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    A MECHANISM FOR ASSISTING IN THE RELEASE OF CONVECTIVE INSTABILITY

    Source: Monthly Weather Review:;1955:;volume( 083 ):;issue: 001::page 1
    Author:
    BEEBE, ROBERT G.
    ,
    BATES, FERDINAND C.
    DOI: 10.1175/1520-0493(1955)083<0001:AMFAIT>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A model is proposed as one means whereby an air mass characterized by the ?typical? tornado sounding is converted to one described by the type of sounding observed in the vicinity of a tornado. By considering certain indications of the vorticity equation, it is possible to analyze configurations of jet axes and jet maxima such that low-level (850 mb.) convergence is surmounted by higher-level (500 mb.) divergence. Thus a model of jet structures is described which assists in, or possibly in some cases effects, the release of convective instability through vertical stretching or lifting. An example is presented to illustrate the use of this model in tornado forecasting and methods of application are outlined.
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      A MECHANISM FOR ASSISTING IN THE RELEASE OF CONVECTIVE INSTABILITY

    URI
    https://yetl.yabesh.ir/yetl1/handle/yetl/4197035
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    • Monthly Weather Review

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    contributor authorBEEBE, ROBERT G.
    contributor authorBATES, FERDINAND C.
    date accessioned2017-06-09T15:55:25Z
    date available2017-06-09T15:55:25Z
    date copyright1955/01/01
    date issued1955
    identifier issn0027-0644
    identifier otherams-56773.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4197035
    description abstractA model is proposed as one means whereby an air mass characterized by the ?typical? tornado sounding is converted to one described by the type of sounding observed in the vicinity of a tornado. By considering certain indications of the vorticity equation, it is possible to analyze configurations of jet axes and jet maxima such that low-level (850 mb.) convergence is surmounted by higher-level (500 mb.) divergence. Thus a model of jet structures is described which assists in, or possibly in some cases effects, the release of convective instability through vertical stretching or lifting. An example is presented to illustrate the use of this model in tornado forecasting and methods of application are outlined.
    publisherAmerican Meteorological Society
    titleA MECHANISM FOR ASSISTING IN THE RELEASE OF CONVECTIVE INSTABILITY
    typeJournal Paper
    journal volume83
    journal issue1
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1955)083<0001:AMFAIT>2.0.CO;2
    journal fristpage1
    journal lastpage10
    treeMonthly Weather Review:;1955:;volume( 083 ):;issue: 001
    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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