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    Subsynoptic-Scale Baroclinic Instability

    Source: Journal of the Atmospheric Sciences:;1982:;Volume( 039 ):;issue: 005::page 1052
    Author:
    Satyamurthy, Prakki
    ,
    Rao, Vadlamudi Brahmananda
    ,
    Moura, Antonio Divino
    DOI: 10.1175/1520-0469(1982)039<1052:SSBI>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A linear stability analysis of the hyperbolic tangent profiles is made. A Boussinesq primitive equation model with high vertical resolution is used. Unstable modes of intermediate scales (Lx ≈ 1000 km) are generated when the curvature, d2?/dz2, of the basic flow in the lower levels is negative. Even if the curvature in the lower levels is positive, intermediate-scale unstable modes appear for smaller static stability and shear (Richardson number not necessarily small) or for certain vertical distributions of diabatic heating due to the liberation of latent heat in the lower troposphere. The amplitude of the most unstable intermediate-scale wave is confined to the lower troposphere and its growth rate increases with the inclusion of diabatic heating.
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      Subsynoptic-Scale Baroclinic Instability

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4154350
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    contributor authorSatyamurthy, Prakki
    contributor authorRao, Vadlamudi Brahmananda
    contributor authorMoura, Antonio Divino
    date accessioned2017-06-09T14:23:04Z
    date available2017-06-09T14:23:04Z
    date copyright1982/05/01
    date issued1982
    identifier issn0022-4928
    identifier otherams-18354.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4154350
    description abstractA linear stability analysis of the hyperbolic tangent profiles is made. A Boussinesq primitive equation model with high vertical resolution is used. Unstable modes of intermediate scales (Lx ≈ 1000 km) are generated when the curvature, d2?/dz2, of the basic flow in the lower levels is negative. Even if the curvature in the lower levels is positive, intermediate-scale unstable modes appear for smaller static stability and shear (Richardson number not necessarily small) or for certain vertical distributions of diabatic heating due to the liberation of latent heat in the lower troposphere. The amplitude of the most unstable intermediate-scale wave is confined to the lower troposphere and its growth rate increases with the inclusion of diabatic heating.
    publisherAmerican Meteorological Society
    titleSubsynoptic-Scale Baroclinic Instability
    typeJournal Paper
    journal volume39
    journal issue5
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1982)039<1052:SSBI>2.0.CO;2
    journal fristpage1052
    journal lastpage1061
    treeJournal of the Atmospheric Sciences:;1982:;Volume( 039 ):;issue: 005
    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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