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    Incorporation of Stratification Effects on the Oceanic Roughness Length in the Derivation of the Neutral Drag Coefficient

    Source: Journal of Physical Oceanography:;1986:;Volume( 016 ):;issue: 009::page 1580
    Author:
    Geernaert, Gerald
    ,
    Katsaros, Kristina B.
    DOI: 10.1175/1520-0485(1986)016<1580:IOSEOT>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Based on the assumption that, over the sea, the roughness length of the wind profile scales with the wind stress, a new formulation that describes the drag coefficient as a function of the given neutral drag coefficient and stability is derived. The new formulation is compared to an earlier formulation where roughness changes with stability were ignored. The two are then illustrated with data collected from both the Marine Remote Sensing Project (1979) and the Tower Ocean Wave and Radar Dependence Experiment (1984). It was found that when the surface roughness was allowed to depend on wind stress (and therefore stability), the stratification correction to the neutral drag coefficient was larger than for the case when the roughness length was not allowed to vary.
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      Incorporation of Stratification Effects on the Oceanic Roughness Length in the Derivation of the Neutral Drag Coefficient

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4164026
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    contributor authorGeernaert, Gerald
    contributor authorKatsaros, Kristina B.
    date accessioned2017-06-09T14:48:02Z
    date available2017-06-09T14:48:02Z
    date copyright1986/09/01
    date issued1986
    identifier issn0022-3670
    identifier otherams-27062.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4164026
    description abstractBased on the assumption that, over the sea, the roughness length of the wind profile scales with the wind stress, a new formulation that describes the drag coefficient as a function of the given neutral drag coefficient and stability is derived. The new formulation is compared to an earlier formulation where roughness changes with stability were ignored. The two are then illustrated with data collected from both the Marine Remote Sensing Project (1979) and the Tower Ocean Wave and Radar Dependence Experiment (1984). It was found that when the surface roughness was allowed to depend on wind stress (and therefore stability), the stratification correction to the neutral drag coefficient was larger than for the case when the roughness length was not allowed to vary.
    publisherAmerican Meteorological Society
    titleIncorporation of Stratification Effects on the Oceanic Roughness Length in the Derivation of the Neutral Drag Coefficient
    typeJournal Paper
    journal volume16
    journal issue9
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1986)016<1580:IOSEOT>2.0.CO;2
    journal fristpage1580
    journal lastpage1584
    treeJournal of Physical Oceanography:;1986:;Volume( 016 ):;issue: 009
    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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