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    Analysis of Surface Current Response to Wind

    Source: Journal of Physical Oceanography:;1979:;Volume( 009 ):;issue: 002::page 401
    Author:
    Kirwan, A. D.
    ,
    McNally, G.
    ,
    Pazan, S.
    ,
    Wert, R.
    DOI: 10.1175/1520-0485(1979)009<0401:AOSCRT>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The response of the surface current to the wind has been described at various times by quadratic and linear laws. The quadratic response leads to Ekman-type currents while the linear response may be indicative of Stokes drift. The velocity records of six satellite-tracked drifters which lost their drogues and the Fleet Numerical Weather Central's surface wind analysis were used to test the relative merits of these responses. It was concluded that a linear law relating the wind and the wind drift surface current was superior to the classic quadratic law. The angle between the wind and the surface current predicted by the model was about 15° cum sole. However, it was also found that a model which superposed the Ekman quadratic response and linear Stokes drift response explained the data just as well as the linear law.
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      Analysis of Surface Current Response to Wind

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4162751
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    contributor authorKirwan, A. D.
    contributor authorMcNally, G.
    contributor authorPazan, S.
    contributor authorWert, R.
    date accessioned2017-06-09T14:45:02Z
    date available2017-06-09T14:45:02Z
    date copyright1979/03/01
    date issued1979
    identifier issn0022-3670
    identifier otherams-25915.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4162751
    description abstractThe response of the surface current to the wind has been described at various times by quadratic and linear laws. The quadratic response leads to Ekman-type currents while the linear response may be indicative of Stokes drift. The velocity records of six satellite-tracked drifters which lost their drogues and the Fleet Numerical Weather Central's surface wind analysis were used to test the relative merits of these responses. It was concluded that a linear law relating the wind and the wind drift surface current was superior to the classic quadratic law. The angle between the wind and the surface current predicted by the model was about 15° cum sole. However, it was also found that a model which superposed the Ekman quadratic response and linear Stokes drift response explained the data just as well as the linear law.
    publisherAmerican Meteorological Society
    titleAnalysis of Surface Current Response to Wind
    typeJournal Paper
    journal volume9
    journal issue2
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1979)009<0401:AOSCRT>2.0.CO;2
    journal fristpage401
    journal lastpage412
    treeJournal of Physical Oceanography:;1979:;Volume( 009 ):;issue: 002
    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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