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    Finite-Amplitude Long Waves on Coastal Currents

    Source: Journal of Physical Oceanography:;1990:;Volume( 020 ):;issue: 001::page 3
    Author:
    Grimshaw, R.
    ,
    Zengxin, Yi
    DOI: 10.1175/1520-0485(1990)020<0003:FALWOC>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Two models of coastal currents are described that allow fully nonlinear wavelike solutions for the limit of long waves. The first model is an adaptation of a model used by Yi and Warn for finite-amplitude ?plane Rossby waves in a channel. It utilizes a particular choice of continental shelf topography to obtain a nonlinear evolution equation for long waves of finite amplitude. The second model describes the waves that form at the vorticity interface between two regions of constant potential vorticity. Again a nonlinear evolution equation is obtained for long waves of finite amplitude. For both model equations, numerical results are presented and compared with the corresponding results for the BDA equation, which is the weakly nonlinear limit for both models.
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      Finite-Amplitude Long Waves on Coastal Currents

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    contributor authorGrimshaw, R.
    contributor authorZengxin, Yi
    date accessioned2017-06-09T14:49:27Z
    date available2017-06-09T14:49:27Z
    date copyright1990/01/01
    date issued1990
    identifier issn0022-3670
    identifier otherams-27588.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4164609
    description abstractTwo models of coastal currents are described that allow fully nonlinear wavelike solutions for the limit of long waves. The first model is an adaptation of a model used by Yi and Warn for finite-amplitude ?plane Rossby waves in a channel. It utilizes a particular choice of continental shelf topography to obtain a nonlinear evolution equation for long waves of finite amplitude. The second model describes the waves that form at the vorticity interface between two regions of constant potential vorticity. Again a nonlinear evolution equation is obtained for long waves of finite amplitude. For both model equations, numerical results are presented and compared with the corresponding results for the BDA equation, which is the weakly nonlinear limit for both models.
    publisherAmerican Meteorological Society
    titleFinite-Amplitude Long Waves on Coastal Currents
    typeJournal Paper
    journal volume20
    journal issue1
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1990)020<0003:FALWOC>2.0.CO;2
    journal fristpage3
    journal lastpage18
    treeJournal of Physical Oceanography:;1990:;Volume( 020 ):;issue: 001
    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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