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    Diffusion Model for a Convective Layer. Part I: Numerical Simulation of Convective Boundary Layer

    Source: Journal of Climate and Applied Meteorology:;1986:;Volume( 025 ):;Issue: 010::page 1445
    Author:
    Sun, Wen-Yih
    ,
    Chang, Chiao-Zen
    DOI: 10.1175/1520-0450(1986)025<1445:DMFACL>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A simple turbulence model is used to study the moist convective boundary layer, in which a prognostic equation is applied to calculate the turbulent kinetic energy E. An observational length scale of the vertical velocity component, l, is used in the mixed layer, while a length scale associated with gravity waves is applied in the stable layer. The eddy coefficient is proportional to El. This model simulates well the temperature, mixing ratio and mean wind observed in the Wangara experiments. The turbulent kinetic energy and eddy fluxes generated are also in good agreement with those observed, as well as with those obtained from other more complicated models. Furthermore, the parameterization and results generated are used in a pollution model, which will be presented in Part II of this study.
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      Diffusion Model for a Convective Layer. Part I: Numerical Simulation of Convective Boundary Layer

    URI
    https://yetl.yabesh.ir/yetl1/handle/yetl/4146252
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    • Journal of Climate and Applied Meteorology

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    contributor authorSun, Wen-Yih
    contributor authorChang, Chiao-Zen
    date accessioned2017-06-09T14:01:24Z
    date available2017-06-09T14:01:24Z
    date copyright1986/10/01
    date issued1986
    identifier issn0733-3021
    identifier otherams-11065.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4146252
    description abstractA simple turbulence model is used to study the moist convective boundary layer, in which a prognostic equation is applied to calculate the turbulent kinetic energy E. An observational length scale of the vertical velocity component, l, is used in the mixed layer, while a length scale associated with gravity waves is applied in the stable layer. The eddy coefficient is proportional to El. This model simulates well the temperature, mixing ratio and mean wind observed in the Wangara experiments. The turbulent kinetic energy and eddy fluxes generated are also in good agreement with those observed, as well as with those obtained from other more complicated models. Furthermore, the parameterization and results generated are used in a pollution model, which will be presented in Part II of this study.
    publisherAmerican Meteorological Society
    titleDiffusion Model for a Convective Layer. Part I: Numerical Simulation of Convective Boundary Layer
    typeJournal Paper
    journal volume25
    journal issue10
    journal titleJournal of Climate and Applied Meteorology
    identifier doi10.1175/1520-0450(1986)025<1445:DMFACL>2.0.CO;2
    journal fristpage1445
    journal lastpage1453
    treeJournal of Climate and Applied Meteorology:;1986:;Volume( 025 ):;Issue: 010
    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