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    A Numerical Study of Atmospheric Density Current Motion Including the Effects of Condensation

    Source: Journal of the Atmospheric Sciences:;1986:;Volume( 043 ):;issue: 024::page 3068
    Author:
    Seitter, Keith L.
    DOI: 10.1175/1520-0469(1986)043<3068:ANSOAD>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A new form of the density current speed equation is presented which uses the surface pressure rise to predict the speed of the current front. This allows the speed prediction to be made with only surface measured quantities. This form of the equation is tested on gust front observations and numerical density current simulations and found to give good results. A simple, moist numerical model is used to simulate dry density currents and moist currents which produce an arc/rop cloud. The numerical results provide information on the lifting associated with density current passage and the forced updraft velocities at the front, and also show that use of the pressure form of the density current speed equation is especially important when condensation is occurring above the density current.
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      A Numerical Study of Atmospheric Density Current Motion Including the Effects of Condensation

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4155541
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    contributor authorSeitter, Keith L.
    date accessioned2017-06-09T14:26:55Z
    date available2017-06-09T14:26:55Z
    date copyright1986/12/01
    date issued1986
    identifier issn0022-4928
    identifier otherams-19426.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4155541
    description abstractA new form of the density current speed equation is presented which uses the surface pressure rise to predict the speed of the current front. This allows the speed prediction to be made with only surface measured quantities. This form of the equation is tested on gust front observations and numerical density current simulations and found to give good results. A simple, moist numerical model is used to simulate dry density currents and moist currents which produce an arc/rop cloud. The numerical results provide information on the lifting associated with density current passage and the forced updraft velocities at the front, and also show that use of the pressure form of the density current speed equation is especially important when condensation is occurring above the density current.
    publisherAmerican Meteorological Society
    titleA Numerical Study of Atmospheric Density Current Motion Including the Effects of Condensation
    typeJournal Paper
    journal volume43
    journal issue24
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1986)043<3068:ANSOAD>2.0.CO;2
    journal fristpage3068
    journal lastpage3076
    treeJournal of the Atmospheric Sciences:;1986:;Volume( 043 ):;issue: 024
    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