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    New Third-Order Moments for the Convective Boundary Layer

    Source: Journal of the Atmospheric Sciences:;2001:;Volume( 058 ):;issue: 009::page 1169
    Author:
    Canuto, V. M.
    ,
    Cheng, Y.
    ,
    Howard, A.
    DOI: 10.1175/1520-0469(2001)058<1169:NTOMFT>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Turbulent convection is inherently a nonlocal phenomenon and a primary condition for a successful treatment of the convective boundary layer is a reliable model of nonlocality. In the dynamic equations governing the convective flux, the turbulent kinetic energy, etc., nonlocality is represented by the third-order moments (TOMs). Since the simplest form, the so-called down gradient approximation (DGA), severely underestimates the TOMs (up to an order of magnitude), a more physical model is needed. In 1994, an analytical model was presented that was derived directly from the dynamical equations for the TOMs. It considerably improved the DGA but was a bit cumbersome to use and, more importantly, it was based on the quasi-normal (QN) approximation for the fourth-order moments. Here, we present a new analytic expression for the TOMs that is structurally simpler than the 1994 expression and avoids the QN approximation. The resulting fit to the LES data is superior to that of the 1994 model.
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      New Third-Order Moments for the Convective Boundary Layer

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4159327
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    contributor authorCanuto, V. M.
    contributor authorCheng, Y.
    contributor authorHoward, A.
    date accessioned2017-06-09T14:36:52Z
    date available2017-06-09T14:36:52Z
    date copyright2001/05/01
    date issued2001
    identifier issn0022-4928
    identifier otherams-22833.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4159327
    description abstractTurbulent convection is inherently a nonlocal phenomenon and a primary condition for a successful treatment of the convective boundary layer is a reliable model of nonlocality. In the dynamic equations governing the convective flux, the turbulent kinetic energy, etc., nonlocality is represented by the third-order moments (TOMs). Since the simplest form, the so-called down gradient approximation (DGA), severely underestimates the TOMs (up to an order of magnitude), a more physical model is needed. In 1994, an analytical model was presented that was derived directly from the dynamical equations for the TOMs. It considerably improved the DGA but was a bit cumbersome to use and, more importantly, it was based on the quasi-normal (QN) approximation for the fourth-order moments. Here, we present a new analytic expression for the TOMs that is structurally simpler than the 1994 expression and avoids the QN approximation. The resulting fit to the LES data is superior to that of the 1994 model.
    publisherAmerican Meteorological Society
    titleNew Third-Order Moments for the Convective Boundary Layer
    typeJournal Paper
    journal volume58
    journal issue9
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(2001)058<1169:NTOMFT>2.0.CO;2
    journal fristpage1169
    journal lastpage1172
    treeJournal of the Atmospheric Sciences:;2001:;Volume( 058 ):;issue: 009
    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