Kinetic Energy Transfer between Internal Gravity Waves and TurbulenceSource: Journal of the Atmospheric Sciences:;1988:;Volume( 045 ):;issue: 003::page 486Author:Finnigan, J. J.
DOI: 10.1175/1520-0469(1988)045<0486:KETBIG>2.0.CO;2Publisher: 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.
|
Collections
Show full item record
contributor author | Finnigan, J. J. | |
date accessioned | 2017-06-09T14:28:02Z | |
date available | 2017-06-09T14:28:02Z | |
date copyright | 1988/02/01 | |
date issued | 1988 | |
identifier issn | 0022-4928 | |
identifier other | ams-19746.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4155896 | |
description 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. | |
publisher | American Meteorological Society | |
title | Kinetic Energy Transfer between Internal Gravity Waves and Turbulence | |
type | Journal Paper | |
journal volume | 45 | |
journal issue | 3 | |
journal title | Journal of the Atmospheric Sciences | |
identifier doi | 10.1175/1520-0469(1988)045<0486:KETBIG>2.0.CO;2 | |
journal fristpage | 486 | |
journal lastpage | 505 | |
tree | Journal of the Atmospheric Sciences:;1988:;Volume( 045 ):;issue: 003 | |
contenttype | Fulltext |