Energy Dissipation Rates of Turbulence in the Stable Free AtmosphereSource: Journal of the Atmospheric Sciences:;1981:;Volume( 038 ):;issue: 004::page 880Author:Weinstock, J.
DOI: 10.1175/1520-0469(1981)038<0880:EDROTI>2.0.CO;2Publisher: American Meteorological Society
Abstract: For stable stratification, it is pointed out that there exists a strong correlation between the intensity of atmospheric turbulence and the energy dissipation rate ?. It is given in terms of the variance of vertical velocity σw2 and the Brunt-Väisälä frequency ?B by ? = 0.4 σw2?B. This relation is argued to have a wider range of applicability in the stratosphere than the previous relation ? = ? σw2, where ? is taken to be constant.
|
Collections
Show full item record
contributor author | Weinstock, J. | |
date accessioned | 2017-06-09T14:22:17Z | |
date available | 2017-06-09T14:22:17Z | |
date copyright | 1981/04/01 | |
date issued | 1981 | |
identifier issn | 0022-4928 | |
identifier other | ams-18133.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4154105 | |
description abstract | For stable stratification, it is pointed out that there exists a strong correlation between the intensity of atmospheric turbulence and the energy dissipation rate ?. It is given in terms of the variance of vertical velocity σw2 and the Brunt-Väisälä frequency ?B by ? = 0.4 σw2?B. This relation is argued to have a wider range of applicability in the stratosphere than the previous relation ? = ? σw2, where ? is taken to be constant. | |
publisher | American Meteorological Society | |
title | Energy Dissipation Rates of Turbulence in the Stable Free Atmosphere | |
type | Journal Paper | |
journal volume | 38 | |
journal issue | 4 | |
journal title | Journal of the Atmospheric Sciences | |
identifier doi | 10.1175/1520-0469(1981)038<0880:EDROTI>2.0.CO;2 | |
journal fristpage | 880 | |
journal lastpage | 883 | |
tree | Journal of the Atmospheric Sciences:;1981:;Volume( 038 ):;issue: 004 | |
contenttype | Fulltext |