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    Observations of the Response of Sea Waves to Veering Winds

    Source: Journal of Physical Oceanography:;1990:;Volume( 020 ):;issue: 012::page 1876
    Author:
    Masson, Diane
    DOI: 10.1175/1520-0485(1990)020<1876:OOTROS>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A data-adaptive technique, the iterative maximum likelihood method, is used to estimate directional wave spectra from data collected by three pitch-and-roll buoys, during two turning wind events of the CASP 86 experiment. A relaxation coefficient is estimated for the response of both the mean wave direction for each frequency band and the main wave direction of the wind sea spectrum to a change in wind direction. The values of the coefficients are found to be consistent with each other, and within the scatter of previous estimates. Also, a definite correlation is established between the wave rms angular spread and the rate of change of wind direction. Finally, the shapes of the estimated directional distributions are tested for symmetry and unimodality. A significant proportion of the estimated distributions are found to be neither unimodal nor symmetric.
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      Observations of the Response of Sea Waves to Veering Winds

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    contributor authorMasson, Diane
    date accessioned2017-06-09T14:49:49Z
    date available2017-06-09T14:49:49Z
    date copyright1990/12/01
    date issued1990
    identifier issn0022-3670
    identifier otherams-27712.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4164748
    description abstractA data-adaptive technique, the iterative maximum likelihood method, is used to estimate directional wave spectra from data collected by three pitch-and-roll buoys, during two turning wind events of the CASP 86 experiment. A relaxation coefficient is estimated for the response of both the mean wave direction for each frequency band and the main wave direction of the wind sea spectrum to a change in wind direction. The values of the coefficients are found to be consistent with each other, and within the scatter of previous estimates. Also, a definite correlation is established between the wave rms angular spread and the rate of change of wind direction. Finally, the shapes of the estimated directional distributions are tested for symmetry and unimodality. A significant proportion of the estimated distributions are found to be neither unimodal nor symmetric.
    publisherAmerican Meteorological Society
    titleObservations of the Response of Sea Waves to Veering Winds
    typeJournal Paper
    journal volume20
    journal issue12
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1990)020<1876:OOTROS>2.0.CO;2
    journal fristpage1876
    journal lastpage1885
    treeJournal of Physical Oceanography:;1990:;Volume( 020 ):;issue: 012
    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
    yabeshDSpacePersian