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    A Numerical Study of Coupling Between the Boundary Layer and Free Atmosphere in an Accelerated Low-Latitude Flow

    Source: Journal of the Atmospheric Sciences:;1972:;Volume( 029 ):;issue: 008::page 1485
    Author:
    Mahrt, Larry J.
    DOI: 10.1175/1520-0469(1972)029<1485:ANSOCB>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The influence of advective accelerations in the low-latitude boundary layer and coupling between this boundary layer and the free atmosphere are numerically examined for steady longitudinally invariant flow. Pressure adjustments in a one-layer representation of the free atmosphere are induced by vertical fluxes of mass, momentum and latent heat out of a multi-level boundary layer model. It is found that vertical motions, resulting from advective accelerations in the boundary layer, can strongly influence pressure adjustments and flow development. As a result, the steady pressure field, generated by specified heating or parameterized latent heating, is quite different than would he predicted by linear boundary layer theory.
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      A Numerical Study of Coupling Between the Boundary Layer and Free Atmosphere in an Accelerated Low-Latitude Flow

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4152049
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    contributor authorMahrt, Larry J.
    date accessioned2017-06-09T14:16:42Z
    date available2017-06-09T14:16:42Z
    date copyright1972/11/01
    date issued1972
    identifier issn0022-4928
    identifier otherams-16283.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4152049
    description abstractThe influence of advective accelerations in the low-latitude boundary layer and coupling between this boundary layer and the free atmosphere are numerically examined for steady longitudinally invariant flow. Pressure adjustments in a one-layer representation of the free atmosphere are induced by vertical fluxes of mass, momentum and latent heat out of a multi-level boundary layer model. It is found that vertical motions, resulting from advective accelerations in the boundary layer, can strongly influence pressure adjustments and flow development. As a result, the steady pressure field, generated by specified heating or parameterized latent heating, is quite different than would he predicted by linear boundary layer theory.
    publisherAmerican Meteorological Society
    titleA Numerical Study of Coupling Between the Boundary Layer and Free Atmosphere in an Accelerated Low-Latitude Flow
    typeJournal Paper
    journal volume29
    journal issue8
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1972)029<1485:ANSOCB>2.0.CO;2
    journal fristpage1485
    journal lastpage1495
    treeJournal of the Atmospheric Sciences:;1972:;Volume( 029 ):;issue: 008
    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