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    A Numerical Model for Dispersion in a Convective Boundary Layer

    Source: Journal of the Atmospheric Sciences:;1993:;Volume( 050 ):;issue: 022::page 3775
    Author:
    Ahmed, Nizam U.
    ,
    Chai, Steven K.
    ,
    Telford, James W.
    DOI: 10.1175/1520-0469(1993)050<3775:ANMFDI>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A numerical model based on the convective plumes observed in the convecting planetary boundary layer has been developed for material dispersion from both elevated and ground source releases. Mechanistic formulation, rather than parameterization, or statistical behavior of PBL phenomenon, has been used as a basis. This model uses two universal constants, the turbulent entrainment constant, a, and decay constant, A. The model results have physical significance with regard to the observed plume behavior in a convective field. An observed case of diffusion has been simulated. The model results are in reasonable agreement with the observation without introducing any adjustable parameters to improve the fit.
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      A Numerical Model for Dispersion in a Convective Boundary Layer

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4157373
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    • Journal of the Atmospheric Sciences

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    contributor authorAhmed, Nizam U.
    contributor authorChai, Steven K.
    contributor authorTelford, James W.
    date accessioned2017-06-09T14:31:55Z
    date available2017-06-09T14:31:55Z
    date copyright1993/11/01
    date issued1993
    identifier issn0022-4928
    identifier otherams-21074.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4157373
    description abstractA numerical model based on the convective plumes observed in the convecting planetary boundary layer has been developed for material dispersion from both elevated and ground source releases. Mechanistic formulation, rather than parameterization, or statistical behavior of PBL phenomenon, has been used as a basis. This model uses two universal constants, the turbulent entrainment constant, a, and decay constant, A. The model results have physical significance with regard to the observed plume behavior in a convective field. An observed case of diffusion has been simulated. The model results are in reasonable agreement with the observation without introducing any adjustable parameters to improve the fit.
    publisherAmerican Meteorological Society
    titleA Numerical Model for Dispersion in a Convective Boundary Layer
    typeJournal Paper
    journal volume50
    journal issue22
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1993)050<3775:ANMFDI>2.0.CO;2
    journal fristpage3775
    journal lastpage3789
    treeJournal of the Atmospheric Sciences:;1993:;Volume( 050 ):;issue: 022
    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