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    Closure Schemes for Stably Stratified Atmospheric Flows without Turbulence Cutoff

    Source: Journal of the Atmospheric Sciences:;2016:;Volume( 073 ):;issue: 012::page 4817
    Author:
    Li, Dan
    ,
    Katul, Gabriel G.
    ,
    Zilitinkevich, Sergej S.
    DOI: 10.1175/JAS-D-16-0101.1
    Publisher: American Meteorological Society
    Abstract: wo recently proposed turbulence closure schemes are compared against the conventional Mellor?Yamada (MY) model for stably stratified atmospheric flows. The Energy- and Flux-Budget (EFB) approach solves the budgets of turbulent momentum and heat fluxes and turbulent kinetic and potential energies. The Cospectral Budget (CSB) approach is formulated in wavenumber space and integrated across all turbulent scales to obtain flow variables in physical space. Unlike the MY model, which is subject to a ?critical gradient Richardson number,? both EFB and CSB models allow turbulence to exist at any gradient Richardson number and predict a saturation of flux Richardson number at sufficiently large . The CSB approach further predicts the value of and reveals a unique expression linking the Rotta and von Kármán constants. Hence, all constants in the CSB model are nontunable and stability independent. All models agree that the dimensionless sensible heat flux decays with increasing . However, the decay rate and subsequent cutoff in the MY model appear abrupt. The MY model further exhibits an abrupt cutoff in the turbulent stress normalized by vertical velocity variance, while the CSB and EFB models display increasing trends. The EFB model produces a rapid increase in the ratio of turbulent potential energy and vertical velocity variance as is approached, suggesting a strong self-preservation mechanism. Vertical anisotropy in the turbulent kinetic energy is parameterized in different ways in MY and EFB, but this consideration is not required in CSB. Differences between EFB and CSB model predictions originate from how the vertical anisotropy is specified in the EFB model.
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      Closure Schemes for Stably Stratified Atmospheric Flows without Turbulence Cutoff

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4220171
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    contributor authorLi, Dan
    contributor authorKatul, Gabriel G.
    contributor authorZilitinkevich, Sergej S.
    date accessioned2017-06-09T16:59:42Z
    date available2017-06-09T16:59:42Z
    date copyright2016/12/01
    date issued2016
    identifier issn0022-4928
    identifier otherams-77596.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4220171
    description abstractwo recently proposed turbulence closure schemes are compared against the conventional Mellor?Yamada (MY) model for stably stratified atmospheric flows. The Energy- and Flux-Budget (EFB) approach solves the budgets of turbulent momentum and heat fluxes and turbulent kinetic and potential energies. The Cospectral Budget (CSB) approach is formulated in wavenumber space and integrated across all turbulent scales to obtain flow variables in physical space. Unlike the MY model, which is subject to a ?critical gradient Richardson number,? both EFB and CSB models allow turbulence to exist at any gradient Richardson number and predict a saturation of flux Richardson number at sufficiently large . The CSB approach further predicts the value of and reveals a unique expression linking the Rotta and von Kármán constants. Hence, all constants in the CSB model are nontunable and stability independent. All models agree that the dimensionless sensible heat flux decays with increasing . However, the decay rate and subsequent cutoff in the MY model appear abrupt. The MY model further exhibits an abrupt cutoff in the turbulent stress normalized by vertical velocity variance, while the CSB and EFB models display increasing trends. The EFB model produces a rapid increase in the ratio of turbulent potential energy and vertical velocity variance as is approached, suggesting a strong self-preservation mechanism. Vertical anisotropy in the turbulent kinetic energy is parameterized in different ways in MY and EFB, but this consideration is not required in CSB. Differences between EFB and CSB model predictions originate from how the vertical anisotropy is specified in the EFB model.
    publisherAmerican Meteorological Society
    titleClosure Schemes for Stably Stratified Atmospheric Flows without Turbulence Cutoff
    typeJournal Paper
    journal volume73
    journal issue12
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/JAS-D-16-0101.1
    journal fristpage4817
    journal lastpage4832
    treeJournal of the Atmospheric Sciences:;2016:;Volume( 073 ):;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
    yabeshDSpacePersian