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    Barotropic Instability and Rossby Wave Radiation

    Source: Journal of the Atmospheric Sciences:;1985:;Volume( 042 ):;issue: 017::page 1825
    Author:
    Halevy, I.
    ,
    Peltier, W. R.
    DOI: 10.1175/1520-0469(1985)042<1825:BIARWR>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A detailed study of linear barotropic instability confirms that the concept of critical level overreflection is fundamental to the understanding of the entire family of unstable modes in this problem. This is in agreement with the general argument presented by Lindzen and Tung and applied by Lindzen et al.. However, our approach in the analysis is somewhat novel, and it may be seen as an extension of the exact method of calculation employed by Davis and Peltier in their work on stratified parallel flows. The practical numerical utility of the neutral stability boundaries as a basis for the determination of both the radiating unstable modes and the fundamental unstable modes is demonstrated. The actual neutral boundaries provide a much tighter restriction on the real phase speeds of the linear disturbances than the one provided by the usual semicircle theorem. Our presentation of complete stability curves for the entire family of unstable modes allows us to clarify the issue of mode coalescence that first appeared in the paper by Dickinson and Clare.
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      Barotropic Instability and Rossby Wave Radiation

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4155197
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    contributor authorHalevy, I.
    contributor authorPeltier, W. R.
    date accessioned2017-06-09T14:25:50Z
    date available2017-06-09T14:25:50Z
    date copyright1985/09/01
    date issued1985
    identifier issn0022-4928
    identifier otherams-19116.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4155197
    description abstractA detailed study of linear barotropic instability confirms that the concept of critical level overreflection is fundamental to the understanding of the entire family of unstable modes in this problem. This is in agreement with the general argument presented by Lindzen and Tung and applied by Lindzen et al.. However, our approach in the analysis is somewhat novel, and it may be seen as an extension of the exact method of calculation employed by Davis and Peltier in their work on stratified parallel flows. The practical numerical utility of the neutral stability boundaries as a basis for the determination of both the radiating unstable modes and the fundamental unstable modes is demonstrated. The actual neutral boundaries provide a much tighter restriction on the real phase speeds of the linear disturbances than the one provided by the usual semicircle theorem. Our presentation of complete stability curves for the entire family of unstable modes allows us to clarify the issue of mode coalescence that first appeared in the paper by Dickinson and Clare.
    publisherAmerican Meteorological Society
    titleBarotropic Instability and Rossby Wave Radiation
    typeJournal Paper
    journal volume42
    journal issue17
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1985)042<1825:BIARWR>2.0.CO;2
    journal fristpage1825
    journal lastpage1837
    treeJournal of the Atmospheric Sciences:;1985:;Volume( 042 ):;issue: 017
    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