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    Observations of Wind-Generated Waves on Variable Current

    Source: Journal of Physical Oceanography:;1976:;Volume( 006 ):;issue: 006::page 962
    Author:
    Long, Steven R.
    ,
    Huang, Norden E.
    DOI: 10.1175/1520-0485(1976)006<0962:OOWGWO>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Laboratory measurements utilizing a laser probe are made for the slopes of wind waves generated on both positive and negative currents at different values of fetch. The data are then processed electronically to yield an average wave-slope spectrum in frequency space with 128 degrees of freedom. These spectra are used to obtain the growth of the spectral components at various frequency bands for increasing wind and different values of fetch and current. The results indicate that the growth of these components is not monotonic with the frictional wind speed U*, but rather exhibits an ?overshoot? phenomena at lower values of U*, and in addition, displays a significant effect due to current. The peak location and spectral intensity of the spectra also show strong influence by the current condition. This results in the rms surface slope value increasing with negative current and decreasing with positive current. The results agree qualitatively with some theoretical predictions. The potential use of the current-induced effects as a means for remote sensing of ocean current is also briefly discussed.
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      Observations of Wind-Generated Waves on Variable Current

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4162465
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    contributor authorLong, Steven R.
    contributor authorHuang, Norden E.
    date accessioned2017-06-09T14:44:24Z
    date available2017-06-09T14:44:24Z
    date copyright1976/11/01
    date issued1976
    identifier issn0022-3670
    identifier otherams-25658.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4162465
    description abstractLaboratory measurements utilizing a laser probe are made for the slopes of wind waves generated on both positive and negative currents at different values of fetch. The data are then processed electronically to yield an average wave-slope spectrum in frequency space with 128 degrees of freedom. These spectra are used to obtain the growth of the spectral components at various frequency bands for increasing wind and different values of fetch and current. The results indicate that the growth of these components is not monotonic with the frictional wind speed U*, but rather exhibits an ?overshoot? phenomena at lower values of U*, and in addition, displays a significant effect due to current. The peak location and spectral intensity of the spectra also show strong influence by the current condition. This results in the rms surface slope value increasing with negative current and decreasing with positive current. The results agree qualitatively with some theoretical predictions. The potential use of the current-induced effects as a means for remote sensing of ocean current is also briefly discussed.
    publisherAmerican Meteorological Society
    titleObservations of Wind-Generated Waves on Variable Current
    typeJournal Paper
    journal volume6
    journal issue6
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1976)006<0962:OOWGWO>2.0.CO;2
    journal fristpage962
    journal lastpage968
    treeJournal of Physical Oceanography:;1976:;Volume( 006 ):;issue: 006
    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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