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    Comparison of Structure Parameter Scaling Expressions with Turbulence Closure Model Predictions

    Source: Journal of the Atmospheric Sciences:;1981:;Volume( 038 ):;issue: 004::page 751
    Author:
    Burk, Stephen D.
    DOI: 10.1175/1520-0469(1981)038<0751:COSPSE>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The convective boundary-layer scaling expressions presented by Wyngaard and LeMone (1980) are compared with predictions from a turbulence closure model. We first examine a model experiment involving a clear-air, convectively driven boundary layer overland. The model results agree well with scaling expressions and observations in the lower boundary layer and near the inversion. In the mid-boundary layer region, however, the closure model underestimates the temperature structure parameter CT2 and overestimates the humidity structure parameter Cq2. A cloud-topped marine boundary layer is examined in a second experiment which uses AMTEX data. Order-of-magnitude differences are found here between interfacial-layer scaling expressions and closure model predictions. Potential sources of this disagreement are discussed.
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      Comparison of Structure Parameter Scaling Expressions with Turbulence Closure Model Predictions

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4154094
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    contributor authorBurk, Stephen D.
    date accessioned2017-06-09T14:22:14Z
    date available2017-06-09T14:22:14Z
    date copyright1981/04/01
    date issued1981
    identifier issn0022-4928
    identifier otherams-18123.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4154094
    description abstractThe convective boundary-layer scaling expressions presented by Wyngaard and LeMone (1980) are compared with predictions from a turbulence closure model. We first examine a model experiment involving a clear-air, convectively driven boundary layer overland. The model results agree well with scaling expressions and observations in the lower boundary layer and near the inversion. In the mid-boundary layer region, however, the closure model underestimates the temperature structure parameter CT2 and overestimates the humidity structure parameter Cq2. A cloud-topped marine boundary layer is examined in a second experiment which uses AMTEX data. Order-of-magnitude differences are found here between interfacial-layer scaling expressions and closure model predictions. Potential sources of this disagreement are discussed.
    publisherAmerican Meteorological Society
    titleComparison of Structure Parameter Scaling Expressions with Turbulence Closure Model Predictions
    typeJournal Paper
    journal volume38
    journal issue4
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1981)038<0751:COSPSE>2.0.CO;2
    journal fristpage751
    journal lastpage761
    treeJournal of the Atmospheric Sciences:;1981:;Volume( 038 ):;issue: 004
    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