulation five days later about  east-northeast of Puerto Rico, when the National Hurricane Center (NHC) classified it as a tropical depression. Moving northwestward, the depression remained poorly organized for several days, with an ill-defined circulation center and sporadic thunderstorms, in part due to unfavorable wind shear from an upper-level low to its north. On August 25, the depression became nearly stationary in response to weakening steering currents. As the upper environment turned less hostile to development, a reconnaissance aircraft found unusually high sustained winds—an indication that the cyclone had quickly strengthened into a strong tropical storm. The NHC named the storm Emily and upgraded it to a hurricane the following day, based on reports of 75 mph (120 km/h) winds from a second reconnaissance mission.

text: Hurricane Emily originated from an African

text: tropical wave

text: that passed through the

text: Cape Verde Islands

text: on August 17, 1993. The wave traversed the

text: tropical Atlantic

text: and

text: developed

text: a closed cyclonic circulation five days later about  east-northeast of

text: Puerto Rico

text: , when the

text: National Hurricane Center

text: (NHC) classified it as a

text: tropical depression

text: . Moving northwestward, the depression remained poorly organized for several days, with an ill-defined circulation center and sporadic thunderstorms, in part due to unfavorable

text: wind shear

text: from an

text: upper-level low

text: to its north. On August 25, the depression became nearly stationary in response to weakening

text: steering currents

text: . As the upper environment turned less hostile to development, a

text: reconnaissance aircraft

text: found unusually high

text: sustained winds

text: —an indication that the cyclone had quickly strengthened into a strong

text: tropical storm

text: . The NHC named the storm Emily and upgraded it to a hurricane the following day, based on reports of 75 mph (120 km/h) winds from a second reconnaissance mission.

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text: The eye of the storm passed near Key West about midday on September 24. Upon making landfall, Hurricane Georges brought a storm surge of up to 12 feet (3.6 m) in Tavernier, Florida, with similar but lesser amounts along the Florida Keys. Wind gusts near the center of the storm reached 125 mph (205 km/h). The islands, some only 7 feet (2 m) high and 300 yards (275 m) wide, are easily flooded, and with up to 10 foot (3 m) waves many parts of the Overseas Highway were under water. Strong winds downed palm trees and power lines, leaving all of the Keys without power. Georges's waves overturned 2 boats in Key West, damaged 1,536 houses, and destroyed 173 homes, many of which were mobile homes. Rainfall amounts amounted to a maximum of 8.41 inches (210 mm) in Tavernier, while other locations reported lesser amounts. Damage in the Florida Keys amounted to $200 million (1998 USD, $250 million 2009 USD). A long-tracked F0 tornado, originally forming as a waterspout, caused moderate damage from Key Biscayne to Cutler Ridge. Another F0 tornado briefly touched down near Miami, damaging cars and trees before lifting. In Charlotte County another F0 tornado tracked for , uprooting several trees along its path before dissipating. On September 25, a waterspout moved onshore near Sebastian and severely damaged a factory; the tornado was rated F1 and caused $700,000 in damages.

text: The eye of the storm passed near Key West about midday on September 24. Upon making landfall, Hurricane Georges brought a storm surge of up to 12 feet (3.6 m) in

text: Tavernier, Florida

text: , with similar but lesser amounts along the Florida Keys. Wind gusts near the center of the storm reached 125 mph (205 km/h). The islands, some only 7 feet (2 m) high and 300 yards (275 m) wide, are easily flooded, and with up to 10 foot (3 m) waves many parts of the

text: Overseas Highway

text: were under water. Strong winds downed palm trees and power lines, leaving all of the Keys without power. Georges's waves overturned 2 boats in Key West, damaged 1,536 houses, and destroyed 173 homes, many of which were mobile homes. Rainfall amounts amounted to a maximum of 8.41 inches (210 mm) in

text: Tavernier

text: , while other locations reported lesser amounts. Damage in the Florida Keys amounted to $200 million (1998 USD, $250 million 2009 USD). A long-tracked

text: tornado, originally forming as a

text: waterspout

text: , caused moderate damage from

text: Key Biscayne

text: to

text: Cutler Ridge

text: . Another F0 tornado briefly touched down near

text: Miami

text: , damaging cars and trees before lifting. In

text: Charlotte County

text: another F0 tornado tracked for , uprooting several trees along its path before dissipating. On September 25, a waterspout moved onshore near

text: Sebastian

text: and severely damaged a factory; the tornado was rated F1 and caused $700,000 in damages.

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answers: NDQ_006452

answers: up to 10 foot

answers: NDQ_006453

answers: storm surge

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answers: hurricane

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answers: slow

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answers: up to 10 foot (3 m) waves

answers: NDQ_006458

answers: a waterspout moved onshore

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answers: storm surge

answers: NDQ_006460

answers: waterspout moved onshore

answers: NDQ_006461

answers: up to 10 foot (3 m) waves

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: 1

text: All of these factors work together to determine the size of wind waves:

text: All of these factors work together to determine the size of wind waves:

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answers: NDQ_006460

answers: 0

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answers: 0

answers: NDQ_006452

answers: The height of the wave

answers: NDQ_006453

answers: Sea level rise

answers: NDQ_006455

answers: wind

answers: NDQ_006456

answers: fast

answers: NDQ_006457

answers: surface

answers: NDQ_006458

answers: Friction

answers: NDQ_006459

answers: wind

answers: NDQ_006460

answers: The water in a wave travels

answers: NDQ_006461

answers: a bottle is a solid

answer: Yes

answer: No

answer: Yes

answer: No

answer: Yes

answer: 1

text: In the Bahamas, Dennis produced moderate winds, rain, and storm surge on San Salvador, Crooked Island, Eleuthera, and Abaco Islands, resulting in damage to roofs and coastal properties. Dennis brought  waves to the east coast of Florida, causing minor erosion and four drowning deaths. The waves left severe erosion and coastal flooding along the Outer Banks of North Carolina. An  deep channel created along Highway 12 isolated three towns on Hatteras Island. In Carteret, Craven, and Dare counties, the storm damaged at least 2,025 homes and businesses to some degree. Heavy rainfall, peaking at  at Ocracoke, fell in eastern North Carolina. Although the precipitation was generally beneficial due to drought conditions, it also damaged crops. Two indirect deaths occurred in Richlands during a weather-related car accident. Similar inland flooding occurred in northern and eastern Virginia, with precipitation reaching  near Lawrenceville. A tornado in Hampton severely damaged five apartment complexes, three of which were condemned completely, as well an assisted living facility; about 460 people were forced to evacuate from the buildings, and as many as 800 vehicles may have been damaged. Overall damage in North Carolina and Virginia totaled about $157 million. Generally minor flooding occurred in the Mid-Atlantic and New England.

text: In the Bahamas, Dennis produced moderate winds, rain, and storm surge on

text: San Salvador

text: Crooked Island

text: Eleuthera

text: , and

text: Abaco Islands

text: , resulting in damage to roofs and coastal properties. Dennis brought  waves to the east coast of Florida, causing minor erosion and four drowning deaths. The waves left severe erosion and coastal flooding along the

text: Outer Banks

text: of North Carolina. An  deep channel created along

text: Highway 12

text: isolated three towns on

text: Hatteras Island

text: . In

text: Carteret

text: Craven

text: , and

text: Dare

text: counties, the storm damaged at least 2,025 homes and businesses to some degree. Heavy rainfall, peaking at  at

text: Ocracoke

text: , fell in eastern North Carolina. Although the precipitation was generally beneficial due to drought conditions, it also damaged crops. Two indirect deaths occurred in

text: Richlands

text: during a weather-related car accident. Similar inland flooding occurred in northern and eastern Virginia, with precipitation reaching  near

text: Lawrenceville

text: . A tornado in

text: Hampton

text: severely damaged five apartment complexes, three of which were condemned completely, as well an assisted living facility; about 460 people were forced to evacuate from the buildings, and as many as 800 vehicles may have been damaged. Overall damage in North Carolina and Virginia totaled about $157 million. Generally minor flooding occurred in the

text: Mid-Atlantic

text: and

text: New England

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answers: 4

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answers: NDQ_006452

answers: waves leave severe erosion and coastal flooding

answers: NDQ_006453

answers: storm surge

answers: NDQ_006455

answers: Dennis

answers: NDQ_006456

answers: slow

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answers: The waves left severe erosion

answers: NDQ_006458

answers: causing minor erosion and four drowning deaths

answers: NDQ_006459

answers: storm surge

answers: NDQ_006460

answers: coastal flooding

answers: NDQ_006461

answers: minor erosion

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: 1

text: In Texas upon landfall, an  to  storm surge inundated lower Padre Island.  The force of the storm tide made 31 cuts completely through the barrier island.  Padre Island suffered significant devastation, and the island's sensitive ecosystem was altered by the storm.  The highest sustained wind was reported as , recorded in the town of South Padre Island, across the Laguna Madre from Port Isabel.  Winds as high as  were measured at the Brownsville National Weather Service office at landfall.  Since the hurricane bent the anemometer 30 degrees from the vertical, it is possible the winds at Brownsville were underestimated.  Gusts of over  were recorded as far inland as the towns of McAllen, Edinburg, Mission, and Pharr, some  from the gulf coast.  Beulah spawned a record 115 tornadoes which destroyed homes, commercial property, and inflicted serious damage on the region's agricultural industry.  The tornado record from Beulah would survive until Hurricane Ivan set a new record in 2004.  The Rio Grande Valley's citrus industry, based on cultivation of the famous "Ruby Red" grapefruit, was particularly hard hit.

text: In Texas upon landfall, an  to  storm surge inundated lower Padre Island.  The force of the storm tide made 31 cuts completely through the barrier island.

text: Padre Island

text: suffered significant devastation, and the island's sensitive ecosystem was altered by the storm.  The highest sustained wind was reported as , recorded in the town of

text: South Padre Island

text: , across the Laguna Madre from

text: Port Isabel

text: .  Winds as high as  were measured at the Brownsville National Weather Service office at landfall.  Since the hurricane bent the

text: anemometer

text: 30 degrees from the vertical, it is possible the winds at Brownsville were underestimated.  Gusts of over  were recorded as far inland as the towns of

text: McAllen

text: Edinburg

text: Mission

text: , and

text: Pharr

text: , some  from the gulf coast.  Beulah spawned a record 115

text: tornado

text: es which destroyed homes, commercial property, and inflicted serious damage on the region's agricultural industry.  The tornado record from Beulah would survive until

text: Hurricane Ivan

text: set a new record in 2004.  The

text: Rio Grande Valley

text: 's citrus industry, based on cultivation of the famous "Ruby Red"

text: grapefruit

text: , was particularly hard hit.

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answers: storm surge

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answers: storm surge

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answers: storm surge

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answers: vertical

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answers: storm tide

answers: NDQ_006460

answers: storm surge

answers: NDQ_006461

answers: the force of the storm tide

answer: Yes

answer: Yes

answer: No

answer: No

answer: No

answer: 1

text: While internal waves of higher magnitudes will often break after crossing over the shelf break, smaller trains will proceed across the shelf unbroken. At low wind speeds these internal waves are evidenced by the formation of wide surface slicks, oriented parallel to the bottom topography, which progress shoreward with the internal waves. Waters above an internal wave converge and sink in its trough and upwell and diverge over its crest. The convergence zones associated with internal wave troughs often accumulate oils and flotsam that occasionally progress shoreward with the slicks. These rafts of flotsam can also harbor high concentrations of larvae of invertebrates and fish an order of magnitude higher than the surrounding waters.

text: While internal waves of higher magnitudes will often break after crossing over the shelf break, smaller trains will proceed across the shelf unbroken. At low wind speeds these internal waves are evidenced by the formation of wide surface slicks, oriented parallel to the bottom topography, which progress shoreward with the internal waves. Waters above an internal wave converge and sink in its trough and upwell and diverge over its crest. The convergence zones associated with internal wave troughs often accumulate oils and

text: flotsam

text: that occasionally progress shoreward with the slicks. These rafts of flotsam can also harbor high concentrations of larvae of

text: invertebrates

text: and fish an order of magnitude higher than the surrounding waters.

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answers: 5

answers: NDQ_006461

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answers: NDQ_006452

answers: higher magnitudes will often break

answers: NDQ_006453

answers: slicks

answers: NDQ_006455

answers: low wind speeds

answers: NDQ_006456

answers: shoreward

answers: NDQ_006457

answers: Internal waves of higher magnitudes will often break

answers: NDQ_006458

answers: surface slicks

answers: NDQ_006459

answers: internal waves

answers: NDQ_006460

answers: shoreward

answers: NDQ_006461

answers: formation of wide surface slicks, oriented parallel to the bottom topography

answer: No

answer: Yes

answer: Yes

answer: No

answer: Yes

answer: 1

text: Another possible initiation pattern tested in rats suggested the thalamocortical (TC) loop is involved in the initiation of spike-and-wave oscillations under certain conditions. In this study, relay and reticular thalamic neurons of epileptic and non-epileptic rats were dual extracellularly recorded and juxtacellularly labeled. Medium oscillations (5–9 Hz) in both types of rats were noted to occur randomly in an unsynchronized pattern in relay and reticular neurons. However, spontaneous spike-and-wave discharges were observed in epileptic rats when the medium oscillations became synchronized, suggesting a dependence of the two. However, since medium ranged oscillations only developed into spike-and-wave discharges spontaneously, genetic factors also seem to contribute to the initiation of synchronized oscillations. These genetic factors may contribute to spike-and-wave oscillations by decreasing the action potential threshold in reticular cells, making them more excitable and potentially easier to initiate synchronized firing. Another study has shown that these medium oscillations have led to spike-and-wave discharges.  The activity of the primary and secondary cortical regions, as well as the adjacent insular cortex were recorded using an EEG and where applied with electrical stimulation. The findings here showed that the onset of spike-and-wave discharged were followed by 5–9 Hz oscillations in these cortical regions as well.

text: insular cortex

text: were recorded using an EEG and where applied with electrical stimulation. The findings here showed that the onset of spike-and-wave discharged were followed by 5–9 Hz oscillations in these cortical regions as well.

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answers: The onset of spike-and-wave discharged were followed by 5–9 Hz oscillations in these cortical regions

answers: NDQ_006453

answers: The onset of spike-and-wave discharges were followed by 5–9 Hz oscillations in these cortical regions as well.

answers: NDQ_006455

answers: spontaneous spike-and-wave discharges

answers: NDQ_006456

answers: unsynchronized

answers: NDQ_006457

answers: The onset of spike-and-wave discharges were followed by 5–9 Hz oscillations in these cortical regions as well

answers: NDQ_006458

answers: The onset of spike-and-wave discharged were followed by 5–9 Hz oscillations in these cortical regions

answers: NDQ_006459

answers: thalamic neurons

answers: NDQ_006460

answers: Waves travel across the ocean to end up on a shoreline

answers: NDQ_006461

answers: TC loop is involved in the initiation of spike-and-wave oscillations under certain conditions

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: On July 27, the precursor to Ernesto moved off the west coast of Africa as a tropical wave. At the time, the wave was associated with a disorganized area of convection. On July 29, a broad low pressure area developed in association with the tropical wave. The National Hurricane Center (NHC) first monitored the tropical wave in its tropical weather outlook on July 30, noting that the system had an accompanying low pressure area and was showing signs of development. The convection slowly organized due to generally favorable environmental conditions. After the circulation became better defined, the NHC initiated advisories on Tropical Depression Five at 2100 UTC on August 1. At the time, the depression was located about 810 mi (1305 km) east of the Lesser Antilles, moving west-northwestward due to an anticyclone to its north. In the 12 hours after its formation, the system's convection became disorganized due to westerly wind shear and dry air, and the NHC remarked the potential for degeneration into a tropical wave. However, the depression's rainbands began to strengthen and become more organized. A Hurricane Hunters flight on August 2 observed tropical storm force winds, and accordingly the NHC upgraded the depression to Tropical Storm Ernesto at 2100 UTC.

text: On July 27, the precursor to Ernesto moved off the west coast of Africa as a

text: tropical wave

text: . At the time, the wave was associated with a disorganized area of

text: convection

text: . On July 29, a broad

text: low pressure area

text: developed in association with the tropical wave. The

text: National Hurricane Center

text: (NHC) first monitored the tropical wave in its tropical weather outlook on July 30, noting that the system had an accompanying low pressure area and was showing signs of

text: development

text: . The convection slowly organized due to generally favorable environmental conditions. After the circulation became better defined, the NHC initiated advisories on Tropical Depression Five at 2100 UTC on August 1. At the time, the depression was located about 810 mi (1305 km) east of the

text: Lesser Antilles

text: , moving west-northwestward due to an

text: anticyclone

text: to its north. In the 12 hours after its formation, the system's convection became disorganized due to westerly

text: wind shear

text: and dry air, and the NHC remarked the potential for degeneration into a tropical wave. However, the depression's

text: rainband

text: s began to strengthen and become more organized. A

text: Hurricane Hunter

text: s flight on August 2 observed tropical storm force winds, and accordingly the NHC upgraded the depression to Tropical Storm Ernesto at 2100 UTC.

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answers: Tropical Depression Five

answers: NDQ_006453

answers: Tropical Depression

answers: NDQ_006455

answers: convection

answers: NDQ_006456

answers: slow

answers: NDQ_006457

answers: The National Hurricane Center

answers: NDQ_006458

answers: a tropical wave

answers: NDQ_006459

answers: convection

answers: NDQ_006460

answers: It moved off the west coast of Africa

answers: NDQ_006461

answers: disorganized area of convection

answer: No

answer: Yes

answer: No

answer: No

answer: No

answer: 1

text: In late September, a large area of disturbed weather associated with two tropical waves formed just east of the Lesser Antilles. The disturbance drifted very slowly west-northwestward, inhibited by strong wind shear that eventually caused the westernmost wave to dissipate. Albeit weak, an elongated remnant trough, or area of low pressure, persisted for several days, stalling over the extreme eastern Caribbean Sea as a nearby upper-level cyclonic vortex retrograded to its north. By October 5, the trough had drifted northward into a more favorable atmospheric environment over the Virgin Islands, which allowed the lowest pressures to extend to the surface. The low became well defined, interacting with the adjacent upper vortex to produce a wide convective band—a concentrated region in which strong showers and thunderstorms can form—over the northeastern Caribbean. Over the next day, the system continued to acquire a prominent subtropical structure: it developed a markedly larger wind radius than typically seen in pure tropical cyclones. Satellite observations also revealed that although the lower wind circulation was distinct, it had become intertwined with the cyclonic vortex aloft to its southwest, confirming the hybrid nature of the system. The National Hurricane Center (NHC) thus classified the system as a subtropical depression at 06:00 UTC on October 6, when it was 265 mi (425 km) north-northwest of San Juan, Puerto Rico.

text: In late September, a large area of disturbed weather associated with two

text: tropical waves

text: formed just east of the

text: Lesser Antilles

text: . The disturbance drifted very slowly west-northwestward, inhibited by strong

text: wind shear

text: that eventually caused the westernmost wave to dissipate. Albeit weak, an elongated remnant

text: trough

text: , or

text: area of low pressure

text: , persisted for several days, stalling over the extreme eastern

text: Caribbean Sea

text: as a nearby

text: upper-level cyclonic vortex

text: retrograded to its north. By October 5, the trough had drifted northward into a more favorable atmospheric environment over the

text: Virgin Islands

text: , which allowed the lowest pressures to extend to the surface. The low became well defined, interacting with the adjacent upper vortex to produce a wide

text: convective

text: band

text: —a concentrated region in which strong showers and thunderstorms can form—over the northeastern Caribbean. Over the next day, the system continued to acquire a prominent

text: subtropical structure

text: : it developed a markedly larger

text: wind radius

text: than typically seen in pure tropical cyclones. Satellite observations also revealed that although the lower wind circulation was distinct, it had become intertwined with the cyclonic vortex aloft to its southwest, confirming the hybrid nature of the system. The

text: National Hurricane Center

text: (NHC) thus classified the system as a

text: subtropical depression

text: at 06:00 UTC on October 6, when it was 265 mi (425 km) north-northwest of

text: San Juan, Puerto Rico

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answers: the westernmost wave to dissipate

answers: NDQ_006453

answers: tropical waves

answers: NDQ_006455

answers: late September

answers: NDQ_006456

answers: very slowly

answers: NDQ_006457

answers: By October 5, the trough had drifted northward into a more favorable atmospheric environment

answers: NDQ_006458

answers: The disturbance drifted very slowly

answers: NDQ_006459

answers: tropical cyclones

answers: NDQ_006460

answers: 425 km

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answers: strong wind shear

answer: No

answer: Yes

answer: Yes

answer: No

answer: No

answer: 1

text: Though the eye is by far the calmest part of the storm, with no wind at the center and typically clear skies, over the ocean it is possibly the most hazardous area. In the eyewall, wind-driven waves all travel in the same direction. In the center of the eye, however, the waves converge from all directions, creating erratic crests that can build on each other to become rogue waves. The maximum height of hurricane waves is unknown, but measurements during Hurricane Ivan when it was a Category 4 hurricane estimated that waves near the eyewall exceeded 40 m (130 ft) from peak to trough.

text: Though the eye is by far the calmest part of the storm, with no wind at the center and typically clear skies, over the ocean it is possibly the most hazardous area. In the eyewall, wind-driven waves all travel in the same direction. In the center of the eye, however, the waves converge from all directions, creating erratic crests that can build on each other to become

text: rogue wave

text: s. The maximum height of hurricane waves is unknown, but measurements during

text: Hurricane Ivan

text: when it was a Category 4 hurricane estimated that waves near the eyewall exceeded 40 m (130 ft) from peak to trough.

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answers: rogue waves

answers: NDQ_006453

answers: crests

answers: NDQ_006455

answers: In the center of the eye

answers: NDQ_006456

answers: trough

answers: NDQ_006457

answers: The maximum height of hurricane waves is unknown

answers: NDQ_006458

answers: trough

answers: NDQ_006459

answers: erratic crests

answers: NDQ_006460

answers: trough

answers: NDQ_006461

answers: waves converge from all directions

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: Yes

answer: 1

text: In fluid dynamics, a breaking wave is a wave whose amplitude reaches a critical level at which some process can suddenly start to occur that causes large amounts of wave energy to be transformed into turbulent kinetic energy.  At this point, simple physical models that describe wave dynamics often become invalid, particularly those that assume linear behaviour.

text: In

text: fluid dynamics

text: , a breaking wave is a

text: wave

text: whose

text: amplitude

text: reaches a critical level at which some process can suddenly start to occur that causes large amounts of wave energy to be transformed into

text: turbulent

text: kinetic energy

text: .  At this point, simple physical models that describe wave dynamics often become invalid, particularly those that assume

text: linear

text: behaviour.

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answers: breaking wave

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text: Crystal Beach, a populous community located roughly at the midpoint of the peninsula, was submerged and destroyed; waves and wind pounded houses, and even some houses elevated on 14-ft (4.3–m) stilts rolled into the waters. The tiny beachfront community of Gilchrist, which sat astride the north-facing Rollover Bay on Bolivar, was completely swept away, save for only a few homes. One of these homes, the only one in its neighborhood to remain intact (although it was rendered uninhabitable), attracted widespread media interest after images of it began to appear in newspapers and on television. At least six bodies were found in an extensive search.	Two flood water sensors in Chambers County, Texas survived Ike's storm surge, while those on eastern Bolivar Peninsula were left inoperable during the hurricane. Along the Eastern shores of Galveston Bay surge heights were measured at 16.9 feet (5.15 m) and a measurement along SH126 measured 17.0 feet (5.18 m). Massive amounts of surge carried debris, largely from Bolivar Peninsula and southern Chambers County were left along the northern coast of Rollover bay Chambers county.

text: Crystal Beach

text: , a populous community located roughly at the midpoint of the peninsula, was submerged and destroyed; waves and wind pounded houses, and even some houses elevated on 14-ft (4.3–m) stilts rolled into the waters. The tiny beachfront community of

text: Gilchrist

text: , which sat astride the north-facing Rollover Bay on Bolivar, was completely swept away, save for only a few homes. One of these homes, the only one in its neighborhood to remain intact (although it was rendered uninhabitable), attracted widespread media interest after images of it began to appear in newspapers and on television. At least six bodies were found in an extensive search.	Two flood water sensors in

text: Chambers County, Texas

text: survived Ike's storm surge, while those on eastern Bolivar Peninsula were left inoperable during the hurricane. Along the Eastern shores of Galveston Bay surge heights were measured at 16.9 feet (5.15 m) and a measurement along SH126 measured 17.0 feet (5.18 m). Massive amounts of surge carried debris, largely from Bolivar Peninsula and southern Chambers County were left along the northern coast of Rollover bay Chambers county.

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text: Hurricane Juan's maximum sustained wind speed at landfall in Nova Scotia was measured at 100 mph (160 km/h). The urban concentration surrounding Halifax Harbour bore the brunt of the highest sustained winds and strongest wind gusts during the storm; some unofficial estimates have placed gusts as high as 145 mph (230 km/h). Wave-rider weather buoys off the entrance of Halifax Harbour snapped their moorings after reportedly recording waves in excess of 65 ft (20 m). Significant erosion occurred on the populated shores of the harbour, particularly in the Bedford Basin where residential properties and railway tracks received most of the wave action. Storm surges of 5 to 7 feet (1.5 to 2 m) were reported in the harbour; it was the highest surge ever recorded in Halifax Harbour. Rainfall was fairly light due to the fast movement and dry air on the southern side of the storm. There were no rainfall reports greater than 2 inches (52 mm).

text: Hurricane Juan's maximum sustained wind speed at landfall in Nova Scotia was measured at 100 mph (160 km/h). The urban concentration surrounding

text: Halifax Harbour

text: bore the brunt of the highest sustained winds and strongest wind gusts during the storm; some unofficial estimates have placed gusts as high as 145 mph (230 km/h). Wave-rider

text: weather buoy

text: s off the entrance of Halifax Harbour snapped their moorings after reportedly recording waves in excess of 65 ft (20 m). Significant erosion occurred on the populated shores of the harbour, particularly in the

text: Bedford Basin

text: where residential properties and railway tracks received most of the wave action. Storm surges of 5 to 7 feet (1.5 to 2 m) were reported in the harbour; it was the highest surge ever recorded in Halifax Harbour. Rainfall was fairly light due to the fast movement and dry air on the southern side of the storm. There were no rainfall reports greater than 2 inches (52 mm).

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answers: 65 ft (20 m)

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answer: Yes

answer: No

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text: In July 1895 the board of directors of the Ilwaco Railway and Navigation Company, known as the IR&N, voted to lease Ocean Wave to the Columbia River and Puget Sound Transportation Company, also known as the CR & PSN and commonly referred to as the White Collar Line. At that time the CR & PSN had on the Columbia River two fast and well-known sternwheelers Telephone and the Bailey Gatzert.  One of the IR&N company directors, Jacob Kamm, did not agree with this decision, and he placed a maritime lien (called a “libel”) on Ocean Wave for $17,851 for services provided by Kamm’s firm, the Vancouver Transportation Company.  While Kamm and Loomis were both on the board of directors of the IR&N, a disagreement between them had arisen, reportedly because Ocean Wave, designed by Kamm, had proven to be a slower boat than Loomis had wanted.

text: In July 1895 the board of directors of the

text: Ilwaco Railway and Navigation Company

text: , known as the IR&N, voted to lease Ocean Wave to the Columbia River and Puget Sound Transportation Company, also known as the CR & PSN and commonly referred to as the White Collar Line. At that time the CR & PSN had on the Columbia River two fast and well-known sternwheelers

text: Telephone

text: and the

text: Bailey Gatzert

text: .  One of the IR&N company directors,

text: Jacob Kamm

text: , did not agree with this decision, and he placed a maritime

text: lien

text: (called a “libel”) on Ocean Wave for $17,851 for services provided by Kamm’s firm, the Vancouver Transportation Company.  While Kamm and Loomis were both on the board of directors of the IR&N, a disagreement between them had arisen, reportedly because Ocean Wave, designed by Kamm, had proven to be a slower boat than Loomis had wanted.

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answers: faster

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answers: NDQ_006458

answers: a slower boat

answers: NDQ_006459

answers: Kamm

answers: NDQ_006460

answers: Columbia River

answers: NDQ_006461

answers: a slower boat

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Weather satellites take advantage of this instability to measure wind speeds over large bodies of water. Waves are generated by the wind, which shears the water at the interface between it and the surrounding air. The computers on board the satellites determine the roughness of the ocean by measuring the wave height. This is done by using radar, where a radio signal is transmitted to the surface and the delay from the reflected signal is recorded, known as the "time of flight". From this meteorologists are able to understand the movement of clouds and the expected air turbulence near them.

text: Weather satellites take advantage of this instability to measure wind speeds over large bodies of water. Waves are generated by the wind, which shears the water at the interface between it and the surrounding air. The computers on board the satellites determine the roughness of the ocean by measuring the wave height. This is done by using

text: radar

text: , where a radio signal is transmitted to the surface and the delay from the reflected signal is recorded, known as the "time of flight". From this meteorologists are able to understand the movement of clouds and the expected air turbulence near them.

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answers: waves break when they become too tall to be supported by their base

answers: NDQ_006453

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answers: wind

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answers: Waves

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answers: waves are generated by the wind

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: 1

text: A tropical wave moved off the coast of Africa on August 7. As it moved across the Atlantic Ocean, it failed to organize. On reaching the eastern Pacific Ocean on August 17, however, an area of convection developed along the wave axis. Dvorak classifications began the next day, and a broad center of circulation gradually formed. Convection was intermittent at first, though it gradually organized and persisted near the center, and on August 20, the disturbance developed into Tropical Depression Nine-E about  south of Puerto Angel, Mexico. It tracked generally west-northwestward, developing more pronounced banding features, and on August 21, the depression intensified into Tropical Storm Howard. The center of Howard became embedded within the deep convection, and the storm quickly strengthened to attain hurricane status late on the 21st. An eye developed as outflow organized further, and Howard began to rapidly intensify to reach peak winds of 150 mph (240 km/h) about 600 miles (965 km) south-southeast of the southern tip of Baja California. At the time of its peak intensity, the eye was small and located within a very cold central dense overcast.

text: A

text: tropical wave

text: moved off the coast of Africa on August 7. As it moved across the Atlantic Ocean, it failed to organize. On reaching the eastern Pacific Ocean on August 17, however, an area of

text: convection

text: developed along the wave axis.

text: Dvorak classifications

text: began the next day, and a broad center of circulation gradually formed. Convection was intermittent at first, though it gradually organized and persisted near the center, and on August 20, the disturbance developed into Tropical Depression Nine-E about  south of

text: Puerto Angel, Mexico

text: . It tracked generally west-northwestward, developing more pronounced

text: banding features

text: , and on August 21, the depression intensified into Tropical Storm Howard. The center of Howard became embedded within the deep convection, and the storm quickly strengthened to attain hurricane status late on the 21st. An

text: eye

text: developed as

text: outflow

text: organized further, and Howard began to

text: rapidly intensify

text: to reach peak winds of 150 mph (240 km/h) about 600 miles (965 km) south-southeast of the southern tip of

text: Baja California

text: . At the time of its peak intensity, the eye was small and located within a very cold

text: central dense overcast

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answers: wave axis

answers: NDQ_006453

answers: Tropical Depression

answers: NDQ_006455

answers: convection developed

answers: NDQ_006456

answers: fast

answers: NDQ_006457

answers: Deep convection

answers: NDQ_006458

answers: On reaching the eastern Pacific Ocean

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answers: convection

answers: NDQ_006460

answers: On reaching the eastern Pacific Ocean

answers: NDQ_006461

answers: a very cold central dense overcast

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Airy wave theory is often applied in ocean engineering and coastal engineering for the modelling of random sea states – giving a description of the wave kinematics and dynamics of high-enough accuracy for many purposes. Further, several second-order nonlinear properties of surface gravity waves, and their propagation, can be estimated from its results. Airy wave theory is also a good approximation for tsunami waves in the ocean, before they steepen near the coast.

text: Airy wave theory is often applied in

text: ocean engineering

text: and

text: coastal engineering

text: for the modelling of

text: random

text: sea state

text: s – giving a description of the wave

text: kinematics

text: and

text: dynamics

text: of high-enough accuracy for many purposes. Further, several

text: second-order

text: nonlinear

text: properties of surface gravity waves, and their propagation, can be estimated from its results. Airy wave theory is also a good approximation for

text: tsunami

text: waves in the ocean, before they steepen near the coast.

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answers: surface gravity waves

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answers: coast

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answers: surface gravity waves

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Equatorial waves are ocean waves trapped close to the equator, meaning that they decay rapidly away from the equator, but can propagate in the longitudinal and vertical directions. Wave trapping is the result of the Earth's rotation and its spherical shape which combine to cause the magnitude of the Coriolis force to increase rapidly away from the equator. Equatorial waves are present in both the tropical atmosphere and ocean and play an important role in the evolution of many climate phenomena such as El Niño. Many physical processes may excite equatorial waves including, in the case of the atmosphere, diabatic heat release associated with cloud formation, and in the case of the ocean, anomalous changes in the strength or direction of the trade winds.

text: Equatorial waves are ocean waves trapped close to the

text: equator

text: , meaning that they decay rapidly away from the equator, but can propagate in the

text: longitudinal

text: and vertical directions. Wave trapping is the result of the Earth's rotation and its spherical shape which combine to cause the magnitude of the

text: Coriolis force

text: to increase rapidly away from the equator. Equatorial waves are present in both the tropical atmosphere and ocean and play an important role in the evolution of many climate phenomena such as

text: El Niño

text: . Many physical processes may excite equatorial waves including, in the case of the atmosphere,

text: diabatic

text: heat release associated with cloud formation, and in the case of the ocean, anomalous changes in the strength or direction of the trade winds.

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answers: Equatorial

answers: NDQ_006453

answers: El Ni o

answers: NDQ_006455

answers: physical processes

answers: NDQ_006456

answers: longitudinal

answers: NDQ_006457

answers: Wave energy is lowest at the surface and increases with depth

answers: NDQ_006458

answers: Coriolis force to increase rapidly away from the equator

answers: NDQ_006459

answers: Earth's rotation and its spherical shape

answers: NDQ_006460

answers: Wave trapping

answers: NDQ_006461

answers: Earth's rotation and its spherical shape

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Hundreds of factors are involved in the lunitidal interval, especially near shorelines. However, if you are far enough away from the coast, the dominating consideration is the speed of gravity waves, which increases with the depth of the ocean. (It is proportional to the square root of the depth, for the extremely long gravity waves that transport the water that is following the moon around the earth. The oceans are about 4 km deep and would have to be at least 22 km deep for these waves to keep up with the moon. As mentioned above, a similar time lag accompanies the solar tides, a complicating factor that varies with the phases of the moon.) By observing the age of leap tides, it becomes clear that the delay can actually exceed 24 hours in some locations.

text: Hundreds of factors are involved in the lunitidal interval, especially near shorelines. However, if you are far enough away from the coast, the dominating consideration is the speed of

text: gravity waves

text: , which increases with the depth of the ocean. (It is proportional to the square root of the depth, for the extremely long gravity waves that transport the water that is following the moon around the earth. The oceans are about 4 km deep and would have to be at least 22 km deep for these waves to keep up with the moon. As mentioned above, a similar time lag accompanies the solar tides, a complicating factor that varies with the phases of the moon.) By observing the age of leap tides, it becomes clear that the delay can actually exceed 24 hours in some locations.

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answers: gravity waves, which increases with the depth of the ocean

answers: NDQ_006453

answers: gravitational waves

answers: NDQ_006455

answers: the moon

answers: NDQ_006456

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answers: NDQ_006457

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answers: NDQ_006459

answers: depth of the ocean

answers: NDQ_006460

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answers: NDQ_006461

answers: gravity waves

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Solar energy from the Sun creates temperature differentials that result in wind. The interaction between wind and the surface of water creates waves, which are larger when there is a greater distance for them to build up. Wave energy potential is greatest between 30° and 60° latitude in both hemispheres on the west coast because of the global direction of wind. When evaluating wave energy as a technology type, it is important to distinguish between the four most common approaches: point absorber buoys, surface attenuators, oscillating water columns, and overtopping devices.

text: Solar energy from the Sun creates temperature differentials that result in wind. The interaction between wind and the surface of water creates waves, which are larger when there is a greater distance for them to build up. Wave energy potential is greatest between 30° and 60° latitude in both hemispheres on the west coast because of the global direction of wind. When evaluating wave energy as a technology type, it is important to distinguish between the four most common approaches:

text: point absorber buoy

text: s,

text: surface attenuator

text: s,

text: oscillating water column

text: s, and

text: overtopping devices

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answers: overtopping devices

answers: NDQ_006453

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answers: NDQ_006455

answers: interaction between wind and the surface of water

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answers: oscillating water columns

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answers: greater distance

answers: NDQ_006460

answers: surface of water

answers: NDQ_006461

answers: oscillating water columns

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: 1

text: In North America, extra-tropical storm surges may occur on the Pacific and Alaska coasts, and north of 31°N on the Atlantic Coast. Extra-tropical storm surges may be possible for the Gulf coast mostly during the wintertime, when extra-tropical cyclones affect the coast, such as in the March 1993 Storm of the Century.

text: In North America, extra-tropical storm surges may occur on the Pacific and Alaska coasts, and north of 31°N on the Atlantic Coast. Extra-tropical storm surges may be possible for the

text: Gulf coast

text: mostly during the wintertime, when extra-tropical cyclones affect the coast, such as in the

text: March 1993 Storm of the Century

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answers: NDQ_006452

answers: extra-tropical

answers: NDQ_006453

answers: storm surge

answers: NDQ_006455

answers: storm surges

answers: NDQ_006456

answers: fast

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answers: surface

answers: NDQ_006458

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answers: NDQ_006459

answers: storm surges

answers: NDQ_006460

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answers: NDQ_006461

answers: extra-tropical

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Similar to Alison, Bella originated on January 18 from a surge in the monsoon trough to the southwest of Sumatra. For several days, the system remained weak as it moved generally west-southwestward. On January 25, it intensified to tropical storm status, but Bella took three more days to intensify to tropical cyclone status, or with 10‑minute maximum sustained winds of 120 km/h (75 mph). The cyclone attained peak intensity on January 29, officially reaching winds of 155 km/h (100 mph). The JTWC unofficially estimated winds of 240 km/h (150 mph), the highest the agency estimated for any storm in the Southern Hemisphere in the year. Bella later turned to the southeast and weakened, passing about 50 km (30 mi) west of Rodrigues on January 31. The storm turned to the south-southwest and back to the southeast again, becoming extratropical on February 4.

text: Similar to Alison, Bella originated on January 18 from a surge in the

text: monsoon trough

text: to the southwest of

text: Sumatra

text: . For several days, the system remained weak as it moved generally west-southwestward. On January 25, it intensified to tropical storm status, but Bella took three more days to intensify to

text: tropical cyclone status

text: , or with 10‑minute maximum sustained winds of 120 km/h (75 mph). The cyclone attained peak intensity on January 29, officially reaching winds of 155 km/h (100 mph). The JTWC unofficially estimated winds of 240 km/h (150 mph), the highest the agency estimated for any storm in the

text: Southern Hemisphere

text: in the year. Bella later turned to the southeast and weakened, passing about 50 km (30 mi) west of

text: Rodrigues

text: on January 31. The storm turned to the south-southwest and back to the southeast again, becoming

text: extratropical

text: on February 4.

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answers: 2: The answer has limited relevance and completeness, with significant gaps or inaccuracy.

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answers: Bella later turned to the southeast and weakened

answers: NDQ_006453

answers: Tropical cyclone

answers: NDQ_006455

answers: monsoon trough

answers: NDQ_006456

answers: forward

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answers: The JTWC unofficially estimated winds of 240 km/h

answers: NDQ_006458

answers: Bella originated on January 18

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answers: tropical cyclone

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answers: Bella originated on January 18

answers: NDQ_006461

answers: Bella originated on January 18 from a surge

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: On September 1 a tropical wave exited the African coast, and moved westward across the Atlantic Ocean. A trough of low pressure moved southeastward through the tropics, and brought the wave more towards the north. Generally favorable conditions for development allowed the wave to organize into a tropical depression on September 5, and two days later it attained tropical storm status. Cindy continued northward, and peaked at  winds on September 8 before turning to the northeast. Strong upper-level shear weakened the storm, and after two days of struggling as a tropical storm, Cindy became extratropical on September 10 to the northwest of the Azores. Cindy did not affect any landmasses.

text: On September 1 a

text: tropical wave

text: exited the African coast, and moved westward across the Atlantic Ocean. A trough of low pressure moved southeastward through the tropics, and brought the wave more towards the north. Generally favorable conditions for development allowed the wave to organize into a tropical depression on September 5, and two days later it attained tropical storm status. Cindy continued northward, and peaked at  winds on September 8 before turning to the northeast. Strong upper-level shear weakened the storm, and after two days of struggling as a tropical storm, Cindy became

text: extratropical

text: on September 10 to the northwest of the

text: Azores

text: . Cindy did not affect any landmasses.

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answers: extratropical

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answers: tropical depression

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answers: Generally favorable conditions for development

answers: NDQ_006456

answers: northward

answers: NDQ_006457

answers: surface-level shear

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answers: shear

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answers: tropical storm

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answers: The wave exited the African coast

answers: NDQ_006461

answers: low pressure

answer: No

answer: No

answer: No

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answer: 1

text: Prior to making landfall, Audrey severely disrupted offshore drilling operations in the Gulf of Mexico. Damages from offshore oil facilities alone was estimated at $16 million. Audrey caused much of its destruction near the border between Texas and Louisiana upon its first and only landfall. The hurricane's strong winds resulted in widespread property and infrastructural damage. Power outages also resulted from the strong winds. However, as typical with most landfalling tropical cyclones, most of the destruction at the coast was the result of the hurricane's strong storm surge, which was amplified by Audrey's rapid deepening just prior to landfall. The hurricane's storm surge was reported to have peaked as high as 12 ft (3.7 m), helping to inundate coastal areas. Damage from the surge alone extended 25 mi (40 km) inland. The rough seas killed nine people offshore after capsizing the boat they were in. Further inland in Louisiana, the storm spawned two tornadoes, causing additional damage. The hurricane also dropped heavy rainfall, peaking at 10.63 in (270 mm) near Basile, Louisiana. In Louisiana and Texas, where Audrey first impacted, damages totaled $128 million.

text: Prior to making landfall, Audrey severely disrupted

text: offshore drilling

text: operations in the

text: Gulf of Mexico

text: . Damages from offshore oil facilities alone was estimated at $16 million. Audrey caused much of its destruction near the border between

text: Texas

text: and Louisiana upon its first and only landfall. The hurricane's strong winds resulted in widespread property and infrastructural damage.

text: Power outage

text: s also resulted from the strong winds. However, as typical with most landfalling tropical cyclones, most of the destruction at the coast was the result of the hurricane's strong

text: storm surge

text: , which was amplified by Audrey's rapid deepening just prior to landfall. The hurricane's storm surge was reported to have peaked as high as 12 ft (3.7 m), helping to inundate coastal areas. Damage from the surge alone extended 25 mi (40 km) inland. The rough seas killed nine people offshore after capsizing the boat they were in. Further inland in Louisiana, the storm spawned two

text: tornado

text: es, causing additional damage. The hurricane also dropped heavy rainfall, peaking at 10.63 in (270 mm) near

text: Basile, Louisiana

text: . In Louisiana and Texas, where Audrey first impacted, damages totaled $128 million.

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answers: The hurricane's strong storm surge

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answers: Deepening

answers: NDQ_006459

answers: storm surge

answers: NDQ_006460

answers: landfall

answers: NDQ_006461

answers: strong winds

answer: No

answer: Yes

answer: Yes

answer: No

answer: No

answer: 1

text: Wave height is determined by wind speed, the duration of time the wind has been blowing, fetch (the distance over which the wind excites the waves) and by the depth and topography of the seafloor (which can focus or disperse the energy of the waves). A given wind speed has a matching practical limit over which time or distance will not produce larger waves. When this limit has been reached the sea is said to be "fully developed".

text: Wave height

text: is determined by wind speed, the duration of time the wind has been blowing, fetch (the distance over which the wind excites the waves) and by the depth and topography of the seafloor (which can focus or disperse the energy of the waves). A given wind speed has a matching practical limit over which time or distance will not produce larger waves. When this limit has been reached the sea is said to be "fully developed".

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answers: NDQ_006452

answers: When this limit has been reached

answers: NDQ_006453

answers: fetch

answers: NDQ_006455

answers: wind

answers: NDQ_006456

answers: fast

answers: NDQ_006457

answers: Wave height is determined by wind speed

answers: NDQ_006458

answers: depth and topography of the seafloor

answers: NDQ_006459

answers: wind speed

answers: NDQ_006460

answers: fetch

answers: NDQ_006461

answers: depth and topography

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: 1

text: Wind wave forecasts are issued regionally by Environment Canada.

text: Wind wave forecasts are issued regionally by

text: Environment Canada

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answers: Wind wave

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answer: Yes

answer: No

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answer: 1

text: The Frisians immigrated into North Frisia from the South in two waves. During the 8th century A.D. they mostly settled on the islands Heligoland, Sylt, Föhr, Amrum and presumably also in parts of the Eiderstedt peninsula. The coastal marshlands of the mainland were settled in a second wave and after a series of storm surges the Frisians also used to settle on the higher inland geest. While the marshland and its bogs had to be drained, the higher geestland cores of the islands were in turn mostly barren and needed fertilisation before a proper agriculture could be established.

text: The

text: Frisians

text: immigrated into North Frisia from the South in two waves. During the 8th century A.D. they mostly settled on the islands

text: Heligoland

text: , Sylt,

text: Föhr

text: Amrum

text: and presumably also in parts of the

text: Eiderstedt

text: peninsula. The coastal marshlands of the mainland were settled in a second wave and after a series of storm surges the Frisians also used to settle on the higher inland

text: geest

text: . While the marshland and its bogs had to be drained, the higher geestland cores of the islands were in turn mostly barren and needed

text: fertilisation

text: before a proper agriculture could be established.

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text: In physics, droplet-shaped waves are casual localized solutions of the wave equation closely related to the X-shaped waves, but, in contrast, possessing a finite support.

text: In

text: physics

text: , droplet-shaped waves are casual localized solutions of the

text: wave equation

text: closely related to the

text: X-shaped waves

text: , but, in contrast, possessing a finite

text: support

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text: Foo helped elevate the popularity of the sport, with his talent, courage, and enthusiasm, and was certainly recognized as one of the greatest big-wave surfers to ever ride the waves. Mark was a favorite subject of photographers, and he had his own cable television surfing program. "If you want to ride the ultimate wave, you have to be willing to pay the ultimate price" was Foo's philosophy, which he certainly lived until the day of his final ride.

text: Foo helped elevate the popularity of the sport, with his talent, courage, and enthusiasm, and was certainly recognized as one of the greatest big-wave surfers to ever ride the waves. Mark was a favorite subject of photographers, and he had his own cable television surfing program. "If you want to ride the ultimate wave, you have to be willing to pay the ultimate price" was Foo's philosophy, which he certainly lived until the day of his final ride.

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answer: No

answer: No

answer: No

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text: The Cribbar is best known for creating annual big waves, popular with experienced big wave surfers from across the world. Wave faces can be in excess of . The Zorba is a reef  further off the coast and can create even higher waves.

text: The Cribbar is best known for creating annual

text: big waves

text: , popular with experienced big wave surfers from across the world. Wave faces can be in excess of . The Zorba is a reef  further off the coast and can create even higher waves.

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answers: Wave faces

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answers: Wave

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answers: annual

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answers: fast

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answers: The Cribbar

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answers: Wave faces

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answers: The Cribbar

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answers: coast

answers: NDQ_006461

answers: create annual big waves

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Whereas the sea state in the storm has a frequency spectrum with more or less always the same shape (i.e. a well defined peak with dominant frequencies within plus or minus 7% of the peak), the swell spectra are more and more narrow, sometimes as 2% or less, as waves disperse further and further away. The result is that wave groups (called sets by surfers) can have a large number of waves.  From about seven waves per group in the storm, this rises to 20 and more in swells from very distant storms.

text: Whereas the sea state in the storm has a

text: frequency spectrum

text: with more or less always the same shape (i.e. a well defined peak with dominant frequencies within plus or minus 7% of the peak), the swell spectra are more and more narrow, sometimes as 2% or less, as waves disperse further and further away. The result is that wave groups (called sets by surfers) can have a large number of waves.  From about seven waves per group in the storm, this rises to 20 and more in swells from very distant storms.

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answers: waves disperse further and further away

answers: NDQ_006453

answers: wave groups

answers: NDQ_006455

answers: storm

answers: NDQ_006456

answers: swell

answers: NDQ_006457

answers: waves disperse further and further away

answers: NDQ_006458

answers: waves disperse further and further away

answers: NDQ_006459

answers: storms

answers: NDQ_006460

answers: Waves

answers: NDQ_006461

answers: waves disperse further and further away

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: After surge from a cyclone has receded, teams of surveyors map high-water marks (HWM) on land, in a rigorous and detailed process that includes photos and written descriptions of the marks. HWMs denote the location and elevation of flood waters from a storm event. When HWMs are analyzed, if the various components of the water height can be broken out so that the portion attributable to surge can be identified, then that mark can be classified as storm surge. Otherwise, it is classified as storm tide. HWMs on land are referenced to a vertical datum (a reference coordinate system). During evaluation, HWMs are divided into four categories based on the confidence in the mark; only HWMs evaluated as "excellent" are used by NHC in post storm analysis of the surge.

text: After surge from a

text: cyclone

text: has receded, teams of surveyors map high-water marks (HWM) on land, in a rigorous and detailed process that includes photos and written descriptions of the marks. HWMs denote the location and elevation of flood waters from a storm event. When HWMs are analyzed, if the various components of the water height can be broken out so that the portion attributable to surge can be identified, then that mark can be classified as storm surge. Otherwise, it is classified as storm tide. HWMs on land are referenced to a vertical datum (a reference coordinate system). During evaluation, HWMs are divided into four categories based on the confidence in the mark; only HWMs evaluated as "excellent" are used by NHC in post storm analysis of the surge.

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answers: HWMs

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answers: storm surge

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answers: NDQ_006460

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answers: NDQ_006461

answers: vertical datum (a reference coordinate system)

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: In New Brunswick, the storm complex produced high winds with gusts of up to 84 mph (135 km/h). The winds downed several trees and power lines which resulted in power outages, with Fredericton being the hardest hit. About 16,000 were without power on the day after the storm struck. The storm produced sustained winds of 76 mph (123 km/h) and gusts to 96 mph (155 km/h) at the Confederation Bridge. There, the wind gust was the highest ever recorded, resulting in the bridge being closed for five hours, the first time the bridge was closed in its history. Waves of up to 30 ft (nine m) in height with a storm surge of over 3.3 ft (one m) hit the northern coastline of Prince Edward Island. Every wharf and many coastal roads from Rustico to East Point were under water from the high waves and storm surge. The winds left much of eastern Prince Edward Island without power.

text: In

text: New Brunswick

text: , the storm complex produced high winds with gusts of up to 84 mph (135 km/h). The winds downed several trees and power lines which resulted in power outages, with

text: Fredericton

text: being the hardest hit. About 16,000 were without power on the day after the storm struck. The storm produced sustained winds of 76 mph (123 km/h) and gusts to 96 mph (155 km/h) at the

text: Confederation Bridge

text: . There, the wind gust was the highest ever recorded, resulting in the bridge being closed for five hours, the first time the bridge was closed in its history. Waves of up to 30 ft (nine m) in height with a storm surge of over 3.3 ft (one m) hit the northern coastline of

text: Prince Edward Island

text: . Every wharf and many coastal roads from

text: Rustico

text: to

text: East Point

text: were under water from the high waves and storm surge. The winds left much of eastern Prince Edward Island without power.

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answers: 96 mph

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answers: high waves and storm surge

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answers: Every wharf and many coastal roads

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answers: storm surge

answers: NDQ_006460

answers: Waves

answers: NDQ_006461

answers: high waves and storm surge

answer: Yes

answer: Yes

answer: No

answer: Yes

answer: No

answer: 1

text: Another factor that contributed to the capsizing was the "squat effect". When a vessel is under way, the movement under it creates low pressure, which has the effect of increasing the vessel's draught. In deep water the effect is small but in shallow water it is greater, because as the water passes underneath it moves faster and causes the draught to increase. This reduced the clearance between the bow doors and water line to 1.5 metres. Although the bow doors were open and 1.5 metres above the water, it was still not enough to cause the ship to capsize, so the investigators looked at the height and volume of water produced by the bow wave. After extensive tests, the investigators found that when the ship travelled at a speed of , the wave was enough to engulf the bow doors. This caused a "step change": if the ship had been sailing at less than 18 knots and not in shallow water, people on the car deck would probably have had time to notice the bow doors were open and close them.

text: Another factor that contributed to the capsizing was the "

text: squat effect

text: ". When a vessel is under way, the movement under it creates low pressure, which has the effect of increasing the vessel's

text: draught

text: . In deep water the effect is small but in shallow water it is greater, because as the water passes underneath it moves faster and causes the draught to increase. This reduced the clearance between the bow doors and water line to 1.5 metres. Although the bow doors were open and 1.5 metres above the water, it was still not enough to cause the ship to capsize, so the investigators looked at the height and volume of water produced by the bow wave. After extensive tests, the investigators found that when the ship travelled at a speed of , the wave was enough to engulf the bow doors. This caused a "step change": if the ship had been sailing at less than 18 knots and not in shallow water, people on the car deck would probably have had time to notice the bow doors were open and close them.

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answers: NDQ_006460

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answers: 0

answers: NDQ_006452

answers: The bow wave

answers: NDQ_006453

answers: shallow water

answers: NDQ_006455

answers: When a vessel is under way

answers: NDQ_006456

answers: slow

answers: NDQ_006457

answers: shallow water

answers: NDQ_006458

answers: shallow water

answers: NDQ_006459

answers: shallow water

answers: NDQ_006460

answers: shallow water

answers: NDQ_006461

answers: the movement under it creates low pressure

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Another surge from the easterlies, combined with the forty-fourth tropical wave of the season, began to develop off the east coast of Luzon in the Philippines on the morning of July 18. At the time, the tropical wave had winds of 15 mph (25 km/h) on its surface. The wave rapidly intensified during the morning and the Joint Typhoon Warning Center upped the system to a tropical depression the same afternoon. The next morning the system was upgraded to a tropical storm and received the name Kate. The new storm had a small, open eyewall which expanded during the day as the storm slowly intensified through and by the late morning of July 20, the storm became a typhoon with winds of 75 mph (120 km/h). That morning, the eye had only a  diameter and had similar surface winds. During the afternoon, the storm made a curve to the southwest from its track and looped back northward. By the morning of July 21, the storm began a northeastern turn towards Taiwan.

text: Another surge from the easterlies, combined with the forty-fourth tropical wave of the season, began to develop off the east coast of

text: Luzon

text: in the Philippines on the morning of July 18. At the time, the tropical wave had winds of 15 mph (25 km/h) on its surface. The wave rapidly intensified during the morning and the Joint Typhoon Warning Center upped the system to a tropical depression the same afternoon. The next morning the system was upgraded to a tropical storm and received the name Kate. The new storm had a small, open eyewall which expanded during the day as the storm slowly intensified through and by the late morning of July 20, the storm became a typhoon with winds of 75 mph (120 km/h). That morning, the eye had only a  diameter and had similar surface winds. During the afternoon, the storm made a curve to the southwest from its track and looped back northward. By the morning of July 21, the storm began a northeastern turn towards Taiwan.

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answers: NDQ_006452

answers: Waves break when they become too tall to be supported by their base

answers: NDQ_006453

answers: tropical wave

answers: NDQ_006455

answers: the easterlies

answers: NDQ_006456

answers: easterlies

answers: NDQ_006457

answers: surface

answers: NDQ_006458

answers: The new storm had a small, open eyewall

answers: NDQ_006459

answers: Typhoon

answers: NDQ_006460

answers: The east coast of Luzon

answers: NDQ_006461

answers: small, open eyewall

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: 1

text: The precursor to Hurricane Bud exited the West Africa coast on May 5 as a tropical wave. The wave slowly intensified as it moved towards the west as an area of thunderstorms, producing showers of the Windward Islands.  On May 12, a low pressure system formed from the tropical wave just south of eastern Panama. Under favorable conditions, it slowly began to organize while east of Tropical Storm Aletta, and after a burst in convection on May 15, the National Hurricane Center began monitoring the system. By early on May 18, the system became nearly stationary while just offshore of Mexico. After wind shear caused it to become less organized later that day, the system began showing signs of development starting on May 19. Although it was re-organizing, the system initially lacked a well-defined surface circulation. On May 20, the system started to rapidly organize while tracking slowly west-northwestward. Later that day, the National Hurricane Center noted that "conditions appear favorable for a tropical depression to form tonight or Monday." It is estimated that Tropical Depression Two-E developed at 1800 UTC on May 20, while located about  south of Acapulco, Guerrero. Although geostationary and microwave satellite imagery indicated moderate easterly wind shear, the National Hurricane Center predicted quick intensification into a hurricane.

text: The precursor to Hurricane Bud exited the

text: West Africa

text: coast on May 5 as a

text: tropical wave

text: . The wave slowly intensified as it moved towards the west as an area of

text: thunderstorm

text: s, producing showers of the

text: Windward Islands

text: .  On May 12, a

text: low pressure system

text: formed from the tropical wave just south of eastern

text: Panama

text: . Under favorable conditions, it slowly began to organize while east of Tropical Storm Aletta, and after a burst in convection on May 15, the

text: National Hurricane Center

text: began monitoring the system. By early on May 18, the system became nearly stationary while just offshore of Mexico. After wind shear caused it to become less organized later that day, the system began showing signs of development starting on May 19. Although it was re-organizing, the system initially lacked a well-defined surface circulation. On May 20, the system started to rapidly organize while tracking slowly west-northwestward. Later that day, the National Hurricane Center noted that "conditions appear favorable for a tropical depression to form tonight or Monday." It is estimated that Tropical Depression Two-E developed at 1800 UTC on May 20, while located about  south of

text: Acapulco

text: Guerrero

text: . Although geostationary and microwave satellite imagery indicated moderate easterly wind shear, the National Hurricane Center predicted quick intensification into a hurricane.

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answers: a hurricane

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answers: Tropical Depression

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answers: tropical

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answers: easterly

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answers: The wave slowly intensified as it moved towards the west

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answers: By early on May 18, the system became nearly stationary

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answers: hurricane

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answers: Waves travel across the ocean

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answers: wind shear

answer: Yes

answer: Yes

answer: No

answer: Yes

answer: No

answer: 1

text: Reaching may, however, put the boat on a course parallel with the crests of the waves.  When the waves are steep, it may be necessary to sail closer to the wind to avoid waves directly on the beam, which create the danger of capsizing.

text: Reaching may, however, put the boat on a course parallel with the crests of the waves.  When the waves are steep, it may be necessary to sail closer to the wind to avoid waves directly on the beam, which create the danger of capsizing.

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answers: waves directly on the beam

answers: NDQ_006453

answers: crests

answers: NDQ_006455

answers: crests

answers: NDQ_006456

answers: parallel

answers: NDQ_006457

answers: Wave energy is lowest at the surface

answers: NDQ_006458

answers: When the waves are steep

answers: NDQ_006459

answers: wind

answers: NDQ_006460

answers: crests

answers: NDQ_006461

answers: sail closer to the wind

answer: No

answer: No

answer: Yes

answer: No

answer: Yes

answer: 1

text: The time is announced by three strokes. While the man fights, he is accompanied by sounds of breaking waves, rumbling earth or the sound of wind, depending on the animal chosen.

text: The time is announced by three strokes. While the man fights, he is accompanied by sounds of breaking waves, rumbling earth or the sound of wind, depending on the animal chosen.

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answers: The time is announced by three strokes

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answers: Friction

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answers: breaking waves

answers: NDQ_006461

answers: rumbling earth

answer: No

answer: Yes

answer: No

answer: No

answer: No

answer: 1

text: For a given topography and bathymetry the surge height is not solely affected by peak wind speed; the size of the storm also affects the peak surge. With any storm the piled up water has an exit path to the sides and this escape mechanism is reduced in proportion to the surge force (for the same peak wind speed) as the storm covers more area.

text: For a given topography and bathymetry the surge height is not solely affected by peak wind speed; the size of the storm also affects the peak surge. With any storm the piled up water has an exit path to the sides and this escape mechanism is reduced in proportion to the surge force (for the same peak wind speed) as the storm covers more area.

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answers: NDQ_006452

answers: peak surge

answers: NDQ_006453

answers: surge

answers: NDQ_006455

answers: storm

answers: NDQ_006456

answers: bathymetry

answers: NDQ_006457

answers: bathymetry

answers: NDQ_006458

answers: With any storm the piled up water has an exit path to the sides

answers: NDQ_006459

answers: storm

answers: NDQ_006460

answers: shoreline

answers: NDQ_006461

answers: the size of the storm also affects the peak surge

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: An atmospheric wave is a periodic disturbance in the fields of atmospheric variables (like surface pressure or geopotential height, temperature, or wind velocity) which may either propagate (traveling wave) or not (standing wave). Atmospheric waves range in spatial and temporal scale from large-scale planetary waves (Rossby waves) to minute sound waves. Atmospheric waves with periods which are harmonics of 1 solar day (e.g. 24 hours, 12 hours, 8 hours... etc.) are known as atmospheric tides.

text: An atmospheric wave is a periodic disturbance in the fields of

text: atmospheric

text: variables (like

text: surface pressure

text: or

text: geopotential height

text: temperature

text: , or

text: wind velocity

text: ) which may either propagate (

text: traveling wave

text: ) or not (

text: standing wave

text: ). Atmospheric waves range in

text: spatial

text: and

text: temporal

text: scale from large-scale planetary waves (

text: Rossby wave

text: s) to minute

text: sound wave

text: s. Atmospheric waves with periods which are

text: harmonics

text: of 1

text: solar day

text: (e.g. 24 hours, 12 hours, 8 hours... etc.) are known as

text: atmospheric tide

text: s.

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answers: standing wave

answers: NDQ_006453

answers: atmospheric tides

answers: NDQ_006455

answers: disturbance

answers: NDQ_006456

answers: standing

answers: NDQ_006457

answers: Atmospheric waves

answers: NDQ_006458

answers: standing wave

answers: NDQ_006459

answers: Rossby waves

answers: NDQ_006460

answers: Atmospheric waves

answers: NDQ_006461

answers: standing wave

answer: Yes

answer: Yes

answer: No

answer: No

answer: No

answer: 1

text: As far as seismic and acoustic waves are concerned, the motion of ocean waves in deep water is, to the leading order, equivalent to a pressure applied at the sea surface. This pressure is nearly equal to the water density times the wave orbital velocity squared. Because of this square, it is not the amplitude of the individual wave trains that matter (red and black lines in the figures) but the amplitude of the sum, the wave groups (blue line in figures).

text: As far as seismic and acoustic waves are concerned, the motion of ocean waves in deep water is, to the

text: leading order

text: , equivalent to a pressure applied at the sea surface. This pressure is nearly equal to the water density times the wave

text: orbital velocity

text: squared. Because of this square, it is not the amplitude of the individual wave trains that matter (red and black lines in the figures) but the amplitude of the sum, the wave groups (blue line in figures).

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answers: waves break when they become too tall

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answers: water density times the wave orbital velocity squared

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answer: No

answer: No

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text: Alberta's electrical demand varies throughout the day and across the seasons. When individuals are fixing supper and using home appliances, demand for power goes up, as it does during heat waves and cold snaps. It tapers off during spring and fall. Like other mechanical devices, generators fail from time to time. If they are wind-powered, their output varies with the wind.

text: Alberta's electrical demand varies throughout the day and across the seasons. When individuals are fixing supper and using home appliances, demand for power goes up, as it does during heat waves and cold snaps. It tapers off during spring and fall. Like other mechanical devices, generators fail from time to time. If they are wind-powered, their output varies with the wind.

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answers: heat waves

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answers: heat waves

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answers: fast

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answers: It tapers off

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answers: It tapers off

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answers: wind

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answers: varies with the wind

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The storm caused an estimated $1.5 billion (1991 US dollars) in damage. The high velocity wind and the storm surge devastated the coastline. Although a concrete levee was in place near the mouth of the Karnaphuli River in Patenga, it was washed away by the storm surge. The cyclone uprooted a 100-ton crane from the Port of Chittagong, and smashed it on the Karnaphuli River Bridge, effectively breaking it into two partitions. A large number of boats and smaller ships ran aground. Bangladesh Navy and Bangladesh Air Force, both of which had bases in Chittagong, were also heavily hit. The Isha Khan Naval Base at Patenga was flooded, with heavy damages to the ships. Most of the fighter planes belonging to the air force were damaged.  Approximately 1 million homes were destroyed, leaving about 10 million people (a substantial portion of Bangladesh's population) homeless. The extensive damage caused the price of building materials to greatly increase.

text: The storm caused an estimated $1.5 billion (1991

text: US dollars

text: ) in damage. The high velocity wind and the

text: storm surge

text: devastated the coastline. Although a concrete levee was in place near the mouth of the

text: Karnaphuli River

text: in

text: Patenga

text: , it was washed away by the storm surge. The cyclone uprooted a 100-ton crane from the

text: Port of Chittagong

text: , and smashed it on the

text: Karnaphuli River Bridge

text: , effectively breaking it into two partitions. A large number of boats and smaller ships ran aground.

text: Bangladesh Navy

text: and

text: Bangladesh Air Force

text: , both of which had bases in Chittagong, were also heavily hit. The Isha Khan Naval Base at Patenga was flooded, with heavy damages to the ships. Most of the fighter planes belonging to the air force were damaged.  Approximately 1 million homes were destroyed, leaving about 10 million people (a substantial portion of Bangladesh's population) homeless. The extensive damage caused the price of building materials to greatly increase.

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answers: The Karnaphuli River Bridge

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answers: high velocity wind

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answers: high velocity

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answers: surface

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answers: A large number of boats and smaller ships ran aground

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answers: boats and smaller ships

answers: NDQ_006460

answers: Waves

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answers: high velocity wind and the storm surge

answer: Yes

answer: Yes

answer: No

answer: No

answer: No

answer: 1

text: A tropical cyclone is a storm system characterized by a low pressure center and numerous thunderstorms that produce strong winds and flooding rain. A tropical cyclone feeds on heat released when moist air rises, resulting in condensation of water vapor contained in the moist air.  Tropical cyclones may produce torrential rain, high waves, and damaging storm surge.  Heavy rains produce significant inland flooding. Storm surges may produce extensive coastal flooding up to  from the coastline.

text: A tropical cyclone is a storm system characterized by a

text: low pressure

text: center and numerous

text: thunderstorms

text: that produce strong winds and flooding

text: rain

text: . A tropical cyclone feeds on heat released when moist air rises, resulting in

text: condensation

text: of

text: water vapor

text: contained in the moist air.  Tropical cyclones may produce torrential rain, high waves, and damaging

text: storm surge

text: .  Heavy rains produce significant inland flooding. Storm surges may produce extensive coastal

text: flood

text: ing up to  from the coastline.

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answers: high waves

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answers: Waves

answers: NDQ_006461

answers: low pressure

answer: No

answer: No

answer: Yes

answer: No

answer: No

answer: 1

text: According to one source, when the bottom fell out of the Klondike market, Ocean Wave was left with nothing to do.  In December 1898, Ocean Wave was taken from Tacoma to the Fraser River in British Columbia to be placed in lay up for an indefinite time.  The owners were reported to have been afraid to keep the vessel in the “teredo-invested water” of Puget Sound.

text: According to one source, when the bottom fell out of the Klondike market, Ocean Wave was left with nothing to do.  In December 1898, Ocean Wave was taken from Tacoma to the

text: Fraser River

text: in

text: British Columbia

text: to be placed in lay up for an indefinite time.  The owners were reported to have been afraid to keep the vessel in the “

text: teredo

text: -invested water” of Puget Sound.

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answers: teredo-invested water

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answers: the bottom fell out

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answers: indefinite

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answers: Puget Sound

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answer: No

answer: No

answer: No

answer: No

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text: On many of the southern shores there isn’t much wave action, as there aren’t long stretches of sea, where they can grow big before washing ashore creating beaches. Small waves make narrow beaches. Big waves make wide beaches.

text: On many of the southern shores there isn’t much wave action, as there aren’t long stretches of sea, where they can grow big before washing ashore creating beaches. Small waves make narrow beaches. Big waves make wide beaches.

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answers: Big waves

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answers: beach

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answers: long stretches of sea

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answers: big

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answers: surface

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answers: Small waves

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answers: stretches of sea

answers: NDQ_006460

answers: creating beaches

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answers: Small waves make narrow beaches

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: In Texas, strong winds were recorded in Harlingen where sustained winds reached  and gusted to . Elsewhere in Texas, large portions of the state east of where Hermine's center tracked recorded gale-force-winds. Along the coast, the system also brought a storm surge, peaking at  in Port Aransas. Damage over the lower Rio Grande Valley was generally minor. Some trees and power lines were knocked down as a result of the high winds, resulting in power outages over the area. About 30,000 customers lost power at one time or another during the storm in the region. The hardest hit were in Cameron and Willacy Counties. In central Texas, an estimated 100,000 residences were left without power, mainly in Bexar County, due to downed trees. According to surveys of the region, roughly 300 trees were downed by the storm. In Georgetown, where the heaviest rain fell, RV parks and nearby Interstate 35 were flooded, prompting a few evacuations.

text: In Texas, strong winds were recorded in

text: Harlingen

text: where sustained winds reached  and gusted to . Elsewhere in Texas, large portions of the state east of where Hermine's center tracked recorded gale-force-winds. Along the coast, the system also brought a

text: storm surge

text: , peaking at  in

text: Port Aransas

text: . Damage over the lower

text: Rio Grande Valley

text: was generally minor. Some trees and power lines were knocked down as a result of the high winds, resulting in power outages over the area. About 30,000 customers lost power at one time or another during the storm in the region. The hardest hit were in

text: Cameron

text: and

text: Willacy

text: Counties. In central Texas, an estimated 100,000 residences were left without power, mainly in

text: Bexar County

text: , due to downed trees. According to surveys of the region, roughly 300 trees were downed by the storm. In Georgetown, where the heaviest rain fell,

text: RV

text: parks and nearby

text: Interstate 35

text: were flooded, prompting a few evacuations.

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answers: storm surge

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answers: storm surge

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answers: storm surge

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answers: fast

answers: NDQ_006457

answers: Gale force-winds

answers: NDQ_006458

answers: storm surge, peaking at in Port Aransas

answers: NDQ_006459

answers: storm surge

answers: NDQ_006460

answers: storm surge

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answers: high winds

answer: Yes

answer: Yes

answer: No

answer: Yes

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answer: 1

text: The western side of the hurricane caused sustained tropical storm-force winds, high waves, and storm surge along much of the New Jersey coast.  In Atlantic City, the surge destroyed much of the boardwalk, and the bridge between Atlantic City and Brigantine collapsed, stranding at least 2,000.  Additionally, the surge inundated several coastal communities; Wildwood was under  of water at the height of the storm, and in Bay Head, the boardwalk was destroyed and dozens of cottages washed into the ocean.  Crops sustained wind damage.  The maximum recorded wind gust was 70 mph at Sandy Hook.

text: The western side of the hurricane caused sustained tropical storm-force winds, high waves, and storm surge along much of the New Jersey coast.  In

text: Atlantic City

text: , the surge destroyed much of the boardwalk, and the bridge between Atlantic City and

text: Brigantine

text: collapsed, stranding at least 2,000.  Additionally, the surge inundated several coastal communities;

text: Wildwood

text: was under  of water at the height of the storm, and in

text: Bay Head

text: , the boardwalk was destroyed and dozens of cottages washed into the ocean.  Crops sustained wind damage.  The maximum recorded wind gust was 70 mph at

text: Sandy Hook

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answers: high

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answers: storm surge

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answers: tropical storm

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answers: ocean

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answers: high waves

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answers: high waves

answers: NDQ_006459

answers: hurricane

answers: NDQ_006460

answers: Waves

answers: NDQ_006461

answers: high waves

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: 1

text: During breaking, a deformation (usually a bulge) forms at the wave crest, either leading side of which is known as the "toe." Parasitic capillary waves are formed, with short wavelengths. Those above the "toe" tend to have much longer wavelengths. This theory is anything but perfect, however, as it is linear. There have been a couple non-linear theories of motion (regarding waves). One put forth uses a perturbation method to expand the description all the way to the third order, and better solutions have been found since then. As for wave deformation, methods much like the boundary integral method and the Boussinesq model have been created.

text: During breaking, a deformation (usually a bulge) forms at the wave crest, either leading side of which is known as the "toe." Parasitic capillary waves are formed, with short wavelengths. Those above the "toe" tend to have much longer wavelengths. This theory is anything but perfect, however, as it is linear. There have been a couple non-linear theories of motion (regarding waves). One put forth uses a

text: perturbation method

text: to expand the description all the way to the third order, and better solutions have been found since then. As for wave deformation, methods much like the

text: boundary integral method

text: and the

text: Boussinesq model

text: have been created.

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answers: Those above the "toe" tend to have much longer wavelengths

answers: NDQ_006453

answers: a bulge

answers: NDQ_006455

answers: breaking

answers: NDQ_006456

answers: non-linear

answers: NDQ_006457

answers: Wave energy is lowest at the surface and increases with depth

answers: NDQ_006458

answers: Parasitic capillary waves

answers: NDQ_006459

answers: wave crest

answers: NDQ_006460

answers: shoreline

answers: NDQ_006461

answers: Parasitic capillary waves are formed

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: No

answer: 1

text: Through the wind stress, the wind generates ocean surface waves; the longer waves have a phase velocity tending towards the wind speed. Momentum of the surface winds is transferred into the energy flux by the ocean surface waves. The increased roughness of the ocean surface, by the presence of the waves, changes the wind near the surface.

text: Through the wind stress, the wind generates

text: ocean surface wave

text: s; the longer waves have a

text: phase velocity

text: tending towards the

text: wind speed

text: Momentum

text: of the surface winds is transferred into the energy

text: flux

text: by the ocean surface waves. The increased

text: roughness

text: of the ocean surface, by the presence of the waves, changes the wind near the surface.

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answers: surface waves

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answers: ocean surface waves

answers: NDQ_006455

answers: the wind

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answers: faster

answers: NDQ_006457

answers: surface

answers: NDQ_006458

answers: increased roughness of the ocean surface

answers: NDQ_006459

answers: the wind

answers: NDQ_006460

answers: surface

answers: NDQ_006461

answers: surface waves

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: It was the usual practice for power transformers to have a 5 volt insulated winding for rectifier filaments, and a 6.3 volt winding for all the other heaters; virtually all valves with 5V filament are rectifiers with cathode connected to heater, in practice full-wave (usable as half-wave by strapping both anodes together), e.g. GZ34. For lower-voltage lower-power requirements, rectifiers with 6.3V heaters and insulated cathodes such as the EZ80 were used, connected to the common filament supply. There is no special nomenclature for EHT rectifiers for cathode-ray tubes; the EY51 and EY86 were rated at 17kV with an average current of 350 microamps. The GY501 is another example (31kV at 1.7mA and used the rare B9D base). In practice most "xY" half-wave rectifiers are EHT types; but there are plenty of exceptions.

text: It was the usual practice for power transformers to have a 5 volt insulated winding for rectifier filaments, and a 6.3 volt winding for all the other heaters; virtually all valves with 5V filament are rectifiers with cathode connected to heater, in practice full-wave (usable as half-wave by strapping both anodes together), e.g. GZ34. For lower-voltage lower-power requirements, rectifiers with 6.3V heaters and insulated cathodes such as the EZ80 were used, connected to the common filament supply. There is no special nomenclature for

text: EHT

text: rectifiers for

text: cathode-ray tube

text: s; the EY51 and EY86 were rated at 17kV with an average current of 350 microamps. The GY501 is another example (31kV at 1.7mA and used the rare B9D base). In practice most "xY" half-wave rectifiers are EHT types; but there are plenty of exceptions.

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answers: half-wave

answers: NDQ_006453

answers: Sea level rise

answers: NDQ_006455

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answers: NDQ_006456

answers: half-wave

answers: NDQ_006457

answers: half-wave

answers: NDQ_006458

answers: half-wave

answers: NDQ_006459

answers: cathode

answers: NDQ_006460

answers: Wave

answers: NDQ_006461

answers: insulated cathodes

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Infragravity waves are surface gravity waves with frequencies lower than the wind waves – consisting of both wind sea and swell – thus corresponding with the part of the wave spectrum lower than the frequencies directly generated by forcing through the wind.

text: Infragravity waves are

text: surface gravity wave

text: s with

text: frequencies

text: lower than the

text: wind wave

text: s – consisting of both

text: wind sea

text: and

text: swell

text: – thus corresponding with the part of the

text: wave spectrum

text: lower than the frequencies directly generated by

text: forcing

text: through the wind.

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text: • Sources of wind wave generation: Sea water wave is generated by many kinds of disturbances such as Seismic events, gravity, and crossing wind. The generation of wind wave is initiated by the disturbances of cross wind field on the surface of the sea water. Two major Mechanisms of surface wave formation by winds (a.k.a.‘The Miles-Phillips Mechanism’) and other sources (ex. earthquakes) of wave formation can explain the generation of wind waves.

text: • Sources of wind wave generation: Sea water wave is generated by many kinds of disturbances such as Seismic events, gravity, and crossing wind. The generation of wind wave is initiated by the disturbances of cross wind field on the surface of the sea water. Two major Mechanisms of surface wave formation by winds (a.k.a.‘The Miles-Phillips Mechanism’) and other sources (ex. earthquakes) of wave formation can explain the generation of wind waves.

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text: After returning to Japan from the United States in 2011, Hamada began working for Pro Wrestling Wave, where she aligned herself with the villainous Black Dahlia stable. On July 2, 2012, Hamada signed a contract to officially make Wave her new home promotion. On October 6, 2013, Hamada and her Las Aventureras tag team partner Yuu Yamagata won the 2013 Dual Shock Wave tournament. On October 30, Hamada and Yamagata defeated the Classic Gals (Cherry and Shuu Shibutani) to win the Wave Tag Team Championship, Hamada's first title in Wave. After a reign of 270 days, the longest in the title's history, Hamada and Yamagata lost the title to Yankii Nichokenju (Isami Kodaka and Yuko Miyamoto) on July 27, 2014. They regained the title from Revolucion Amandla (Kyoko Kimura and Tomoka Nakagawa) on October 29. On February 11, 2015, Hamada became a double champion, when she defeated Hikaru Shida for the Wave Single Championship. On March 15, Hamada and Yamagata lost the Wave Tag Team Championship to Mio Shirai and Misaki Ohata. On October 30, Hamada and Yamagata won the Wave Tag Team Championship for the third time, when they defeated Kayoko Haruyama and Tsubasa Kuragaki in the finals of the 2015 Dual Shock Wave tournament. On December 27, Hamada lost the Wave Single Championship to her tag team partner Yuu Yamagata. On August 7, 2016, Hamada and Yamagata lost the Wave Tag Team Championship to Misaki Ohata and Ryo Mizunami.

text: After returning to Japan from the

text: United States

text: in 2011, Hamada began working for

text: Pro Wrestling Wave

text: , where she aligned herself with the

text: villainous

text: Black Dahlia

entity_name: Glossary of professional wrestling terms

text: stable

text: . On July 2, 2012, Hamada signed a contract to officially make Wave her new home promotion. On October 6, 2013, Hamada and her Las Aventureras tag team partner Yuu Yamagata won the

text: 2013 Dual Shock Wave

text: tournament. On October 30, Hamada and Yamagata defeated the Classic Gals (Cherry and

text: Shuu Shibutani

text: ) to win the

text: Wave Tag Team Championship

text: , Hamada's first title in Wave. After a reign of 270 days, the longest in the title's history, Hamada and Yamagata lost the title to

text: Yankii Nichokenju

text: Isami Kodaka

text: and

text: Yuko Miyamoto

text: ) on July 27, 2014. They regained the title from Revolucion Amandla (

text: Kyoko Kimura

text: and Tomoka Nakagawa) on October 29. On February 11, 2015, Hamada became a double champion, when she defeated

text: Hikaru Shida

text: for the

text: Wave Single Championship

text: . On March 15, Hamada and Yamagata lost the Wave Tag Team Championship to Mio Shirai and Misaki Ohata. On October 30, Hamada and Yamagata won the Wave Tag Team Championship for the third time, when they defeated

text: Kayoko Haruyama

text: and

text: Tsubasa Kuragaki

text: in the finals of the

text: 2015 Dual Shock Wave

text: tournament. On December 27, Hamada lost the Wave Single Championship to her tag team partner Yuu Yamagata. On August 7, 2016, Hamada and Yamagata lost the Wave Tag Team Championship to Misaki Ohata and Ryo Mizunami.

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answers: On March 15, Hamada and Yamagata lost the Wave Tag Team Championship

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answer: No

answer: No

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text: By August 26, the possibility of unprecedented cataclysm was already being considered. Many of the computer models had shifted the potential path of Katrina  westward from the Florida Panhandle, putting the city of New Orleans directly in the center of their track probabilities; the chances of a direct hit were forecast at 17%, with strike probability rising to 29% by August 28. This scenario was considered a potential catastrophe because some parts of New Orleans and the metro area are below sea level. Since the storm surge produced by the hurricane's right-front quadrant (containing the strongest winds) was forecast to be , emergency management officials in New Orleans feared that the storm surge could go over the tops of levees protecting the city, causing major flooding.

text: By August 26, the possibility of unprecedented cataclysm was already being considered. Many of the computer models had shifted the potential path of Katrina  westward from the Florida Panhandle, putting the city of New Orleans directly in the center of their track probabilities; the chances of a direct hit were forecast at 17%, with strike probability rising to 29% by August 28. This scenario was considered a potential catastrophe because some parts of New Orleans and the metro area are below sea level. Since the storm surge produced by the hurricane's right-front quadrant (containing the strongest winds) was forecast to be , emergency management officials in New Orleans feared that the storm surge could go over the tops of levees protecting the city, causing major flooding.

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answers: hurricane

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answers: storm surge

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answer: Yes

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answer: 1

text: In full-wave rectification both halves of the AC waveform are utilised.  The cathode is connected to the + side of the DC load, the other side being connected to the center tap of the transformer secondary winding, which always remains at zero potential with respect to ground or earth. For each AC phase, a wire from each end of that phase winding is connected to a separate anode "arm" on the mercury-arc rectifier. When the voltage at each anode becomes positive, it will begin to conduct through the mercury vapor from the cathode.  As the anodes of each AC phase are fed from opposite ends of the centre tapped transformer winding, one will always be positive with respect to the center tap and both halves of the AC Waveform will cause current to flow in one direction only through the load. This rectification of the whole AC waveform is thus called full-wave rectification.

text: In full-wave rectification both halves of the AC waveform are utilised.  The

text: cathode

text: is connected to the + side of the DC load, the other side being connected to the

text: center tap

text: of the

text: transformer

text: secondary winding, which always remains at zero potential with respect to ground or earth. For each AC phase, a wire from each end of that phase winding is connected to a separate

text: anode

text: "arm" on the mercury-arc rectifier. When the voltage at each anode becomes positive, it will begin to conduct through the mercury vapor from the cathode.  As the anodes of each AC phase are fed from opposite ends of the centre tapped transformer winding, one will always be positive with respect to the center tap and both halves of the AC Waveform will cause current to flow in one direction only through the load. This rectification of the whole AC waveform is thus called full-wave rectification.

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answers: AC Waveform

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answers: Sea level rise

answers: NDQ_006455

answers: When

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answers: one direction only

answers: NDQ_006457

answers: Wave energy is lowest at the surface and increases with depth

answers: NDQ_006458

answers: rectification of the whole AC Waveform

answers: NDQ_006459

answers: mercury-arc rectifier

answers: NDQ_006460

answers: Earth

answers: NDQ_006461

answers: current to flow in one direction only through the load

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: OPC began to produce experimental gridded significant wave height forecasts in 2006, a first step toward digital marine service for high seas and offshore areas. Additional gridded products such as surface pressure and winds are under development. Recently, OPC began to use the NWS operational extratropical storm surge model output to provide experimental extratropical storm surge guidance for coastal weather forecast offices to assist them in coastal flood warning and forecast operations.

text: OPC began to produce experimental gridded significant wave height forecasts in 2006, a first step toward digital marine service for high seas and offshore areas. Additional gridded products such as surface pressure and winds are under development. Recently, OPC began to use the NWS operational extratropical

text: storm surge

text: model output to provide experimental

text: extratropical storm

text: surge guidance for coastal weather forecast offices to assist them in

text: coastal flood warning

text: and forecast operations.

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text: The origins of Tropical Depression Eighteen-E were from a tropical wave that exited the coast of Africa on October 7. It briefly spawned a low-pressure area as the wave continued westward without development. On October 20, the wave entered the Pacific Ocean, developing an area of thunderstorms about four days later. By 1200 UTC on October 26, a tropical depression formed about 155 mi (260 km) south of Manzanillo. Initially, Tropical Depression Eighteen-E was located in an area of light wind shear, and the NHC anticipated further organization and strengthening to near hurricane status. The tropical depression initially maintained a steady westward motion away from the Mexican coastline, due to a ridge north of the cyclone. By October 17, convection had decreased, and the depression was not forecast to intensify as much. Possibly due to intrusion of dry air, the circulation became exposed from the thunderstorms, and having weakened, it turned to a southward drift. By 0000 UTC on October 28, the system had weakened to a non-convective remnant low, which dissipated the following day.

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answers: Tropical Depression Eighteen-E

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answers: Tropical Depression

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answers: tropical wave

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answers: westward

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answers: Tropical Depression Eighteen-E

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answers: The origins of Tropical Depression Eighteen-E were from a tropical wave

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answers: Tropical Depression Eighteen-E

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answer: No

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answer: 1

text: The strain wave gearing theory is based on elastic dynamics and utilizes the flexibility of metal. The mechanism has three basic components: a wave generator, a flexspline, and a circular spline. More complex versions have a fourth component normally used to shorten the overall length or to increase the gear reduction within a smaller diameter, but still follow the same basic principles.The wave generator is made up of two separate parts: an elliptical disk called a wave generator plug and an outer ball bearing. The gear plug is inserted into the bearing, giving the bearing an elliptical shape as well.The flexspline is like a shallow cup. The sides of the spline are very thin, but the bottom is thick and rigid. This results in significant flexibility of the walls at the open end due to the thin wall, but in the closed side being quite rigid and able to be tightly secured (to a shaft, for example). Teeth are positioned radially around the outside of the open end of the flexspline. The flexspline fits tightly over the wave generator, so that when the wave generator plug is rotated, the flexspline deforms to the shape of a rotating ellipse but does not rotate with the wave generator.The circular spline is a rigid circular ring with teeth on the inside. The flexspline and wave generator are placed inside the circular spline, meshing the teeth of the flexspline and the circular spline. Because the flexspline has an elliptical shape, its teeth only actually mesh with the teeth of the circular spline in two regions on opposite sides of the flexspline, along the major axis of the ellipse.Assume that the wave generator is the input rotation. As the wave generator plug rotates, the flexspline teeth which are meshed with those of the circular spline change. The major axis of the flexspline actually rotates with wave generator, so the points where the teeth mesh revolve around the center point at the same rate as the wave generator. The key to the design of the strain wave gear is that there are fewer teeth (for example two fewer) on the flexspline than there are on the circular spline. This means that for every full rotation of the wave generator, the flexspline would be required to rotate a slight amount (two teeth, for example) backward relative to the circular spline. Thus the rotation action of the wave generator results in a much slower rotation of the flexspline in the opposite direction.For a strain wave gearing mechanism, the gearing reduction ratio can be calculated from the number of teeth on each gear:

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answers: elliptical shape

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answers: 0: The answer is not relevant or complete at all.

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answers: flexspline is like a shallow cup

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answers: flexspline fits tightly over the wave generator

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answers: flexspline does not rotate with the wave generator.

answers: NDQ_006453

answers: changes with the wave generator

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answers: the wave generator plug is rotated

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answers: oscillating

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answers: flexspline teeth mesh with those of the circular spline change

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answers: The major axis of the flexspline actually rotates with wave generator

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answers: ellipse

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answers: The major axis of the ellipse

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answers: because the flexspline has an elliptical shape

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Battered by wind, rain and storm surge, some beachfront neighborhoods were completely leveled. Preliminary estimates by Mississippi officials calculated that 90% of the structures within half a mile of the coastline were completely destroyed, and that storm surges traveled as much as  inland in portions of the state's coast. One apartment complex with approximately thirty residents seeking shelter inside collapsed. More than half of the 13 casinos in the state, which were floated on barges to comply with Mississippi land-based gambling laws, were washed hundreds of yards inland by waves.

text: Battered by wind, rain and storm surge, some beachfront neighborhoods were completely leveled. Preliminary estimates by Mississippi officials calculated that 90% of the structures within half a mile of the coastline were completely destroyed, and that storm surges traveled as much as  inland in portions of the state's coast. One apartment complex with approximately thirty residents seeking shelter inside collapsed. More than half of the 13 casinos in the state, which were floated on barges to comply with Mississippi land-based gambling laws, were washed hundreds of yards inland by waves.

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answers: waves

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answers: storm surge

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answers: storm surges

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answers: inland

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answers: surface

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answers: Beachfront neighborhoods were completely leveled

answers: NDQ_006459

answers: barges

answers: NDQ_006460

answers: beachfront neighborhoods

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answer: Yes

answer: Yes

answer: Yes

answer: No

answer: No

answer: 1

text: Two main processes can explain the transfer of energy from the short wind waves to the long infragravity waves, and both are important in shallow water and for steep wind waves. The most common process is the subharmonic interaction of trains of wind waves which was first observed by Munk and Tucker and explained by Longuet-Higgins and Stewart. Because wind waves are not monochromatic they form groups. The Stokes drift induced by these groupy waves transports more water where the waves are highest. The waves also push the water around in a way that can be interpreted as a force: the divergence of the radiation stresses. Combining mass and momentum conservation, Longuet-Higgins and Stewart give, with three different methods, the now well-known result. Namely, the mean sea level oscillates with a wavelength that is equal to the length of the group, with a low level where the wind waves are highest and a high level where these waves are lowest. This oscillation of the sea surface is proportional to the square of the short wave amplitude and becomes very large when the group speed approaches the speed of shallow water waves. The details of this process are modified when the bottom is sloping, which is generally the case near the shore, but the theory captures the important effect, observed in most conditions, that the high water of this 'surf beat' arrives with the waves of lowest amplitude.

text: Two main processes can explain the transfer of energy from the short wind waves to the long infragravity waves, and both are important in shallow water and for steep wind waves. The most common process is the

text: subharmonic

text: interaction of trains of wind waves which was first observed by Munk and Tucker and explained by Longuet-Higgins and Stewart. Because wind waves are not

text: monochromatic

text: they form groups. The

text: Stokes drift

text: induced by these groupy waves transports more water where the waves are highest. The waves also push the water around in a way that can be interpreted as a force: the divergence of the radiation stresses. Combining mass and momentum conservation, Longuet-Higgins and Stewart give, with three different methods, the now well-known result. Namely, the mean sea level oscillates with a wavelength that is equal to the length of the group, with a low level where the wind waves are highest and a high level where these waves are lowest. This oscillation of the sea surface is proportional to the square of the short wave amplitude and becomes very large when the

text: group speed

text: approaches the speed of shallow water waves. The details of this process are modified when the bottom is sloping, which is generally the case near the shore, but the theory captures the important effect, observed in most conditions, that the high water of this 'surf beat' arrives with the waves of lowest amplitude.

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answers: steep wind waves

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answers: The Stokes drift induced by these groupy waves

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answers: The Stokes drift

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answers: Stokes drift induced by these groupy waves transports more water where the waves are highest

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: 1

text: Individually, each of these waves travels at the speed of light in vacuum, not at the (slower) speed of light in glass. Yet when the waves are added up, they surprisingly create only a wave that travels at the slower speed.

text: Individually, each of these waves travels at the speed of light in vacuum, not at the (slower) speed of light in glass. Yet when the waves are added up, they surprisingly create only a wave that travels at the slower speed.

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answers: wave that travels at the slower speed

answers: NDQ_006453

answers: a wave

answers: NDQ_006455

answers: added up

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answers: faster

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answers: waves travels at the speed of light in vacuum

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answers: waves travels at the speed of light in vacuum

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answers: added up

answers: NDQ_006460

answers: wave travels at the slower speed

answers: NDQ_006461

answers: each of these waves travels at the speed of light in vacuum

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Waves are formed in a similar manner to hydraulics and are sometimes also considered hydraulics as well.  Waves are noted by the large smooth face on the water rushing down. Sometimes a particularly large wave will also be followed by a "wave train", a long series of waves. These standing waves can be smooth or, particularly the larger ones, can be breaking waves (also called "whitecaps" or "haystacks").

text: Wave

text: s are formed in a similar manner to hydraulics and are sometimes also considered hydraulics as well.  Waves are noted by the large smooth face on the water rushing down. Sometimes a particularly large wave will also be followed by a "wave train", a long series of waves. These

text: standing wave

text: s can be smooth or, particularly the larger ones, can be breaking waves (also called "whitecaps" or "haystacks").

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answers: breaking waves

answers: NDQ_006453

answers: whitecaps

answers: NDQ_006455

answers: water rushing down

answers: NDQ_006456

answers: rushing

answers: NDQ_006457

answers: Wave energy is lowest at the surface

answers: NDQ_006458

answers: Waves are formed in a similar manner to hydraulics

answers: NDQ_006459

answers: wave train

answers: NDQ_006460

answers: Waves are formed in a similar manner to hydraulics

answers: NDQ_006461

answers: water rushing down

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Waves are disturbances that carry energy as they move. Mechanical waves propagate through a medium – air or water, making it oscillate as they pass by. Wind waves are sea surface waves that create the characteristic chaotic pattern of any large body of water, though their statistical behaviour can be predicted with wind wave models. As waves in water or wind pass over sand, they create patterns of ripples. When winds blow over large bodies of sand, they create dunes, sometimes in extensive dune fields as in the Taklamakan desert. Dunes may form a range of patterns including crescents, very long straight lines, stars, domes, parabolas, and longitudinal or Seif ('sword') shapes.

text: Wave

text: s are disturbances that carry energy as they move.

text: Mechanical wave

text: s propagate through a medium – air or water, making it

text: oscillate

text: as they pass by.

text: Wind wave

text: s are sea

text: surface wave

text: s that create the characteristic chaotic pattern of any large body of water, though their statistical behaviour can be predicted with wind wave models. As waves in water or wind pass over sand, they create patterns of ripples. When winds blow over large bodies of sand, they create

text: dune

text: s, sometimes in extensive dune fields as in the

text: Taklamakan

text: desert. Dunes may form a range of patterns including crescents, very long straight lines, stars, domes, parabolas, and longitudinal or Seif ('sword') shapes.

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answers: Parabolas

answers: NDQ_006453

answers: Ripples

answers: NDQ_006455

answers: mechanical waves propagate

answers: NDQ_006456

answers: oscillate

answers: NDQ_006457

answers: Surface waves

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answers: Ripples

answers: NDQ_006459

answers: wind

answers: NDQ_006460

answers: Sea surface waves

answers: NDQ_006461

answers: mechanical waves propagate

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: 1

text: The origins of Hurricane Jeanne were from a tropical wave that moved off the coast of Africa on September 7. Containing a scattered area of moderate convection, the wave tracked westward at 12–17 mph (19–28 km/h), located to the south of a large ridge. The system initially showed no signs of development, with unfavorably dry air persisting across the region. On September 11, convection became slightly better organized, and the next day broad cyclonic turning became evident. However, overall development was hindered by upper-level wind shear from Hurricane Ivan in the Caribbean Sea, as well as from an upper-level low to the north of the wave.

text: The origins of Hurricane Jeanne were from a

text: tropical wave

text: that moved off the coast of Africa on September 7. Containing a scattered area of moderate

text: convection

text: , the wave tracked westward at 12–17 mph (19–28 km/h), located to the south of a large

text: ridge

text: . The system initially showed no signs of development, with unfavorably dry air persisting across the region. On September 11, convection became slightly better organized, and the next day broad cyclonic turning became evident. However, overall development was hindered by upper-level

text: wind shear

text: from

text: Hurricane Ivan

text: in the

text: Caribbean Sea

text: , as well as from an upper-level low to the north of the wave.

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answers: upper-level wind shear

answers: NDQ_006453

answers: tropical wave

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answers: tropical

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answers: westward

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answers: surface

answers: NDQ_006458

answers: The origins of Hurricane Jeanne

answers: NDQ_006459

answers: convection

answers: NDQ_006460

answers: It moves off the coast

answers: NDQ_006461

answers: moderate convection

answer: Yes

answer: Yes

answer: No

answer: No

answer: No

answer: 1

text: This hurricane could perhaps generate enormous waves in the ocean and the waves would migrate outwards. Oceanographers should test how high these waves would be in the postulated nearby swamps and delta area. They would be wind driven waves and would not reach from the top of an ocean to the bottom like a tsunami. Nonetheless, waves as big and as devastating as those that humans call freak waves might be regular.  Simple bacterial and algal life would not be threatened.

text: This hurricane could perhaps generate enormous waves in the ocean and the waves would migrate outwards.

text: Oceanographers

text: should test how high these waves would be in the postulated nearby swamps and delta area. They would be wind driven waves and would not reach from the top of an ocean to the bottom like a

text: tsunami

text: . Nonetheless, waves as big and as devastating as those that humans call

text: freak waves

text: might be regular.  Simple bacterial and algal life would not be threatened.

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answers: Waves break when they become too tall to be supported by their base

answers: NDQ_006453

answers: swamps

answers: NDQ_006455

answers: wind driven

answers: NDQ_006456

answers: bottom

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answers: They would be wind driven waves

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answers: would not reach from the top of an ocean to the bottom like a tsunami

answers: NDQ_006459

answers: wind

answers: NDQ_006460

answers: They would be wind driven waves

answers: NDQ_006461

answers: wind driven waves

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: 1

text: A tropical wave emerged from the west coast of Africa on August 30 and tracked westward across the Atlantic Ocean, maintaining a vigorous area of convection along the wave axis. By September 1 most of the  deep convection had been stripped away by southwesterly wind shear.  Despite this, the wave remained well-defined as it continued west-northwest. The wave split into two pieces; the northern portion passed between the Leeward Islands and Hurricane Maria on September 3, while the southern portion moved into the Caribbean Sea. On September 4, the northern portion of the wave began to interact with an upper-level low pressure system and an elongated trough that was located between Bermuda and the Leeward Islands—the same trough which contributed to the development of Hurricane Ophelia. As a result of the low wind shear, convection redeveloped and organized along the wave axis. Convective banding formed around a broad surface low. It is estimated that the system developed into a tropical depression at 1800 UTC on September 5. At the time it was located approximately  to the south-southwest of Bermuda.

text: A

text: tropical wave

text: emerged from the west coast of Africa on August 30 and tracked westward across the Atlantic Ocean, maintaining a vigorous area of

text: convection

text: along the wave axis. By September 1 most of the  deep convection had been stripped away by southwesterly wind shear.  Despite this, the wave remained well-defined as it continued west-northwest. The wave split into two pieces; the northern portion passed between the

text: Leeward Islands

text: and

text: Hurricane Maria

text: on September 3, while the southern portion moved into the

text: Caribbean Sea

text: . On September 4, the northern portion of the wave began to interact with an upper-level

text: low pressure system

text: and an elongated

text: trough

text: that was located between

text: Bermuda

text: and the Leeward Islands—the same trough which contributed to the development of

text: Hurricane Ophelia

text: . As a result of the low wind shear, convection redeveloped and organized along the wave axis.

text: Convective banding

text: formed around a broad

text: surface low

text: . It is estimated that the system developed into a tropical depression at 1800

text: UTC

text: on September 5. At the time it was located approximately  to the south-southwest of Bermuda.

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answers: NDQ_006452

answers: The wave split into two pieces

answers: NDQ_006453

answers: surface low

answers: NDQ_006455

answers: convection

answers: NDQ_006456

answers: east-west

answers: NDQ_006457

answers: surface low

answers: NDQ_006458

answers: It is estimated that the system developed into a tropical depression

answers: NDQ_006459

answers: convection

answers: NDQ_006460

answers: The wave split into two pieces

answers: NDQ_006461

answers: low wind shear

answer: No

answer: Yes

answer: Yes

answer: No

answer: No

answer: 1

text: While the storm was moving east across the Gulf of Mexico, Gabrielle produced rip currents along the coast of Alabama, killing one man in Orange Beach. High surf along the Florida Panhandle destroyed a retaining wall in Pensacola Beach. In the Florida Keys, there was an indirect drowning death of a man who fell off his boat; this was due to a combination of high seas, engine failure, and intoxication. Upon making landfall, Gabrielle produced moderate winds along coastal areas of western Florida, with sustained winds of  at Venice. The same station reported a wind gust of . High tides from rough waves and the storm surge reached , the highest tide since 1926. The tide flooded the northern shoreline of Charlotte Harbor and at the entrance to the Peace River, while further to the south a surge of greater than  inundated the barrier island at Fort Myers Beach and flooded some cars. Beach erosion was common in the areas where the storm surge was greatest.

text: While the storm was moving east across the Gulf of Mexico, Gabrielle produced

text: rip current

text: s along the coast of Alabama, killing one man in

text: Orange Beach

text: . High surf along the

text: Florida Panhandle

text: destroyed a retaining wall in

text: Pensacola Beach

text: . In the Florida Keys, there was an indirect drowning death of a man who fell off his boat; this was due to a combination of high seas, engine failure, and intoxication. Upon making landfall, Gabrielle produced moderate winds along coastal areas of western Florida, with sustained winds of  at Venice. The same station reported a wind gust of . High tides from rough waves and the

text: storm surge

text: reached , the highest tide since 1926. The tide flooded the northern shoreline of

text: Charlotte Harbor

text: and at the entrance to the

text: Peace River

text: , while further to the south a surge of greater than  inundated the

text: barrier island

text: at

text: Fort Myers Beach

text: and flooded some cars. Beach erosion was common in the areas where the storm surge was greatest.

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answers: NDQ_006452

answers: High tides

answers: NDQ_006453

answers: storm surge

answers: NDQ_006455

answers: high seas

answers: NDQ_006456

answers: currents

answers: NDQ_006457

answers: High surf

answers: NDQ_006458

answers: Beach erosion

answers: NDQ_006459

answers: high seas

answers: NDQ_006460

answers: High tide

answers: NDQ_006461

answers: High tides

answer: No

answer: No

answer: Yes

answer: No

answer: No

answer: 1

text: A very long, fast, tubing right hand point break breaks along the west side of the bay. The break is regarded as one of the best right hand point breaks in the entire world, in both consistency and quality, in season. It has been divided up into several sections, including, from the top of the point, Kitchen Windows, Magna tubes, Boneyards, Supertubes, Impossibles, Tubes, the Point, and Albatross. "Supertubes", which itself breaks for about 300m or more, is regarded as the best part of the wave. On rare occasions (large wave sizes, wide-breaking waves, and even swells), Boneyards can link up all the way to the Point for a ride over one kilometre long. Optimal size is considered to be from about 4 to 10 feet (Hawaiian scale), or about 8 to 20 feet wave faces. The most consistent waves occur between about May to mid September, also often coinciding with offshore winds, although good waves can occasionally occur at other times of the year.

text: A very long, fast, tubing right hand point break breaks along the west side of the bay. The break is regarded as one of the best right hand point breaks in the entire world, in both consistency and quality, in season. It has been divided up into several sections, including, from the top of the point, Kitchen Windows, Magna tubes, Boneyards, Supertubes, Impossibles, Tubes, the Point, and Albatross. "Supertubes", which itself breaks for about 300m or more, is regarded as the best part of the wave. On rare occasions (large wave sizes, wide-breaking waves, and even swells), Boneyards can link up all the way to the Point for a ride over one kilometre long. Optimal size is considered to be from about 4 to 10 feet (Hawaiian scale), or about 8 to 20 feet wave faces. The most consistent waves occur between about May to mid September, also often coinciding with offshore winds, although good waves can occasionally occur at other times of the year.

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answers: Optimal size

answers: NDQ_006453

answers: offshore winds

answers: NDQ_006455

answers: offshore winds

answers: NDQ_006456

answers: fast

answers: NDQ_006457

answers: Optimal size

answers: NDQ_006458

answers: Boneyards

answers: NDQ_006459

answers: offshore winds

answers: NDQ_006460

answers: Point

answers: NDQ_006461

answers: It has been divided up into several sections

answer: Yes

answer: Yes

answer: No

answer: Yes

answer: No

answer: 1

text: Individual waves in deep water break when the wave steepness—the ratio of the wave height H to the wavelength λ—exceeds about 0.07, so for H > 0.07 λ. In shallow water, with the water depth small compared to the wavelength, the individual waves break when their wave height H is larger than 0.8 times the water depth h, that is H > 0.8 h. Waves can also break if the wind grows strong enough to blow the crest off the base of the wave.

text: Individual waves in deep water break when the wave steepness—the

text: ratio

text: of the

text: wave height

text: H to the

text: wavelength

text: λ—exceeds about 0.07, so for H > 0.07 λ. In shallow water, with the water depth small compared to the wavelength, the individual waves break when their wave height H is larger than 0.8 times the water depth h, that is H > 0.8 h. Waves can also break if the wind grows strong enough to blow the crest off the base of the wave.

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answers: Waves can also break

answers: NDQ_006461

answers: the water depth small compared to the wavelength

answer: Yes

answer: Yes

answer: No

answer: Yes

answer: No

answer: 1

text: Local wind conditions affect wave quality, since the surface of a wave can become choppy in blustery conditions. Ideal conditions include a light to moderate "offshore" wind, because it blows into the front of the wave, making it a "barrel" or "tube" wave. Waves are Left handed and Right Handed depending upon the breaking formation of the wave.

text: Local wind conditions affect wave quality, since the surface of a wave can become choppy in blustery conditions. Ideal conditions include a light to moderate "offshore" wind, because it blows into the front of the wave, making it a

text: "barrel"

text: or "tube" wave. Waves are Left handed and Right Handed depending upon the breaking formation of the wave.

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answers: Breaking formation of the wave

answers: NDQ_006453

answers: choppy

answers: NDQ_006455

answers: wind

answers: NDQ_006456

answers: offshore

answers: NDQ_006457

answers: surface of a wave can become choppy in blustery conditions

answers: NDQ_006458

answers: "offshore" wind

answers: NDQ_006459

answers: offshore" wind

answers: NDQ_006460

answers: Shoreline

answers: NDQ_006461

answers: wind

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: Yes

answer: 1

text: The break is regarded as one of the best right-hand point breaks in the entire world, in both consistency and quality, in season. It has been divided up into several sections, including, from the top of the point, Kitchen Windows, Magna tubes, Boneyards, Supertubes, Impossibles, Tubes, the Point, and Albatross. "Supertubes", which itself breaks for about 300m or more, is regarded as the best part of the wave. On rare occasions (large wave sizes, wide-breaking waves, and even swells), Boneyards can link up all the way to the Point for a ride over one kilometer long. The most consistent waves occur between about May to mid September, also often coinciding with offshore winds, although good waves can occasionally occur at other times of the year.

text: The break is regarded as one of the best right-hand point breaks in the entire world, in both consistency and quality, in season. It has been divided up into several sections, including, from the top of the point, Kitchen Windows, Magna tubes, Boneyards, Supertubes, Impossibles, Tubes, the Point, and Albatross. "Supertubes", which itself breaks for about 300m or more, is regarded as the best part of the wave. On rare occasions (large wave sizes, wide-breaking waves, and even swells), Boneyards can link up all the way to the Point for a ride over one kilometer long. The most consistent waves occur between about May to mid September, also often coinciding with offshore winds, although good waves can occasionally occur at other times of the year.

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answers: Boneyards

answers: NDQ_006453

answers: offshore winds

answers: NDQ_006455

answers: offshore winds

answers: NDQ_006456

answers: slow

answers: NDQ_006457

answers: Boneyards

answers: NDQ_006458

answers: Boneyards

answers: NDQ_006459

answers: offshore winds

answers: NDQ_006460

answers: point

answers: NDQ_006461

answers: offshore winds

answer: Yes

answer: Yes

answer: No

answer: Yes

answer: No

answer: 1

text: Isaac's large wind field contributed to a strong storm surge peaking at  at a buoy offshore of Shell Beach. The strong waves inundated large areas of the state's coastal regions, particularly in Plaquemines Parish. The hurricane also brought heavy rainfall, leading to severe inland flooding. Rainfall amounts peaked statewide at  in Hammond. Including adjacent states, the storm surge and inland flooding alone caused $407 million in insured losses. Isaac's strong winds caused infrastructural and crop damage, in addition to storm surge and heavy rains. A WeatherBug weather station in Poydras reported a 97 mph (156 km/h) wind gust, the fastest measured in association with the storm. The strong winds also caused a widespread power outage, with 901,000 electricity customers losing power. In the aftermath of the hurricane, the Federal Emergency Management Agency (FEMA) granted $204.8 million in public assistance funds and $129.3 million in individual assistance funding.

text: Isaac's large wind field contributed to a strong

text: storm surge

text: peaking at  at a

text: buoy

text: offshore of Shell Beach. The strong waves inundated large areas of the state's coastal regions, particularly in

text: Plaquemines Parish

text: . The hurricane also brought heavy rainfall, leading to severe inland

text: flooding

text: . Rainfall amounts peaked statewide at  in

text: Hammond

text: . Including adjacent states, the storm surge and inland flooding alone caused $407 million in insured losses. Isaac's strong winds caused infrastructural and crop damage, in addition to storm surge and heavy rains. A

text: WeatherBug

text: weather station in

text: Poydras

text: reported a 97 mph (156 km/h) wind gust, the fastest measured in association with the storm. The strong winds also caused a widespread

text: power outage

text: , with 901,000 electricity customers losing power. In the aftermath of the hurricane, the

text: Federal Emergency Management Agency

text: (FEMA) granted $204.8 million in public assistance funds and $129.3 million in individual assistance funding.

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answers: NDQ_006460

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answers: NDQ_006461

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answers: NDQ_006452

answers: strong storm surge

answers: NDQ_006453

answers: storm surge

answers: NDQ_006455

answers: strong storm surge

answers: NDQ_006456

answers: slowed

answers: NDQ_006457

answers: The strong waves inundated large areas

answers: NDQ_006458

answers: strong storm surge

answers: NDQ_006459

answers: wind

answers: NDQ_006460

answers: storm surge

answers: NDQ_006461

answers: buoy

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: 1

text: Ripples appear on smooth water when the wind blows, but will die quickly if the wind stops. The restoring force that allows them to propagate is surface tension. Sea waves are larger-scale, often irregular motions that form under sustained winds. These waves tend to last much longer, even after the wind has died, and the restoring force that allows them to propagate is gravity. As waves propagate away from their area of origin, they naturally separate into groups of common direction and wavelength. The sets of waves formed in this way are known as swells.

text: Ripples appear on smooth water when the wind blows, but will die quickly if the wind stops. The restoring force that allows them to propagate is

text: surface tension

text: . Sea waves are larger-scale, often irregular motions that form under sustained winds. These waves tend to last much longer, even after the wind has died, and the restoring force that allows them to propagate is gravity. As waves propagate away from their area of origin, they naturally separate into groups of common direction and wavelength. The sets of waves formed in this way are known as swells.

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answers: NDQ_006452

answers: Gravity

answers: NDQ_006453

answers: swells

answers: NDQ_006455

answers: the wind blows

answers: NDQ_006456

answers: irregular motions

answers: NDQ_006457

answers: surface tension

answers: NDQ_006458

answers: surface tension

answers: NDQ_006459

answers: sustained winds

answers: NDQ_006460

answers: As waves propagate away from their area of origin

answers: NDQ_006461

answers: surface tension

answer: No

answer: No

answer: Yes

answer: No

answer: Yes

answer: 1

text: The Green Weenie was a green plastic rattle in the shape of a hot dog, which when waved at opposing players, purportedly put a jinx on them. Conversely, when waved at Pirate players it allegedly bestowed good luck.

text: The Green Weenie was a green plastic rattle in the shape of a

text: hot dog

text: , which when waved at opposing players, purportedly put a

text: jinx

text: on them. Conversely, when waved at Pirate players it allegedly bestowed good luck.

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