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dc.contributor.authorKudryavtsev, Vladimireng
dc.contributor.authorJohannessen, Johnny A.eng
dc.date.accessioned2006-01-11T11:38:36Z
dc.date.available2006-01-11T11:38:36Z
dc.date.issued2004-10eng
dc.PublishedGeophysical Research Letters 31(20): L20310en
dc.identifier.issn0094-8276en_US
dc.identifier.urihttps://hdl.handle.net/1956/865
dc.description.abstractThe paper presents an attempt to estimate short wave generation by wave breaking. A breaking wave crest disturbs the surface and generates sub-surface turbulence. The locally disturbed area further disperses and feeds short wave energy to the surroundings. The total short wave energy results from summing up the effect of wave breaking events randomly distributed over the sea surface. The rate of short wave generation is determined by the frequency of wavebreaking events per unit area. The source of short wave energy is isotropic, thus it generates waves at cross and opposite wind directions. The model qualitatively reproduces observed directional property of short wind wave spectra and mean square slope.en_US
dc.format.extent125073 byteseng
dc.format.mimetypeapplication/pdfeng
dc.language.isoengeng
dc.publisherAmerican Geophysical Unionen_US
dc.subjectOceanographyeng
dc.titleOn effect of wave breaking on short wind wavesen_US
dc.typePeer reviewed
dc.typeJournal article
dc.description.versionpublishedVersionen_US
dc.rights.holderCopyright 2004 by the American Geophysical Unionen_US
dc.identifier.doihttps://doi.org/10.1029/2004gl020619
dc.source.journalGeophysical Research Letters
dc.source.4031
dc.source.1420


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