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    The Mixing Efficiency of Stratified Turbulent Boundary Layers

    Source: Journal of Physical Oceanography:;2016:;Volume( 046 ):;issue: 010::page 3181
    Author:
    Scotti, Alberto
    ,
    White, Brian
    DOI: 10.1175/JPO-D-16-0095.1
    Publisher: American Meteorological Society
    Abstract: he mixing efficiency observed in stratified turbulent boundary layers is considered within the framework of the Monin?Obukhov similarity theory. It is shown that the efficiency within the layer increases with distance from the boundary. Near the boundary, the efficiency is proportional to the distance from the boundary scaled with the Monin?Obukhov length. Far from the boundary, the efficiency relaxes to a value that depends on the overall thickness of the layer relative to the Monin?Obukhov layer. This value approaches 1/6 when the thickness is larger than 1/2 of the Monin?Obukhov length. The same analysis shows that the buoyancy Reynolds number cannot be used to unequivocally predict the efficiency. The ?1/2 scaling between the efficiency and buoyancy Reynolds number that has been observed in field measurements and experiments is shown to depend on an extra dimensional scale and thus is not universal.
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      The Mixing Efficiency of Stratified Turbulent Boundary Layers

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4227221
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    contributor authorScotti, Alberto
    contributor authorWhite, Brian
    date accessioned2017-06-09T17:22:10Z
    date available2017-06-09T17:22:10Z
    date copyright2016/10/01
    date issued2016
    identifier issn0022-3670
    identifier otherams-83941.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4227221
    description abstracthe mixing efficiency observed in stratified turbulent boundary layers is considered within the framework of the Monin?Obukhov similarity theory. It is shown that the efficiency within the layer increases with distance from the boundary. Near the boundary, the efficiency is proportional to the distance from the boundary scaled with the Monin?Obukhov length. Far from the boundary, the efficiency relaxes to a value that depends on the overall thickness of the layer relative to the Monin?Obukhov layer. This value approaches 1/6 when the thickness is larger than 1/2 of the Monin?Obukhov length. The same analysis shows that the buoyancy Reynolds number cannot be used to unequivocally predict the efficiency. The ?1/2 scaling between the efficiency and buoyancy Reynolds number that has been observed in field measurements and experiments is shown to depend on an extra dimensional scale and thus is not universal.
    publisherAmerican Meteorological Society
    titleThe Mixing Efficiency of Stratified Turbulent Boundary Layers
    typeJournal Paper
    journal volume46
    journal issue10
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/JPO-D-16-0095.1
    journal fristpage3181
    journal lastpage3191
    treeJournal of Physical Oceanography:;2016:;Volume( 046 ):;issue: 010
    contenttypeFulltext
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    yabeshDSpacePersian
     
    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian