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    Second-Order Closure PBL Model with New Third-Order Moments: Comparison with LES Data

    Source: Journal of the Atmospheric Sciences:;1994:;Volume( 051 ):;issue: 012::page 1605
    Author:
    Canuto, V. M.
    ,
    Minotti, F.
    ,
    Ronchi, C.
    ,
    Ypma, R. M.
    ,
    Zeman, O.
    DOI: 10.1175/1520-0469(1994)051<1605:SOCPMW>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: This paper contains two parts. In the first part, a new set of diagnostic equations is derived for the third-order moments for a buoyancy-driven flow, by exact inversion of the prognostic equations for the third-order moment equations in the stationary case. The third-order moments exhibit a universal structure: they all are a linear combination of the derivatives of all the second-order moments, w2, w?, ?2, and q2. Each term of the sum contains a turbulent diffusivity Dt, which also exhibits a universal structure of the form Dt = a?t + bw?. Since the sign of the convective flux changes depending on stable or unstable stratification, Dt varies according to the type of stratification. Here ?t ? wl (l is a mixing length and w is an rms velocity) represents the ?mechanical? part, while the ?buoyancy? part is represented by the convective flux w?. The quantities a and b are functions of the variable (Nτ)2, where N2 = gα?Θ/?z and τ is the turbulence time scale. The new expressions for the third-order moments generalize those of Zeman and Lumley, which were subsequently adopted by Sun and Ogura, Chen and Cotton, and Finger and Schmidt in their treatments of the convective boundary layer. In the second part, the new expressions for the third-order moments are used to solve the ensemble average equations describing a purely convective boundary layer heated from below at a constant rate. The computed second- and third-order moments are then compared with the corresponding LES results, most of which are obtained by running a new LES code, and part of which are taken from published results. The ensemble average results compare favorably with the LES data.
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      Second-Order Closure PBL Model with New Third-Order Moments: Comparison with LES Data

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4157515
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    • Journal of the Atmospheric Sciences

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    contributor authorCanuto, V. M.
    contributor authorMinotti, F.
    contributor authorRonchi, C.
    contributor authorYpma, R. M.
    contributor authorZeman, O.
    date accessioned2017-06-09T14:32:17Z
    date available2017-06-09T14:32:17Z
    date copyright1994/06/01
    date issued1994
    identifier issn0022-4928
    identifier otherams-21201.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4157515
    description abstractThis paper contains two parts. In the first part, a new set of diagnostic equations is derived for the third-order moments for a buoyancy-driven flow, by exact inversion of the prognostic equations for the third-order moment equations in the stationary case. The third-order moments exhibit a universal structure: they all are a linear combination of the derivatives of all the second-order moments, w2, w?, ?2, and q2. Each term of the sum contains a turbulent diffusivity Dt, which also exhibits a universal structure of the form Dt = a?t + bw?. Since the sign of the convective flux changes depending on stable or unstable stratification, Dt varies according to the type of stratification. Here ?t ? wl (l is a mixing length and w is an rms velocity) represents the ?mechanical? part, while the ?buoyancy? part is represented by the convective flux w?. The quantities a and b are functions of the variable (Nτ)2, where N2 = gα?Θ/?z and τ is the turbulence time scale. The new expressions for the third-order moments generalize those of Zeman and Lumley, which were subsequently adopted by Sun and Ogura, Chen and Cotton, and Finger and Schmidt in their treatments of the convective boundary layer. In the second part, the new expressions for the third-order moments are used to solve the ensemble average equations describing a purely convective boundary layer heated from below at a constant rate. The computed second- and third-order moments are then compared with the corresponding LES results, most of which are obtained by running a new LES code, and part of which are taken from published results. The ensemble average results compare favorably with the LES data.
    publisherAmerican Meteorological Society
    titleSecond-Order Closure PBL Model with New Third-Order Moments: Comparison with LES Data
    typeJournal Paper
    journal volume51
    journal issue12
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1994)051<1605:SOCPMW>2.0.CO;2
    journal fristpage1605
    journal lastpage1618
    treeJournal of the Atmospheric Sciences:;1994:;Volume( 051 ):;issue: 012
    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
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