Growth and dissipation of wind-forced, deep-water waves
Identifieur interne : 004F17 ( Main/Exploration ); précédent : 004F16; suivant : 004F18Growth and dissipation of wind-forced, deep-water waves
Auteurs : Laurent Grare [France] ; William L. Peirson [Australie] ; Hubert Branger [France] ; James W. Walker [Australie] ; Jean-Paul Giovanangeli [France] ; Vladimir Makin [Pays-Bas]Source :
- Journal of Fluid Mechanics [ 0022-1120 ] ; 2013.
Descripteurs français
- Pascal (Inist)
English descriptors
Abstract
The input of energy by wind to water waves is compared with the observed growth of the waves using a suite of microphysical measurement techniques in the laboratory. These include measured tangential stresses in the water and air immediately adjacent to the interface with corresponding form drag measurements above wind-forced freely propagating waves. The drag data sets are consistent but the comparison has highlighted important issues in relation to the measurement of fluctuating pressures above freely propagating waves. Derived normalized wind input values show good collapse as a function of mean wave steepness and are significantly in excess of the assembly of net wave growth measurements by Peirson & Garcia (J. Fluid Mech., vol. 608, 2008, pp. 243-274) at low steepness. Sheltering coefficients in the form of Jeffreys (Proc. R. Soc. Lond. Ser. A, vol. 107, 1925, pp. 189-206) are derived that are consistent with values previously obtained by Donelan & Pierson (J. Geophys. Res., vol. 92, 1987, pp. 4971-5029), Donelan (Wind-over-Wave Couplings: Perspectives and Prospects, Clarendon, 1999, pp. 183-194) and Donelan et al. (J. Phys. Oceanogr., vol. 36, 2006, pp. 1672-1689). The sheltering coefficients exhibit substantial scatter. By carefully measuring the associated growth of the surface wave fields, systematic energy budgets for the interaction between wind and waves are obtained. For non-breaking waves, there is a significant and systematic misclose in the radiative transfer equation if wave-turbulence interactions are not included. Significantly higher levels of turbulent wave attenuation are found in comparison with the theoretical estimates by Teixeira & Belcher (J. Fluid Mech., vol. 458, 2002, pp. 229-267) and Ardhuin & Jenkins (J. Phys. Oceanogr., vol. 36, 2006, pp. 551-557). Suitable normalizations of attenuation for wind-forced wave fields exhibit consistent behaviour in the presence and absence of wave breaking. Closure of the surface energy flux budget is obtained by comparing the normalized energy loss rates due to breaking with the values previously determined by Banner & Peirson (J. Fluid Mech., vol. 585, 2007, pp. 93-115) and Drazen et al.(J. Fluid Mech., vol. 611, 2008, pp. 307-332) when expressed as a function of mean wave steepness. Their normalized energy loss rates obtained for non-wind forced breaking wave groups are remarkably consistent with the levels found during this present study when breaking waves are subject to wind forcing.
Affiliations:
Links toward previous steps (curation, corpus...)
- to stream PascalFrancis, to step Corpus: 000A47
- to stream PascalFrancis, to step Curation: 005425
- to stream PascalFrancis, to step Checkpoint: 000917
- to stream Main, to step Merge: 005091
- to stream Main, to step Curation: 004F17
Le document en format XML
<record><TEI><teiHeader><fileDesc><titleStmt><title xml:lang="en" level="a">Growth and dissipation of wind-forced, deep-water waves</title><author><name sortKey="Grare, Laurent" sort="Grare, Laurent" uniqKey="Grare L" first="Laurent" last="Grare">Laurent Grare</name><affiliation wicri:level="4"><inist:fA14 i1="01"><s1>Institut de Recherche sur les Phenomenes Hors Equilibre, CNRS UMR 6594, Aix-Marseille Universite</s1><s3>FRA</s3><sZ>1 aut.</sZ><sZ>3 aut.</sZ><sZ>5 aut.</sZ></inist:fA14><country>France</country><wicri:noRegion>Aix-Marseille Universite</wicri:noRegion><placeName><settlement type="city">Marseille</settlement><region type="region" nuts="2">Provence-Alpes-Côte d'Azur</region></placeName><orgName type="university">Université d'Aix-Marseille</orgName></affiliation></author><author><name sortKey="Peirson, William L" sort="Peirson, William L" uniqKey="Peirson W" first="William L." last="Peirson">William L. Peirson</name><affiliation wicri:level="1"><inist:fA14 i1="02"><s1>Water Research Laboratory, School of Civil and Environmental Engineering, University of New South Wales, King Street</s1><s2>Manly Vale NSW 2093</s2><s3>AUS</s3><sZ>2 aut.</sZ><sZ>4 aut.</sZ></inist:fA14><country>Australie</country><wicri:noRegion>Manly Vale NSW 2093</wicri:noRegion></affiliation></author><author><name sortKey="Branger, Hubert" sort="Branger, Hubert" uniqKey="Branger H" first="Hubert" last="Branger">Hubert Branger</name><affiliation wicri:level="4"><inist:fA14 i1="01"><s1>Institut de Recherche sur les Phenomenes Hors Equilibre, CNRS UMR 6594, Aix-Marseille Universite</s1><s3>FRA</s3><sZ>1 aut.</sZ><sZ>3 aut.</sZ><sZ>5 aut.</sZ></inist:fA14><country>France</country><wicri:noRegion>Aix-Marseille Universite</wicri:noRegion><placeName><settlement type="city">Marseille</settlement><region type="region" nuts="2">Provence-Alpes-Côte d'Azur</region></placeName><orgName type="university">Université d'Aix-Marseille</orgName></affiliation></author><author><name sortKey="Walker, James W" sort="Walker, James W" uniqKey="Walker J" first="James W." last="Walker">James W. Walker</name><affiliation wicri:level="1"><inist:fA14 i1="02"><s1>Water Research Laboratory, School of Civil and Environmental Engineering, University of New South Wales, King Street</s1><s2>Manly Vale NSW 2093</s2><s3>AUS</s3><sZ>2 aut.</sZ><sZ>4 aut.</sZ></inist:fA14><country>Australie</country><wicri:noRegion>Manly Vale NSW 2093</wicri:noRegion></affiliation></author><author><name sortKey="Giovanangeli, Jean Paul" sort="Giovanangeli, Jean Paul" uniqKey="Giovanangeli J" first="Jean-Paul" last="Giovanangeli">Jean-Paul Giovanangeli</name><affiliation wicri:level="4"><inist:fA14 i1="01"><s1>Institut de Recherche sur les Phenomenes Hors Equilibre, CNRS UMR 6594, Aix-Marseille Universite</s1><s3>FRA</s3><sZ>1 aut.</sZ><sZ>3 aut.</sZ><sZ>5 aut.</sZ></inist:fA14><country>France</country><wicri:noRegion>Aix-Marseille Universite</wicri:noRegion><placeName><settlement type="city">Marseille</settlement><region type="region" nuts="2">Provence-Alpes-Côte d'Azur</region></placeName><orgName type="university">Université d'Aix-Marseille</orgName></affiliation></author><author><name sortKey="Makin, Vladimir" sort="Makin, Vladimir" uniqKey="Makin V" first="Vladimir" last="Makin">Vladimir Makin</name><affiliation wicri:level="1"><inist:fA14 i1="03"><s1>KNMI, PO Box 201</s1><s2>3730 AE De Bilt</s2><s3>NLD</s3><sZ>6 aut.</sZ></inist:fA14><country>Pays-Bas</country><wicri:noRegion>3730 AE De Bilt</wicri:noRegion></affiliation></author></titleStmt><publicationStmt><idno type="wicri:source">INIST</idno><idno type="inist">13-0184420</idno><date when="2013">2013</date><idno type="stanalyst">PASCAL 13-0184420 INIST</idno><idno type="RBID">Pascal:13-0184420</idno><idno type="wicri:Area/PascalFrancis/Corpus">000A47</idno><idno type="wicri:Area/PascalFrancis/Curation">005425</idno><idno type="wicri:Area/PascalFrancis/Checkpoint">000917</idno><idno type="wicri:explorRef" wicri:stream="PascalFrancis" wicri:step="Checkpoint">000917</idno><idno type="wicri:doubleKey">0022-1120:2013:Grare L:growth:and:dissipation</idno><idno type="wicri:Area/Main/Merge">005091</idno><idno type="wicri:Area/Main/Curation">004F17</idno><idno type="wicri:Area/Main/Exploration">004F17</idno></publicationStmt><sourceDesc><biblStruct><analytic><title xml:lang="en" level="a">Growth and dissipation of wind-forced, deep-water waves</title><author><name sortKey="Grare, Laurent" sort="Grare, Laurent" uniqKey="Grare L" first="Laurent" last="Grare">Laurent Grare</name><affiliation wicri:level="4"><inist:fA14 i1="01"><s1>Institut de Recherche sur les Phenomenes Hors Equilibre, CNRS UMR 6594, Aix-Marseille Universite</s1><s3>FRA</s3><sZ>1 aut.</sZ><sZ>3 aut.</sZ><sZ>5 aut.</sZ></inist:fA14><country>France</country><wicri:noRegion>Aix-Marseille Universite</wicri:noRegion><placeName><settlement type="city">Marseille</settlement><region type="region" nuts="2">Provence-Alpes-Côte d'Azur</region></placeName><orgName type="university">Université d'Aix-Marseille</orgName></affiliation></author><author><name sortKey="Peirson, William L" sort="Peirson, William L" uniqKey="Peirson W" first="William L." last="Peirson">William L. Peirson</name><affiliation wicri:level="1"><inist:fA14 i1="02"><s1>Water Research Laboratory, School of Civil and Environmental Engineering, University of New South Wales, King Street</s1><s2>Manly Vale NSW 2093</s2><s3>AUS</s3><sZ>2 aut.</sZ><sZ>4 aut.</sZ></inist:fA14><country>Australie</country><wicri:noRegion>Manly Vale NSW 2093</wicri:noRegion></affiliation></author><author><name sortKey="Branger, Hubert" sort="Branger, Hubert" uniqKey="Branger H" first="Hubert" last="Branger">Hubert Branger</name><affiliation wicri:level="4"><inist:fA14 i1="01"><s1>Institut de Recherche sur les Phenomenes Hors Equilibre, CNRS UMR 6594, Aix-Marseille Universite</s1><s3>FRA</s3><sZ>1 aut.</sZ><sZ>3 aut.</sZ><sZ>5 aut.</sZ></inist:fA14><country>France</country><wicri:noRegion>Aix-Marseille Universite</wicri:noRegion><placeName><settlement type="city">Marseille</settlement><region type="region" nuts="2">Provence-Alpes-Côte d'Azur</region></placeName><orgName type="university">Université d'Aix-Marseille</orgName></affiliation></author><author><name sortKey="Walker, James W" sort="Walker, James W" uniqKey="Walker J" first="James W." last="Walker">James W. Walker</name><affiliation wicri:level="1"><inist:fA14 i1="02"><s1>Water Research Laboratory, School of Civil and Environmental Engineering, University of New South Wales, King Street</s1><s2>Manly Vale NSW 2093</s2><s3>AUS</s3><sZ>2 aut.</sZ><sZ>4 aut.</sZ></inist:fA14><country>Australie</country><wicri:noRegion>Manly Vale NSW 2093</wicri:noRegion></affiliation></author><author><name sortKey="Giovanangeli, Jean Paul" sort="Giovanangeli, Jean Paul" uniqKey="Giovanangeli J" first="Jean-Paul" last="Giovanangeli">Jean-Paul Giovanangeli</name><affiliation wicri:level="4"><inist:fA14 i1="01"><s1>Institut de Recherche sur les Phenomenes Hors Equilibre, CNRS UMR 6594, Aix-Marseille Universite</s1><s3>FRA</s3><sZ>1 aut.</sZ><sZ>3 aut.</sZ><sZ>5 aut.</sZ></inist:fA14><country>France</country><wicri:noRegion>Aix-Marseille Universite</wicri:noRegion><placeName><settlement type="city">Marseille</settlement><region type="region" nuts="2">Provence-Alpes-Côte d'Azur</region></placeName><orgName type="university">Université d'Aix-Marseille</orgName></affiliation></author><author><name sortKey="Makin, Vladimir" sort="Makin, Vladimir" uniqKey="Makin V" first="Vladimir" last="Makin">Vladimir Makin</name><affiliation wicri:level="1"><inist:fA14 i1="03"><s1>KNMI, PO Box 201</s1><s2>3730 AE De Bilt</s2><s3>NLD</s3><sZ>6 aut.</sZ></inist:fA14><country>Pays-Bas</country><wicri:noRegion>3730 AE De Bilt</wicri:noRegion></affiliation></author></analytic><series><title level="j" type="main">Journal of Fluid Mechanics</title><title level="j" type="abbreviated">J. Fluid Mech.</title><idno type="ISSN">0022-1120</idno><imprint><date when="2013">2013</date></imprint></series></biblStruct></sourceDesc><seriesStmt><title level="j" type="main">Journal of Fluid Mechanics</title><title level="j" type="abbreviated">J. Fluid Mech.</title><idno type="ISSN">0022-1120</idno></seriesStmt></fileDesc><profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Deep water</term><term>Surface gravity wave</term><term>Test facility</term><term>Wind wave</term><term>experimental studies</term></keywords><keywords scheme="Pascal" xml:lang="fr"><term>Vague vent</term><term>Onde surface gravité</term><term>Etude expérimentale</term><term>Installation essai</term><term>Eau profonde</term></keywords></textClass></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">The input of energy by wind to water waves is compared with the observed growth of the waves using a suite of microphysical measurement techniques in the laboratory. These include measured tangential stresses in the water and air immediately adjacent to the interface with corresponding form drag measurements above wind-forced freely propagating waves. The drag data sets are consistent but the comparison has highlighted important issues in relation to the measurement of fluctuating pressures above freely propagating waves. Derived normalized wind input values show good collapse as a function of mean wave steepness and are significantly in excess of the assembly of net wave growth measurements by Peirson & Garcia (J. Fluid Mech., vol. 608, 2008, pp. 243-274) at low steepness. Sheltering coefficients in the form of Jeffreys (Proc. R. Soc. Lond. Ser. A, vol. 107, 1925, pp. 189-206) are derived that are consistent with values previously obtained by Donelan & Pierson (J. Geophys. Res., vol. 92, 1987, pp. 4971-5029), Donelan (Wind-over-Wave Couplings: Perspectives and Prospects, Clarendon, 1999, pp. 183-194) and Donelan et al. (J. Phys. Oceanogr., vol. 36, 2006, pp. 1672-1689). The sheltering coefficients exhibit substantial scatter. By carefully measuring the associated growth of the surface wave fields, systematic energy budgets for the interaction between wind and waves are obtained. For non-breaking waves, there is a significant and systematic misclose in the radiative transfer equation if wave-turbulence interactions are not included. Significantly higher levels of turbulent wave attenuation are found in comparison with the theoretical estimates by Teixeira & Belcher (J. Fluid Mech., vol. 458, 2002, pp. 229-267) and Ardhuin & Jenkins (J. Phys. Oceanogr., vol. 36, 2006, pp. 551-557). Suitable normalizations of attenuation for wind-forced wave fields exhibit consistent behaviour in the presence and absence of wave breaking. Closure of the surface energy flux budget is obtained by comparing the normalized energy loss rates due to breaking with the values previously determined by Banner & Peirson (J. Fluid Mech., vol. 585, 2007, pp. 93-115) and Drazen et al.(J. Fluid Mech., vol. 611, 2008, pp. 307-332) when expressed as a function of mean wave steepness. Their normalized energy loss rates obtained for non-wind forced breaking wave groups are remarkably consistent with the levels found during this present study when breaking waves are subject to wind forcing.</div></front></TEI><affiliations><list><country><li>Australie</li><li>France</li><li>Pays-Bas</li></country><region><li>Provence-Alpes-Côte d'Azur</li></region><settlement><li>Marseille</li></settlement><orgName><li>Université d'Aix-Marseille</li></orgName></list><tree><country name="France"><region name="Provence-Alpes-Côte d'Azur"><name sortKey="Grare, Laurent" sort="Grare, Laurent" uniqKey="Grare L" first="Laurent" last="Grare">Laurent Grare</name></region><name sortKey="Branger, Hubert" sort="Branger, Hubert" uniqKey="Branger H" first="Hubert" last="Branger">Hubert Branger</name><name sortKey="Giovanangeli, Jean Paul" sort="Giovanangeli, Jean Paul" uniqKey="Giovanangeli J" first="Jean-Paul" last="Giovanangeli">Jean-Paul Giovanangeli</name></country><country name="Australie"><noRegion><name sortKey="Peirson, William L" sort="Peirson, William L" uniqKey="Peirson W" first="William L." last="Peirson">William L. Peirson</name></noRegion><name sortKey="Walker, James W" sort="Walker, James W" uniqKey="Walker J" first="James W." last="Walker">James W. Walker</name></country><country name="Pays-Bas"><noRegion><name sortKey="Makin, Vladimir" sort="Makin, Vladimir" uniqKey="Makin V" first="Vladimir" last="Makin">Vladimir Makin</name></noRegion></country></tree></affiliations></record>Pour manipuler ce document sous Unix (Dilib)
EXPLOR_STEP=$WICRI_ROOT/Wicri/Asie/explor/AustralieFrV1/Data/Main/Exploration
HfdSelect -h $EXPLOR_STEP/biblio.hfd -nk 004F17 | SxmlIndent | more
Ou
HfdSelect -h $EXPLOR_AREA/Data/Main/Exploration/biblio.hfd -nk 004F17 | SxmlIndent | more
Pour mettre un lien sur cette page dans le réseau Wicri
{{Explor lien
|wiki= Wicri/Asie
|area= AustralieFrV1
|flux= Main
|étape= Exploration
|type= RBID
|clé= Pascal:13-0184420
|texte= Growth and dissipation of wind-forced, deep-water waves
}}
| This area was generated with Dilib version V0.6.33. |  |