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    Effects of Water Waves on Wind Shear Stress for Current Modeling

    Source: Journal of Atmospheric and Oceanic Technology:;1992:;volume( 009 ):;issue: 006::page 850
    Author:
    Johnson, H. K.
    ,
    Vested, H. J.
    DOI: 10.1175/1520-0426(1992)009<0850:EOWWOW>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: With the goal of improving the formulation of the wind shear stress used in numerical current modeling, a new method for including the effect of water waves on sea roughness is presented. The method is a hybrid of earlier sea roughness models by Kitaigorodskii and Volkov and Donelan, with two distinctions: 1) the roughness height is assumed to be proportional to a wave height representing high-frequency waves (k>1.5kp) in the spectrum, and 2) the hybrid model is calibrated to give drag coefficients obtained by Smith and Banke for their site conditions and verified by comparisons with other independent datasets. In deep water, this model gives a sea roughness that increases with wave age (Cp/U*) in the early stages of wave growth (up to Cp/U*=5), after which the sea roughness decreases with wave age. This method yields wave-modified Cd values for several test cases and can be used directly in numerical current models.
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      Effects of Water Waves on Wind Shear Stress for Current Modeling

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4220177
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    contributor authorJohnson, H. K.
    contributor authorVested, H. J.
    date accessioned2017-06-09T16:59:44Z
    date available2017-06-09T16:59:44Z
    date copyright1992/12/01
    date issued1992
    identifier issn0739-0572
    identifier otherams-776.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4220177
    description abstractWith the goal of improving the formulation of the wind shear stress used in numerical current modeling, a new method for including the effect of water waves on sea roughness is presented. The method is a hybrid of earlier sea roughness models by Kitaigorodskii and Volkov and Donelan, with two distinctions: 1) the roughness height is assumed to be proportional to a wave height representing high-frequency waves (k>1.5kp) in the spectrum, and 2) the hybrid model is calibrated to give drag coefficients obtained by Smith and Banke for their site conditions and verified by comparisons with other independent datasets. In deep water, this model gives a sea roughness that increases with wave age (Cp/U*) in the early stages of wave growth (up to Cp/U*=5), after which the sea roughness decreases with wave age. This method yields wave-modified Cd values for several test cases and can be used directly in numerical current models.
    publisherAmerican Meteorological Society
    titleEffects of Water Waves on Wind Shear Stress for Current Modeling
    typeJournal Paper
    journal volume9
    journal issue6
    journal titleJournal of Atmospheric and Oceanic Technology
    identifier doi10.1175/1520-0426(1992)009<0850:EOWWOW>2.0.CO;2
    journal fristpage850
    journal lastpage861
    treeJournal of Atmospheric and Oceanic Technology:;1992:;volume( 009 ):;issue: 006
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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