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    Katabatic Flow: Analytic Solution for Gradually Varying Eddy Diffusivities

    Source: Journal of the Atmospheric Sciences:;2001:;Volume( 058 ):;issue: 021::page 3349
    Author:
    Grisogono, Branko
    ,
    Oerlemans, Johannes
    DOI: 10.1175/1520-0469(2001)058<3349:KFASFG>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A simple form of the Prandtl model addressing pure katabatic flows is solved. The new analytic solution is valid for almost any assigned eddy diffusivity K(z) and constant Prandtl number. This model assumes a one-dimensional steady state for momentum and heat balance. Its approximate solution, obtained using the WKB method, appears as a generalization and improvement of the classic analytic solution for the constant-K case. It is compared favorably against a numerical solution. A comparison with observations from PASTEX, Austria 1994, shows that the new solution is much closer to the data than the constant-K solution. The dynamics revealed with this new solution is discussed (relatively sharper near-surface profiles, their gradients, and the low-level jet), and a suggestion toward improving boundary layer parameterizations is offered.
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      Katabatic Flow: Analytic Solution for Gradually Varying Eddy Diffusivities

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4159474
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    contributor authorGrisogono, Branko
    contributor authorOerlemans, Johannes
    date accessioned2017-06-09T14:37:13Z
    date available2017-06-09T14:37:13Z
    date copyright2001/11/01
    date issued2001
    identifier issn0022-4928
    identifier otherams-22966.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4159474
    description abstractA simple form of the Prandtl model addressing pure katabatic flows is solved. The new analytic solution is valid for almost any assigned eddy diffusivity K(z) and constant Prandtl number. This model assumes a one-dimensional steady state for momentum and heat balance. Its approximate solution, obtained using the WKB method, appears as a generalization and improvement of the classic analytic solution for the constant-K case. It is compared favorably against a numerical solution. A comparison with observations from PASTEX, Austria 1994, shows that the new solution is much closer to the data than the constant-K solution. The dynamics revealed with this new solution is discussed (relatively sharper near-surface profiles, their gradients, and the low-level jet), and a suggestion toward improving boundary layer parameterizations is offered.
    publisherAmerican Meteorological Society
    titleKatabatic Flow: Analytic Solution for Gradually Varying Eddy Diffusivities
    typeJournal Paper
    journal volume58
    journal issue21
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(2001)058<3349:KFASFG>2.0.CO;2
    journal fristpage3349
    journal lastpage3354
    treeJournal of the Atmospheric Sciences:;2001:;Volume( 058 ):;issue: 021
    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