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    On the Linear Parameterization of Drag Coefficient over Sea Surface

    Source: Journal of Physical Oceanography:;2004:;Volume( 034 ):;issue: 012::page 2847
    Author:
    Guan, Changlong
    ,
    Xie, Lian
    DOI: 10.1175/JPO2664.1
    Publisher: American Meteorological Society
    Abstract: Combining the logarithmic law with the Charnock relation yields a drag coefficient that is a function of wind speed with the Charnock coefficient as a parameter. It is found that the function is nearly linear within the typically measured range of the drag coefficient. The slope of the linear function is dominated by the Charnock coefficient. When the Charnock relation is extended to a wave age?dependent function, the drag coefficient remains a near-linear function of wind speed after invoking the 3/2 power law. The slope of the linear function is dominated by wave steepness.
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      On the Linear Parameterization of Drag Coefficient over Sea Surface

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4225668
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    contributor authorGuan, Changlong
    contributor authorXie, Lian
    date accessioned2017-06-09T17:17:37Z
    date available2017-06-09T17:17:37Z
    date copyright2004/12/01
    date issued2004
    identifier issn0022-3670
    identifier otherams-82542.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4225668
    description abstractCombining the logarithmic law with the Charnock relation yields a drag coefficient that is a function of wind speed with the Charnock coefficient as a parameter. It is found that the function is nearly linear within the typically measured range of the drag coefficient. The slope of the linear function is dominated by the Charnock coefficient. When the Charnock relation is extended to a wave age?dependent function, the drag coefficient remains a near-linear function of wind speed after invoking the 3/2 power law. The slope of the linear function is dominated by wave steepness.
    publisherAmerican Meteorological Society
    titleOn the Linear Parameterization of Drag Coefficient over Sea Surface
    typeJournal Paper
    journal volume34
    journal issue12
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/JPO2664.1
    journal fristpage2847
    journal lastpage2851
    treeJournal of Physical Oceanography:;2004:;Volume( 034 ):;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
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