AustralieFrV1, PascalFrancis, Curation, bibRecord, 005245

On the variability of sea drag in finite water depth : Surface Waves and Wave-Coupled Effects in Lower Atmosphere and Upper Ocean

Identifieur interne : 005245 ( PascalFrancis/Curation ); précédent : 005244; suivant : 005246

On the variability of sea drag in finite water depth : Surface Waves and Wave-Coupled Effects in Lower Atmosphere and Upper Ocean

Auteurs : A. Toffoli [Australie] ; L. Loffredo [Belgique] ; P. Le Roy [Australie, France] ; J.-M. Lefevre [France] ; A. V. Babanin [Australie]

Source :

Journal of geophysical research [ 0148-0227 ] ; 2012.

RBID : Pascal:13-0084645

Descripteurs français

Pascal (Inist)
- Traînée, Couplage, Couche limite atmosphérique, Surface marine, Modèle, Coefficient traînée, Vitesse vent, Paramétrisation, Onde atmosphérique, Lac, Interface air mer, Vapeur eau, Densité, Vitesse frottement, Vague vent, Humidité relative, Analyse statistique, Rugosité, Australie.
Wicri :
- geographic : Australie.
- topic : Lac.

English descriptors

KwdEn :
- Atmospheric boundary layer, Atmospheric wave, Australia, Drag, Drag coefficient, Friction velocity, Relative humidity, Sea surface, Wind velocity, Wind wave, air-sea interface, coupling, density, lakes, models, parametrization, roughness, statistical analysis, water vapor.

Abstract

[1] The coupling between the atmospheric boundary layer and the ocean surface in large-scale models is usually parameterized in terms of the sea drag coefficient, which is routinely estimated as a function of mean wind speed. The scatter of data around such parametric dependencies, however, is very significant and imposes a serious limitation on the forecasts and predictions that make use of sea surface drag parameterizations. The analysis of an atmospheric and wave data set collected in finite water depth at the Lake George measurement site (Australia) suggests that this variability relates to a number of parameters at the air-sea interface other than wind speed alone. In particular, results indicate that the sea drag depends on water depth and wave steepness, which make the wave profile more vertically asymmetric, and the concentration of water vapor in the air, which modifies air density and friction velocity. These dependencies are used to derive parametric functions based on the combined contribution of wind, waves and relative humidity. A standard statistical analysis confirms a substantial improvement in the prediction of the drag coefficient and sea surface roughness when additional parameters are taken into account.

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A03		`1`		`@0 J. geophys. res.`
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A08	`01`	`1`	`ENG`	`@1 On the variability of sea drag in finite water depth : Surface Waves and Wave-Coupled Effects in Lower Atmosphere and Upper Ocean`
A11	`01`	`1`		`@1 TOFFOLI (A.)`
A11	`02`	`1`		`@1 LOFFREDO (L.)`
A11	`03`	`1`		`@1 LE ROY (P.)`
A11	`04`	`1`		`@1 LEFEVRE (J.-M.)`
A11	`05`	`1`		`@1 BABANIN (A. V.)`
A14	`01`			`@1 Faculty of Engineering and Industrial Sciences, Swinburne University of Technology @2 Hawthorn, Victoria @3 AUS @Z 1 aut. @Z 3 aut. @Z 5 aut.`
A14	`02`			`@1 Hydraulics Laboratory, Katholieke Universiteit Leuven @2 Heverlee @3 BEL @Z 2 aut.`
A14	`03`			`@1 Meteo France @2 Toulouse @3 FRA @Z 3 aut. @Z 4 aut.`
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A44				`@0 0000 @1 © 2013 INIST-CNRS. All rights reserved.`
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C01	`01`		`ENG`	@0 [1] The coupling between the atmospheric boundary layer and the ocean surface in large-scale models is usually parameterized in terms of the sea drag coefficient, which is routinely estimated as a function of mean wind speed. The scatter of data around such parametric dependencies, however, is very significant and imposes a serious limitation on the forecasts and predictions that make use of sea surface drag parameterizations. The analysis of an atmospheric and wave data set collected in finite water depth at the Lake George measurement site (Australia) suggests that this variability relates to a number of parameters at the air-sea interface other than wind speed alone. In particular, results indicate that the sea drag depends on water depth and wave steepness, which make the wave profile more vertically asymmetric, and the concentration of water vapor in the air, which modifies air density and friction velocity. These dependencies are used to derive parametric functions based on the combined contribution of wind, waves and relative humidity. A standard statistical analysis confirms a substantial improvement in the prediction of the drag coefficient and sea surface roughness when additional parameters are taken into account.
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C03	`03`	`X`	`SPA`	`@0 Capa límite atmosférico @5 03`
C03	`04`	`X`	`FRE`	`@0 Surface marine @5 04`
C03	`04`	`X`	`ENG`	`@0 Sea surface @5 04`
C03	`04`	`X`	`SPA`	`@0 Superficie marina @5 04`
C03	`05`	`2`	`FRE`	`@0 Modèle @5 05`
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C03	`05`	`2`	`SPA`	`@0 Modelo @5 05`
C03	`06`	`X`	`FRE`	`@0 Coefficient traînée @5 06`
C03	`06`	`X`	`ENG`	`@0 Drag coefficient @5 06`
C03	`06`	`X`	`SPA`	`@0 Coeficiente resistencia aerodinámica @5 06`
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C03	`07`	`X`	`SPA`	`@0 Velocidad viento @5 07`
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C03	`09`	`X`	`FRE`	`@0 Onde atmosphérique @5 09`
C03	`09`	`X`	`ENG`	`@0 Atmospheric wave @5 09`
C03	`09`	`X`	`SPA`	`@0 Onda atmosférica @5 09`
C03	`10`	`2`	`FRE`	`@0 Lac @5 10`
C03	`10`	`2`	`ENG`	`@0 lakes @5 10`
C03	`10`	`2`	`SPA`	`@0 Lago @5 10`
C03	`11`	`2`	`FRE`	`@0 Interface air mer @5 11`
C03	`11`	`2`	`ENG`	`@0 air-sea interface @5 11`
C03	`11`	`2`	`SPA`	`@0 Interfase aire mar @5 11`
C03	`12`	`2`	`FRE`	`@0 Vapeur eau @5 12`
C03	`12`	`2`	`ENG`	`@0 water vapor @5 12`
C03	`12`	`2`	`SPA`	`@0 Vapor agua @5 12`
C03	`13`	`2`	`FRE`	`@0 Densité @5 13`
C03	`13`	`2`	`ENG`	`@0 density @5 13`
C03	`13`	`2`	`SPA`	`@0 Densidad @5 13`
C03	`14`	`X`	`FRE`	`@0 Vitesse frottement @5 14`
C03	`14`	`X`	`ENG`	`@0 Friction velocity @5 14`
C03	`14`	`X`	`SPA`	`@0 Velocidad rozamiento @5 14`
C03	`15`	`X`	`FRE`	`@0 Vague vent @5 15`
C03	`15`	`X`	`ENG`	`@0 Wind wave @5 15`
C03	`15`	`X`	`SPA`	`@0 Ola viento @5 15`
C03	`16`	`X`	`FRE`	`@0 Humidité relative @5 16`
C03	`16`	`X`	`ENG`	`@0 Relative humidity @5 16`
C03	`16`	`X`	`SPA`	`@0 Humedad relativa @5 16`
C03	`17`	`2`	`FRE`	`@0 Analyse statistique @5 17`
C03	`17`	`2`	`ENG`	`@0 statistical analysis @5 17`
C03	`18`	`2`	`FRE`	`@0 Rugosité @5 18`
C03	`18`	`2`	`ENG`	`@0 roughness @5 18`
C03	`18`	`2`	`SPA`	`@0 Rugosidad @5 18`
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C03	`19`	`2`	`ENG`	`@0 Australia @2 NG @5 21`
C03	`19`	`2`	`SPA`	`@0 Australia @2 NG @5 21`
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Le document en format XML

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<front><div type="abstract" xml:lang="en">[1] The coupling between the atmospheric boundary layer and the ocean surface in large-scale models is usually parameterized in terms of the sea drag coefficient, which is routinely estimated as a function of mean wind speed. The scatter of data around such parametric dependencies, however, is very significant and imposes a serious limitation on the forecasts and predictions that make use of sea surface drag parameterizations. The analysis of an atmospheric and wave data set collected in finite water depth at the Lake George measurement site (Australia) suggests that this variability relates to a number of parameters at the air-sea interface other than wind speed alone. In particular, results indicate that the sea drag depends on water depth and wave steepness, which make the wave profile more vertically asymmetric, and the concentration of water vapor in the air, which modifies air density and friction velocity. These dependencies are used to derive parametric functions based on the combined contribution of wind, waves and relative humidity. A standard statistical analysis confirms a substantial improvement in the prediction of the drag coefficient and sea surface roughness when additional parameters are taken into account.</div>
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<fC03 i1="03" i2="X" l="ENG"><s0>Atmospheric boundary layer</s0>
<s5>03</s5>
</fC03>
<fC03 i1="03" i2="X" l="SPA"><s0>Capa límite atmosférico</s0>
<s5>03</s5>
</fC03>
<fC03 i1="04" i2="X" l="FRE"><s0>Surface marine</s0>
<s5>04</s5>
</fC03>
<fC03 i1="04" i2="X" l="ENG"><s0>Sea surface</s0>
<s5>04</s5>
</fC03>
<fC03 i1="04" i2="X" l="SPA"><s0>Superficie marina</s0>
<s5>04</s5>
</fC03>
<fC03 i1="05" i2="2" l="FRE"><s0>Modèle</s0>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="2" l="ENG"><s0>models</s0>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="2" l="SPA"><s0>Modelo</s0>
<s5>05</s5>
</fC03>
<fC03 i1="06" i2="X" l="FRE"><s0>Coefficient traînée</s0>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="X" l="ENG"><s0>Drag coefficient</s0>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="X" l="SPA"><s0>Coeficiente resistencia aerodinámica</s0>
<s5>06</s5>
</fC03>
<fC03 i1="07" i2="X" l="FRE"><s0>Vitesse vent</s0>
<s5>07</s5>
</fC03>
<fC03 i1="07" i2="X" l="ENG"><s0>Wind velocity</s0>
<s5>07</s5>
</fC03>
<fC03 i1="07" i2="X" l="SPA"><s0>Velocidad viento</s0>
<s5>07</s5>
</fC03>
<fC03 i1="08" i2="2" l="FRE"><s0>Paramétrisation</s0>
<s5>08</s5>
</fC03>
<fC03 i1="08" i2="2" l="ENG"><s0>parametrization</s0>
<s5>08</s5>
</fC03>
<fC03 i1="09" i2="X" l="FRE"><s0>Onde atmosphérique</s0>
<s5>09</s5>
</fC03>
<fC03 i1="09" i2="X" l="ENG"><s0>Atmospheric wave</s0>
<s5>09</s5>
</fC03>
<fC03 i1="09" i2="X" l="SPA"><s0>Onda atmosférica</s0>
<s5>09</s5>
</fC03>
<fC03 i1="10" i2="2" l="FRE"><s0>Lac</s0>
<s5>10</s5>
</fC03>
<fC03 i1="10" i2="2" l="ENG"><s0>lakes</s0>
<s5>10</s5>
</fC03>
<fC03 i1="10" i2="2" l="SPA"><s0>Lago</s0>
<s5>10</s5>
</fC03>
<fC03 i1="11" i2="2" l="FRE"><s0>Interface air mer</s0>
<s5>11</s5>
</fC03>
<fC03 i1="11" i2="2" l="ENG"><s0>air-sea interface</s0>
<s5>11</s5>
</fC03>
<fC03 i1="11" i2="2" l="SPA"><s0>Interfase aire mar</s0>
<s5>11</s5>
</fC03>
<fC03 i1="12" i2="2" l="FRE"><s0>Vapeur eau</s0>
<s5>12</s5>
</fC03>
<fC03 i1="12" i2="2" l="ENG"><s0>water vapor</s0>
<s5>12</s5>
</fC03>
<fC03 i1="12" i2="2" l="SPA"><s0>Vapor agua</s0>
<s5>12</s5>
</fC03>
<fC03 i1="13" i2="2" l="FRE"><s0>Densité</s0>
<s5>13</s5>
</fC03>
<fC03 i1="13" i2="2" l="ENG"><s0>density</s0>
<s5>13</s5>
</fC03>
<fC03 i1="13" i2="2" l="SPA"><s0>Densidad</s0>
<s5>13</s5>
</fC03>
<fC03 i1="14" i2="X" l="FRE"><s0>Vitesse frottement</s0>
<s5>14</s5>
</fC03>
<fC03 i1="14" i2="X" l="ENG"><s0>Friction velocity</s0>
<s5>14</s5>
</fC03>
<fC03 i1="14" i2="X" l="SPA"><s0>Velocidad rozamiento</s0>
<s5>14</s5>
</fC03>
<fC03 i1="15" i2="X" l="FRE"><s0>Vague vent</s0>
<s5>15</s5>
</fC03>
<fC03 i1="15" i2="X" l="ENG"><s0>Wind wave</s0>
<s5>15</s5>
</fC03>
<fC03 i1="15" i2="X" l="SPA"><s0>Ola viento</s0>
<s5>15</s5>
</fC03>
<fC03 i1="16" i2="X" l="FRE"><s0>Humidité relative</s0>
<s5>16</s5>
</fC03>
<fC03 i1="16" i2="X" l="ENG"><s0>Relative humidity</s0>
<s5>16</s5>
</fC03>
<fC03 i1="16" i2="X" l="SPA"><s0>Humedad relativa</s0>
<s5>16</s5>
</fC03>
<fC03 i1="17" i2="2" l="FRE"><s0>Analyse statistique</s0>
<s5>17</s5>
</fC03>
<fC03 i1="17" i2="2" l="ENG"><s0>statistical analysis</s0>
<s5>17</s5>
</fC03>
<fC03 i1="18" i2="2" l="FRE"><s0>Rugosité</s0>
<s5>18</s5>
</fC03>
<fC03 i1="18" i2="2" l="ENG"><s0>roughness</s0>
<s5>18</s5>
</fC03>
<fC03 i1="18" i2="2" l="SPA"><s0>Rugosidad</s0>
<s5>18</s5>
</fC03>
<fC03 i1="19" i2="2" l="FRE"><s0>Australie</s0>
<s2>NG</s2>
<s5>21</s5>
</fC03>
<fC03 i1="19" i2="2" l="ENG"><s0>Australia</s0>
<s2>NG</s2>
<s5>21</s5>
</fC03>
<fC03 i1="19" i2="2" l="SPA"><s0>Australia</s0>
<s2>NG</s2>
<s5>21</s5>
</fC03>
<fC07 i1="01" i2="2" l="FRE"><s0>Australasie</s0>
</fC07>
<fC07 i1="01" i2="2" l="ENG"><s0>Australasia</s0>
</fC07>
<fC07 i1="01" i2="2" l="SPA"><s0>Australasia</s0>
</fC07>
<fN21><s1>056</s1>
</fN21>
<fN44 i1="01"><s1>OTO</s1>
</fN44>
<fN82><s1>OTO</s1>
</fN82>
</pA>
</standard>
</inist>
</record>

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   |texte=   On the variability of sea drag in finite water depth : Surface Waves and Wave-Coupled Effects in Lower Atmosphere and Upper Ocean
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Data generation: Tue Dec 5 10:43:12 2017. Site generation: Tue Mar 5 14:07:20 2024

	Serveur d'exploration sur les relations entre la France et l'Australie
	Attention, ce site est en cours de développement ! Attention, site généré par des moyens informatiques à partir de corpus bruts. Les informations ne sont donc pas validées.

Serveur d'exploration sur les relations entre la France et l'Australie

On the variability of sea drag in finite water depth : Surface Waves and Wave-Coupled Effects in Lower Atmosphere and Upper Ocean

On the variability of sea drag in finite water depth : Surface Waves and Wave-Coupled Effects in Lower Atmosphere and Upper Ocean

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