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    Baroclinic Instability in a Fluid with Three Layers

    Source: Journal of the Atmospheric Sciences:;1977:;Volume( 034 ):;issue: 008::page 1224
    Author:
    Davey, M. K.
    DOI: 10.1175/1520-0469(1977)034<1224:BIIAFW>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A three-layer model is used to study the effect of curvature in the vertical profile of the horizontal velocity on the linear baroclinic instability of a simple quasi-geostrophic flow. Potential vorticity is conserved and the ?-effect is included. The results indicate that the range of unstable wavelengths increases as the curvature is increased from zero. For a given physical state, there may be more than one critical wavelength for which the waves are marginally stable. Growth rates for ? = 0 and the structure of the fastest growing waves are given. A comparison is made between two-layer, three-layer and continuous systems.
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      Baroclinic Instability in a Fluid with Three Layers

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4153216
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    contributor authorDavey, M. K.
    date accessioned2017-06-09T14:19:39Z
    date available2017-06-09T14:19:39Z
    date copyright1977/08/01
    date issued1977
    identifier issn0022-4928
    identifier otherams-17333.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4153216
    description abstractA three-layer model is used to study the effect of curvature in the vertical profile of the horizontal velocity on the linear baroclinic instability of a simple quasi-geostrophic flow. Potential vorticity is conserved and the ?-effect is included. The results indicate that the range of unstable wavelengths increases as the curvature is increased from zero. For a given physical state, there may be more than one critical wavelength for which the waves are marginally stable. Growth rates for ? = 0 and the structure of the fastest growing waves are given. A comparison is made between two-layer, three-layer and continuous systems.
    publisherAmerican Meteorological Society
    titleBaroclinic Instability in a Fluid with Three Layers
    typeJournal Paper
    journal volume34
    journal issue8
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1977)034<1224:BIIAFW>2.0.CO;2
    journal fristpage1224
    journal lastpage1234
    treeJournal of the Atmospheric Sciences:;1977:;Volume( 034 ):;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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