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    On the Effect of Dissipation on Shear Instabilities in the Stable Atmospheric Boundary Layer

    Source: Journal of the Atmospheric Sciences:;1984:;Volume( 041 ):;issue: 005::page 888
    Author:
    Fuà, D.
    ,
    Einaudi, F.
    DOI: 10.1175/1520-0469(1984)041<0888:OTEODO>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: We are presenting the results of a stability analysis of a background wind shear in the presence of stable stratification and of height dependent coefficients of eddy viscosity and eddy thermal conduction. It is shown that the vertical gradients of the eddy coefficients substantially affect the phase velocities, growth rates and vertical structure of the gravity wave and are responsible for the appearance of some counter-gradient heat fluxes and Reynolds stresses. It is suggested that these gradients may explain the observed counter-gradient fluxes in the stable atmospheric boundary layer.
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      On the Effect of Dissipation on Shear Instabilities in the Stable Atmospheric Boundary Layer

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4154826
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    contributor authorFuà, D.
    contributor authorEinaudi, F.
    date accessioned2017-06-09T14:24:40Z
    date available2017-06-09T14:24:40Z
    date copyright1984/03/01
    date issued1984
    identifier issn0022-4928
    identifier otherams-18783.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4154826
    description abstractWe are presenting the results of a stability analysis of a background wind shear in the presence of stable stratification and of height dependent coefficients of eddy viscosity and eddy thermal conduction. It is shown that the vertical gradients of the eddy coefficients substantially affect the phase velocities, growth rates and vertical structure of the gravity wave and are responsible for the appearance of some counter-gradient heat fluxes and Reynolds stresses. It is suggested that these gradients may explain the observed counter-gradient fluxes in the stable atmospheric boundary layer.
    publisherAmerican Meteorological Society
    titleOn the Effect of Dissipation on Shear Instabilities in the Stable Atmospheric Boundary Layer
    typeJournal Paper
    journal volume41
    journal issue5
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1984)041<0888:OTEODO>2.0.CO;2
    journal fristpage888
    journal lastpage900
    treeJournal of the Atmospheric Sciences:;1984:;Volume( 041 ):;issue: 005
    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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