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    Formulation of Turbulent Fluxes in the Stable Boundary Layer

    Source: Journal of the Atmospheric Sciences:;2003:;Volume( 060 ):;issue: 020::page 2538
    Author:
    Mahrt, L.
    ,
    Vickers, Dean
    DOI: 10.1175/1520-0469(2003)060<2538:FOTFIT>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The mixing lengths for heat and momentum are computed from seven levels of eddy correlation data during the Cooperative Atmosphere?Surface Exchange Study-1999 (CASES-99). A number of formulations of the mixing length are evaluated, including surface layer similarity theory, several hybrid similarity theories, a formulation based on the Richardson number, and a formulation based on the local shear. A formulation of the mixing length is examined, which approaches z-less similarity for large z and surface layer similarity close to the ground surface. A generalized version includes a dependence on boundary layer depth, which approaches the usual boundary layer height dependence for neutral conditions. However, for many of the observational cases, a boundary layer did not exist in the usual sense, in that turbulence was generated primarily above the surface inversion layer and occasionally extended downward toward the surface. For these cases, inclusion of z-less turbulence is crucial.
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      Formulation of Turbulent Fluxes in the Stable Boundary Layer

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4159898
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    contributor authorMahrt, L.
    contributor authorVickers, Dean
    date accessioned2017-06-09T14:38:22Z
    date available2017-06-09T14:38:22Z
    date copyright2003/10/01
    date issued2003
    identifier issn0022-4928
    identifier otherams-23347.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4159898
    description abstractThe mixing lengths for heat and momentum are computed from seven levels of eddy correlation data during the Cooperative Atmosphere?Surface Exchange Study-1999 (CASES-99). A number of formulations of the mixing length are evaluated, including surface layer similarity theory, several hybrid similarity theories, a formulation based on the Richardson number, and a formulation based on the local shear. A formulation of the mixing length is examined, which approaches z-less similarity for large z and surface layer similarity close to the ground surface. A generalized version includes a dependence on boundary layer depth, which approaches the usual boundary layer height dependence for neutral conditions. However, for many of the observational cases, a boundary layer did not exist in the usual sense, in that turbulence was generated primarily above the surface inversion layer and occasionally extended downward toward the surface. For these cases, inclusion of z-less turbulence is crucial.
    publisherAmerican Meteorological Society
    titleFormulation of Turbulent Fluxes in the Stable Boundary Layer
    typeJournal Paper
    journal volume60
    journal issue20
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(2003)060<2538:FOTFIT>2.0.CO;2
    journal fristpage2538
    journal lastpage2548
    treeJournal of the Atmospheric Sciences:;2003:;Volume( 060 ):;issue: 020
    contenttypeFulltext
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    yabeshDSpacePersian
     
    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian