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    A Dynamic Roughness Equation and Its Application to Wind Stress Determination at the Air-Sea Interface

    Source: Journal of Physical Oceanography:;1974:;Volume( 004 ):;issue: 001::page 116
    Author:
    Hsu, S. A.
    DOI: 10.1175/1520-0485(1974)004<0116:ADREAI>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A dynamic roughness equation including major wind and wave interaction parameters (wind shear velocity, wave height, and phase velocity) is derived. Because this equation implicitly incorporates the effects of wave steepness, relative water depth, and wind duration and fetch, it may be applied to a wide variety of natural conditions. This equation was used to construct a nomogram which can be utilized to determine the wind stress at the sea surface, given phase velocities, wave heights, and the wind speed at any height in the atmospheric boundary layer. The proposed relationships are verified by the available field and laboratory data under near-neutral atmospheric stability conditions from which the appropriate parameters could be determined.
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      A Dynamic Roughness Equation and Its Application to Wind Stress Determination at the Air-Sea Interface

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4162197
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    contributor authorHsu, S. A.
    date accessioned2017-06-09T14:43:49Z
    date available2017-06-09T14:43:49Z
    date copyright1974/01/01
    date issued1974
    identifier issn0022-3670
    identifier otherams-25416.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4162197
    description abstractA dynamic roughness equation including major wind and wave interaction parameters (wind shear velocity, wave height, and phase velocity) is derived. Because this equation implicitly incorporates the effects of wave steepness, relative water depth, and wind duration and fetch, it may be applied to a wide variety of natural conditions. This equation was used to construct a nomogram which can be utilized to determine the wind stress at the sea surface, given phase velocities, wave heights, and the wind speed at any height in the atmospheric boundary layer. The proposed relationships are verified by the available field and laboratory data under near-neutral atmospheric stability conditions from which the appropriate parameters could be determined.
    publisherAmerican Meteorological Society
    titleA Dynamic Roughness Equation and Its Application to Wind Stress Determination at the Air-Sea Interface
    typeJournal Paper
    journal volume4
    journal issue1
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1974)004<0116:ADREAI>2.0.CO;2
    journal fristpage116
    journal lastpage120
    treeJournal of Physical Oceanography:;1974:;Volume( 004 ):;issue: 001
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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