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    The Three-Dimensional Current and Surface Wave Equations

    Source: Journal of Physical Oceanography:;2003:;Volume( 033 ):;issue: 009::page 1978
    Author:
    Mellor, George
    DOI: 10.1175/1520-0485(2003)033<1978:TTCASW>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Surface wave equations appropriate to three-dimensional ocean models apparently have not been presented in the literature. It is the intent of this paper to correct that deficiency. Thus, expressions for vertically dependent radiation stresses and a definition of the Doppler velocity for a vertically dependent current field are obtained. Other quantities such as vertically dependent surface pressure forcing are derived for inclusion in the momentum and wave energy equations. The equations include terms that represent the production of turbulence energy by currents and waves. These results are a necessary precursor for three-dimensional ocean models that handle surface waves together with wind- and buoyancy-driven currents. Although the third dimension has been added here, the analysis is based on the assumption that the depth dependence of wave motions is provided by linear theory, an assumption that is the basis of much of the wave literature.
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      The Three-Dimensional Current and Surface Wave Equations

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    contributor authorMellor, George
    date accessioned2017-06-09T14:55:56Z
    date available2017-06-09T14:55:56Z
    date copyright2003/09/01
    date issued2003
    identifier issn0022-3670
    identifier otherams-29922.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4167203
    description abstractSurface wave equations appropriate to three-dimensional ocean models apparently have not been presented in the literature. It is the intent of this paper to correct that deficiency. Thus, expressions for vertically dependent radiation stresses and a definition of the Doppler velocity for a vertically dependent current field are obtained. Other quantities such as vertically dependent surface pressure forcing are derived for inclusion in the momentum and wave energy equations. The equations include terms that represent the production of turbulence energy by currents and waves. These results are a necessary precursor for three-dimensional ocean models that handle surface waves together with wind- and buoyancy-driven currents. Although the third dimension has been added here, the analysis is based on the assumption that the depth dependence of wave motions is provided by linear theory, an assumption that is the basis of much of the wave literature.
    publisherAmerican Meteorological Society
    titleThe Three-Dimensional Current and Surface Wave Equations
    typeJournal Paper
    journal volume33
    journal issue9
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(2003)033<1978:TTCASW>2.0.CO;2
    journal fristpage1978
    journal lastpage1989
    treeJournal of Physical Oceanography:;2003:;Volume( 033 ):;issue: 009
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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