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    Baroclinic Waves and Frontogenesis in a Non-Uniform Potential Vorticity Semi-Geostrophic Model

    Source: Journal of the Atmospheric Sciences:;1982:;Volume( 039 ):;issue: 009::page 1999
    Author:
    Heckley, W. A.
    ,
    Hoskins, B. J.
    DOI: 10.1175/1520-0469(1982)039<1999:BWAFIA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A three-dimensional semi-geostrophic model is used to study the nonlinear development of baroclinic waves on a zonal jet in a model atmosphere with a large change in potential vorticity in the region of the tropopause. The surface frontogenesis proceeds much as in the previous studies in which the tropopause was represented by a lid. However, the upper air development is much more realistic. In particular, there is a locally indirect forcing of the vertical circulation in the region of the upper air front which is easily understood in the present content.
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      Baroclinic Waves and Frontogenesis in a Non-Uniform Potential Vorticity Semi-Geostrophic Model

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4154415
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    • Journal of the Atmospheric Sciences

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    contributor authorHeckley, W. A.
    contributor authorHoskins, B. J.
    date accessioned2017-06-09T14:23:20Z
    date available2017-06-09T14:23:20Z
    date copyright1982/09/01
    date issued1982
    identifier issn0022-4928
    identifier otherams-18412.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4154415
    description abstractA three-dimensional semi-geostrophic model is used to study the nonlinear development of baroclinic waves on a zonal jet in a model atmosphere with a large change in potential vorticity in the region of the tropopause. The surface frontogenesis proceeds much as in the previous studies in which the tropopause was represented by a lid. However, the upper air development is much more realistic. In particular, there is a locally indirect forcing of the vertical circulation in the region of the upper air front which is easily understood in the present content.
    publisherAmerican Meteorological Society
    titleBaroclinic Waves and Frontogenesis in a Non-Uniform Potential Vorticity Semi-Geostrophic Model
    typeJournal Paper
    journal volume39
    journal issue9
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1982)039<1999:BWAFIA>2.0.CO;2
    journal fristpage1999
    journal lastpage2016
    treeJournal of the Atmospheric Sciences:;1982:;Volume( 039 ):;issue: 009
    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