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    The Stability of a Stationary Rossby Wave in a Baroclinic Zonal Flow

    Source: Journal of the Atmospheric Sciences:;1978:;Volume( 035 ):;issue: 008::page 1388
    Author:
    Merkine, Lee-Or
    ,
    Israeli, Moshe
    DOI: 10.1175/1520-0469(1978)035<1388:TSOASR>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The stability of a stationary baroclinic Rossby wave embedded in a baroclinic zonal flow is investigated in the framework of the two-layer model. This investigation is relevant to the question of mountain-induced cyclogenesis, where such flow configurations may exist on the lee side of the topography. It is found that when the amplitude of the stationary Rossby wave is sufficiently large a flow which is stable upstream may become unstable downstream. The influence of the baroclinic shear is to reduce the growth rate of the instability in comparison to the corresponding barotropic case. Nonetheless the growth rates obtained can he significantly larger than those obtained for a baroclinic parallel zonal flow, possessing the same baroclinicity.
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      The Stability of a Stationary Rossby Wave in a Baroclinic Zonal Flow

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4153428
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    contributor authorMerkine, Lee-Or
    contributor authorIsraeli, Moshe
    date accessioned2017-06-09T14:20:16Z
    date available2017-06-09T14:20:16Z
    date copyright1978/08/01
    date issued1978
    identifier issn0022-4928
    identifier otherams-17524.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4153428
    description abstractThe stability of a stationary baroclinic Rossby wave embedded in a baroclinic zonal flow is investigated in the framework of the two-layer model. This investigation is relevant to the question of mountain-induced cyclogenesis, where such flow configurations may exist on the lee side of the topography. It is found that when the amplitude of the stationary Rossby wave is sufficiently large a flow which is stable upstream may become unstable downstream. The influence of the baroclinic shear is to reduce the growth rate of the instability in comparison to the corresponding barotropic case. Nonetheless the growth rates obtained can he significantly larger than those obtained for a baroclinic parallel zonal flow, possessing the same baroclinicity.
    publisherAmerican Meteorological Society
    titleThe Stability of a Stationary Rossby Wave in a Baroclinic Zonal Flow
    typeJournal Paper
    journal volume35
    journal issue8
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1978)035<1388:TSOASR>2.0.CO;2
    journal fristpage1388
    journal lastpage1394
    treeJournal of the Atmospheric Sciences:;1978:;Volume( 035 ):;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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