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    Vortex Generation Through Balanced Adjustment

    Source: Journal of Physical Oceanography:;1988:;Volume( 018 ):;issue: 008::page 1178
    Author:
    McWilliams, James C.
    DOI: 10.1175/1520-0485(1988)018<1178:VGTBA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The problem of geostrophic adjustment, originally considered by C.G. Rossby, is solved in an axisymmetric geometry for a continuously stratified fluid, where the adjusted final state is in hydrostatic, gradient-wind balance. This problem is relevant to the generation of submesoscale coherent vortices in the ocean: diapycnal mixing events can create a local anomaly of less strongly stratified fluid, which then develops a balancing circulation through adjustment. An analytical solution is obtained for a few uniform-density layers, and this is compared with numerical solutions for continuous stratification. In both representations, two-dimensional solutions are compared with axisymmetric ones.
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      Vortex Generation Through Balanced Adjustment

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4164397
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    contributor authorMcWilliams, James C.
    date accessioned2017-06-09T14:48:57Z
    date available2017-06-09T14:48:57Z
    date copyright1988/08/01
    date issued1988
    identifier issn0022-3670
    identifier otherams-27397.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4164397
    description abstractThe problem of geostrophic adjustment, originally considered by C.G. Rossby, is solved in an axisymmetric geometry for a continuously stratified fluid, where the adjusted final state is in hydrostatic, gradient-wind balance. This problem is relevant to the generation of submesoscale coherent vortices in the ocean: diapycnal mixing events can create a local anomaly of less strongly stratified fluid, which then develops a balancing circulation through adjustment. An analytical solution is obtained for a few uniform-density layers, and this is compared with numerical solutions for continuous stratification. In both representations, two-dimensional solutions are compared with axisymmetric ones.
    publisherAmerican Meteorological Society
    titleVortex Generation Through Balanced Adjustment
    typeJournal Paper
    journal volume18
    journal issue8
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1988)018<1178:VGTBA>2.0.CO;2
    journal fristpage1178
    journal lastpage1192
    treeJournal of Physical Oceanography:;1988:;Volume( 018 ):;issue: 008
    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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