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    A Numerical Simulation of Barotropic Instability. Part III: Wave–Wave Interaction in the Presence of Dissipation

    Source: Journal of the Atmospheric Sciences:;1986:;Volume( 043 ):;issue: 010::page 1045
    Author:
    Schoeberl, Mark R.
    ,
    Nielsen, J. Eric
    DOI: 10.1175/1520-0469(1986)043<1045:ANSOBI>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A fully nonlinear model of barotropic instability including dissipation is used to investigate the evolution of the integrated enstrophy and vorticity. The dissipation independent limits on the integrated enstrophy and the long period oscillation in the integrated enstrophy found by Schoeberl and Lindzen are verified. The enstrophy oscillations are similar to those previously noted for two-dimensional Kelvin-Helmholtz instabilities. They are produced by advection of the vorticity back and forth across the region of instability by the largest scale wave. A simple expression that accurately estimates the period of these oscillations is derived using the saturation theory.
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      A Numerical Simulation of Barotropic Instability. Part III: Wave–Wave Interaction in the Presence of Dissipation

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4155385
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    contributor authorSchoeberl, Mark R.
    contributor authorNielsen, J. Eric
    date accessioned2017-06-09T14:26:24Z
    date available2017-06-09T14:26:24Z
    date copyright1986/05/01
    date issued1986
    identifier issn0022-4928
    identifier otherams-19286.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4155385
    description abstractA fully nonlinear model of barotropic instability including dissipation is used to investigate the evolution of the integrated enstrophy and vorticity. The dissipation independent limits on the integrated enstrophy and the long period oscillation in the integrated enstrophy found by Schoeberl and Lindzen are verified. The enstrophy oscillations are similar to those previously noted for two-dimensional Kelvin-Helmholtz instabilities. They are produced by advection of the vorticity back and forth across the region of instability by the largest scale wave. A simple expression that accurately estimates the period of these oscillations is derived using the saturation theory.
    publisherAmerican Meteorological Society
    titleA Numerical Simulation of Barotropic Instability. Part III: Wave–Wave Interaction in the Presence of Dissipation
    typeJournal Paper
    journal volume43
    journal issue10
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1986)043<1045:ANSOBI>2.0.CO;2
    journal fristpage1045
    journal lastpage1050
    treeJournal of the Atmospheric Sciences:;1986:;Volume( 043 ):;issue: 010
    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