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    A Quasi-equilibrium Turbulent Energy Model for Geophysical Flows

    Source: Journal of the Atmospheric Sciences:;1988:;Volume( 045 ):;issue: 001::page 55
    Author:
    Galperin, B.
    ,
    Kantha, L. H.
    ,
    Hassid, S.
    ,
    Rosati, A.
    DOI: 10.1175/1520-0469(1988)045<0055:AQETEM>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The Mellor-Yamada hierarchy of turbulent closure models is reexamined to show that the elimination of a slight inconsistency in their analysis leads to a quasi-equilibrium model that is somewhat simpler than their level 2½ model. Also the need to impose realizability conditions restricting the dependence of exchange coefficients on shearing rates is eliminated. The model is therefore more robust while the principal advantage of the level 2½ model, namely the solution of a prognostic equation for turbulent kinetic energy is retained. Its performance is shown to be not much different from that of level 2½.
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      A Quasi-equilibrium Turbulent Energy Model for Geophysical Flows

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4155868
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    contributor authorGalperin, B.
    contributor authorKantha, L. H.
    contributor authorHassid, S.
    contributor authorRosati, A.
    date accessioned2017-06-09T14:27:54Z
    date available2017-06-09T14:27:54Z
    date copyright1988/01/01
    date issued1988
    identifier issn0022-4928
    identifier otherams-19720.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4155868
    description abstractThe Mellor-Yamada hierarchy of turbulent closure models is reexamined to show that the elimination of a slight inconsistency in their analysis leads to a quasi-equilibrium model that is somewhat simpler than their level 2½ model. Also the need to impose realizability conditions restricting the dependence of exchange coefficients on shearing rates is eliminated. The model is therefore more robust while the principal advantage of the level 2½ model, namely the solution of a prognostic equation for turbulent kinetic energy is retained. Its performance is shown to be not much different from that of level 2½.
    publisherAmerican Meteorological Society
    titleA Quasi-equilibrium Turbulent Energy Model for Geophysical Flows
    typeJournal Paper
    journal volume45
    journal issue1
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1988)045<0055:AQETEM>2.0.CO;2
    journal fristpage55
    journal lastpage62
    treeJournal of the Atmospheric Sciences:;1988:;Volume( 045 ):;issue: 001
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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