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    Refraction of Surface Gravity Waves by Shear Waves

    Source: Journal of Physical Oceanography:;2006:;Volume( 036 ):;issue: 004::page 629
    Author:
    Henderson, Stephen M.
    ,
    Guza, R. T.
    ,
    Elgar, Steve
    ,
    Herbers, T. H. C.
    DOI: 10.1175/JPO2890.1
    Publisher: American Meteorological Society
    Abstract: Previous field observations indicate that the directional spread of swell-frequency (nominally 0.1 Hz) surface gravity waves increases during shoreward propagation across the surf zone. This directional broadening contrasts with the narrowing observed seaward of the surf zone and predicted by Snell?s law for bathymetric refraction. Field-observed broadening was predicted by a new model for refraction of swell by lower-frequency (nominally 0.01 Hz) current and elevation fluctuations. The observations and the model suggest that refraction by the cross-shore currents of energetic shear waves contributed substantially to the observed broadening.
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      Refraction of Surface Gravity Waves by Shear Waves

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4225918
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    • Journal of Physical Oceanography

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    contributor authorHenderson, Stephen M.
    contributor authorGuza, R. T.
    contributor authorElgar, Steve
    contributor authorHerbers, T. H. C.
    date accessioned2017-06-09T17:18:11Z
    date available2017-06-09T17:18:11Z
    date copyright2006/04/01
    date issued2006
    identifier issn0022-3670
    identifier otherams-82768.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4225918
    description abstractPrevious field observations indicate that the directional spread of swell-frequency (nominally 0.1 Hz) surface gravity waves increases during shoreward propagation across the surf zone. This directional broadening contrasts with the narrowing observed seaward of the surf zone and predicted by Snell?s law for bathymetric refraction. Field-observed broadening was predicted by a new model for refraction of swell by lower-frequency (nominally 0.01 Hz) current and elevation fluctuations. The observations and the model suggest that refraction by the cross-shore currents of energetic shear waves contributed substantially to the observed broadening.
    publisherAmerican Meteorological Society
    titleRefraction of Surface Gravity Waves by Shear Waves
    typeJournal Paper
    journal volume36
    journal issue4
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/JPO2890.1
    journal fristpage629
    journal lastpage635
    treeJournal of Physical Oceanography:;2006:;Volume( 036 ):;issue: 004
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
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