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    Kinetic Energy Transfer between Internal Gravity Waves and Turbulence

    Source: Journal of the Atmospheric Sciences:;1988:;Volume( 045 ):;issue: 003::page 486
    Author:
    Finnigan, J. J.
    DOI: 10.1175/1520-0469(1988)045<0486:KETBIG>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: We describe a reliable method for distinguishing the mean, wave and turbulence fields when internal waves with changing amplitude perturb the turbulent boundary layer. By integrating the component wave and turbulence kinetic energy budgets through the turbulent layer, we show that only mechanism trasnferring energy between wave and turbulent fields is the work done by the periodic part of the turbulent stress against the wave rate of strain. When these components are π/2 out of phase. the net energy transfer is zero. Eight wave-turbulence interaction events of differing stability are analyzed and interpreted using rapid distortion theory. When density stratification is approximately steady, the phase relationship does not change from π/2 However, periodicity in the stratification changes the phase angle and leads to strong energy transfer from wave to turbulence.
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      Kinetic Energy Transfer between Internal Gravity Waves and Turbulence

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4155896
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    contributor authorFinnigan, J. J.
    date accessioned2017-06-09T14:28:02Z
    date available2017-06-09T14:28:02Z
    date copyright1988/02/01
    date issued1988
    identifier issn0022-4928
    identifier otherams-19746.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4155896
    description abstractWe describe a reliable method for distinguishing the mean, wave and turbulence fields when internal waves with changing amplitude perturb the turbulent boundary layer. By integrating the component wave and turbulence kinetic energy budgets through the turbulent layer, we show that only mechanism trasnferring energy between wave and turbulent fields is the work done by the periodic part of the turbulent stress against the wave rate of strain. When these components are π/2 out of phase. the net energy transfer is zero. Eight wave-turbulence interaction events of differing stability are analyzed and interpreted using rapid distortion theory. When density stratification is approximately steady, the phase relationship does not change from π/2 However, periodicity in the stratification changes the phase angle and leads to strong energy transfer from wave to turbulence.
    publisherAmerican Meteorological Society
    titleKinetic Energy Transfer between Internal Gravity Waves and Turbulence
    typeJournal Paper
    journal volume45
    journal issue3
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1988)045<0486:KETBIG>2.0.CO;2
    journal fristpage486
    journal lastpage505
    treeJournal of the Atmospheric Sciences:;1988:;Volume( 045 ):;issue: 003
    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