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    The Goddard Coastal Wave Model. Part II: Kinematics

    Source: Journal of Physical Oceanography:;1996:;Volume( 026 ):;issue: 006::page 848
    Author:
    Lin, Ray Q.
    ,
    Huang, Norden E.
    DOI: 10.1175/1520-0485(1996)026<0848:TGCWMP>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A new coastal wave model is being developed to study air?sea interaction processes in the coastal region. The kinematics of this model, which govern the wave propagation, are reported. This new model is based on the action conservation equation rather than on the energy transport equation; it also employs the full nonlinear dispersion relationship in water of arbitrary depth. With these improvements, it includes nonstationary wave-current interaction processes and functions in coastal regions with variable finite water depths. Numerical results show that these changes cause significant differences between the new model and the WAM model when waves encounter any steady or unsteady current, and when waves propagate over changing bottom topography in a shallow water region. Such conditions are very common and should not be neglected in the coastal regions.
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      The Goddard Coastal Wave Model. Part II: Kinematics

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4165644
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    contributor authorLin, Ray Q.
    contributor authorHuang, Norden E.
    date accessioned2017-06-09T14:52:04Z
    date available2017-06-09T14:52:04Z
    date copyright1996/06/01
    date issued1996
    identifier issn0022-3670
    identifier otherams-28519.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4165644
    description abstractA new coastal wave model is being developed to study air?sea interaction processes in the coastal region. The kinematics of this model, which govern the wave propagation, are reported. This new model is based on the action conservation equation rather than on the energy transport equation; it also employs the full nonlinear dispersion relationship in water of arbitrary depth. With these improvements, it includes nonstationary wave-current interaction processes and functions in coastal regions with variable finite water depths. Numerical results show that these changes cause significant differences between the new model and the WAM model when waves encounter any steady or unsteady current, and when waves propagate over changing bottom topography in a shallow water region. Such conditions are very common and should not be neglected in the coastal regions.
    publisherAmerican Meteorological Society
    titleThe Goddard Coastal Wave Model. Part II: Kinematics
    typeJournal Paper
    journal volume26
    journal issue6
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1996)026<0848:TGCWMP>2.0.CO;2
    journal fristpage848
    journal lastpage862
    treeJournal of Physical Oceanography:;1996:;Volume( 026 ):;issue: 006
    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
    yabeshDSpacePersian