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    Baroclinic Instability of a Rotating Hadley Cell

    Source: Journal of the Atmospheric Sciences:;1981:;Volume( 038 ):;issue: 010::page 2130
    Author:
    Antar, Basil N.
    ,
    Fowlis, William W.
    DOI: 10.1175/1520-0469(1981)038<2130:BIOARH>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The stability of a thin fluid layer between two rotating plates which are subjected to a horizontal temperature gradient is studied. First, the solution for the stationary basic state is obtained in a closed form. This solution identifies Ekman and thermal layers adjacent to the plates and interior temperature and velocity fields which are almost linear functions of height. Then the stability of that basic state with respect to infinitesimal zonal waves is analyzed via the solution of the complete viscous linear equations for the perturbations. The character of the growth rates is found to be similar to the growth rates of the classical baroclinic waves. The neutral stability curves for these waves possessed a knee in the Rossby-Taylor number plane to the left of which all perturbations are stable. The region of instability is found to depend on the Prandtl number, the vertical stratification parameter, and both the meridional and zonal wavenumbers. It is found in general that the flow is unstable for small enough Ekman numbers and for Rossby numbers less than 10. It is also found that increased vertical stable stratification and increased Prandtl number stabilize the flow.
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      Baroclinic Instability of a Rotating Hadley Cell

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4154191
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    • Journal of the Atmospheric Sciences

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    contributor authorAntar, Basil N.
    contributor authorFowlis, William W.
    date accessioned2017-06-09T14:22:34Z
    date available2017-06-09T14:22:34Z
    date copyright1981/10/01
    date issued1981
    identifier issn0022-4928
    identifier otherams-18210.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4154191
    description abstractThe stability of a thin fluid layer between two rotating plates which are subjected to a horizontal temperature gradient is studied. First, the solution for the stationary basic state is obtained in a closed form. This solution identifies Ekman and thermal layers adjacent to the plates and interior temperature and velocity fields which are almost linear functions of height. Then the stability of that basic state with respect to infinitesimal zonal waves is analyzed via the solution of the complete viscous linear equations for the perturbations. The character of the growth rates is found to be similar to the growth rates of the classical baroclinic waves. The neutral stability curves for these waves possessed a knee in the Rossby-Taylor number plane to the left of which all perturbations are stable. The region of instability is found to depend on the Prandtl number, the vertical stratification parameter, and both the meridional and zonal wavenumbers. It is found in general that the flow is unstable for small enough Ekman numbers and for Rossby numbers less than 10. It is also found that increased vertical stable stratification and increased Prandtl number stabilize the flow.
    publisherAmerican Meteorological Society
    titleBaroclinic Instability of a Rotating Hadley Cell
    typeJournal Paper
    journal volume38
    journal issue10
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1981)038<2130:BIOARH>2.0.CO;2
    journal fristpage2130
    journal lastpage2141
    treeJournal of the Atmospheric Sciences:;1981:;Volume( 038 ):;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
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