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    The Influence of Topography on the Stability of Jets

    Source: Journal of Physical Oceanography:;2005:;Volume( 035 ):;issue: 005::page 811
    Author:
    Poulin, F. J.
    ,
    Flierl, G. R.
    DOI: 10.1175/JPO2719.1
    Publisher: American Meteorological Society
    Abstract: In this article, the effect shelflike topography has on the stability of a jet that flows along the smooth shelf is addressed. The linear stability problem is solved to determine for which nondimensional parameters a shelf can either destabilize or stabilize a jet. These calculations reveal an intricate dependence of growth rate on topography. In particular, the authors determine that retrograde topography (with the shallow water on the left) always stabilizes the jet (in relation to the flat-bottom equivalent), whereas prograde topography (with the shallow water on the right) can either stabilize or destabilize the jet depending on the particular values of the Rossby number and topographic parameters. For Rossby numbers of order 1 and larger, prograde topography is strictly stabilizing. For small Rossby numbers, small-amplitude topography destabilizes whereas large topography stabilizes. The nonlinear evolution of these instabilities is explored to confirm the predictions from the linear theory and, also, to illustrate how stabilization is directly related to fluid transport across the shelf.
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      The Influence of Topography on the Stability of Jets

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4225728
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    contributor authorPoulin, F. J.
    contributor authorFlierl, G. R.
    date accessioned2017-06-09T17:17:44Z
    date available2017-06-09T17:17:44Z
    date copyright2005/05/01
    date issued2005
    identifier issn0022-3670
    identifier otherams-82597.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4225728
    description abstractIn this article, the effect shelflike topography has on the stability of a jet that flows along the smooth shelf is addressed. The linear stability problem is solved to determine for which nondimensional parameters a shelf can either destabilize or stabilize a jet. These calculations reveal an intricate dependence of growth rate on topography. In particular, the authors determine that retrograde topography (with the shallow water on the left) always stabilizes the jet (in relation to the flat-bottom equivalent), whereas prograde topography (with the shallow water on the right) can either stabilize or destabilize the jet depending on the particular values of the Rossby number and topographic parameters. For Rossby numbers of order 1 and larger, prograde topography is strictly stabilizing. For small Rossby numbers, small-amplitude topography destabilizes whereas large topography stabilizes. The nonlinear evolution of these instabilities is explored to confirm the predictions from the linear theory and, also, to illustrate how stabilization is directly related to fluid transport across the shelf.
    publisherAmerican Meteorological Society
    titleThe Influence of Topography on the Stability of Jets
    typeJournal Paper
    journal volume35
    journal issue5
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/JPO2719.1
    journal fristpage811
    journal lastpage825
    treeJournal of Physical Oceanography:;2005:;Volume( 035 ):;issue: 005
    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