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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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