The Effect of Ambient Stratification and Moisture on the Motion of Atmospheric Undular BoresSource: Journal of the Atmospheric Sciences:;1986:;Volume( 043 ):;issue: 002::page 171Author:Crook, N. Andrew
DOI: 10.1175/1520-0469(1986)043<0171:TEOASA>2.0.CO;2Publisher: American Meteorological Society
Abstract: A numerical model is used to examine the effects of ambient stratification on the behavior of an atmospheric undular bore. It is shown that stratification reduces the amplitude of the disturbance at low levels by allowing energy to propagate upward. This reduction of amplitude can be inhibited by specifying winds opposing the wave motion in the middle and upper troposphere. Mean observations in the region where the Morning Glory is prevalent support this result. The effects of moisture are also examined. If condensation does not occur, moisture increases the disturbance amplitude by reducing, through virtual temperature effects, the stability of the atmosphere. However, if condensation occurs, the wave amplitude is decreased compared with a dry atmosphere with the same effective stability. Finally, it is shown that cloud formation increases the wavelength of the disturbance.
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contributor author | Crook, N. Andrew | |
date accessioned | 2017-06-09T14:26:11Z | |
date available | 2017-06-09T14:26:11Z | |
date copyright | 1986/01/01 | |
date issued | 1986 | |
identifier issn | 0022-4928 | |
identifier other | ams-19216.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4155308 | |
description abstract | A numerical model is used to examine the effects of ambient stratification on the behavior of an atmospheric undular bore. It is shown that stratification reduces the amplitude of the disturbance at low levels by allowing energy to propagate upward. This reduction of amplitude can be inhibited by specifying winds opposing the wave motion in the middle and upper troposphere. Mean observations in the region where the Morning Glory is prevalent support this result. The effects of moisture are also examined. If condensation does not occur, moisture increases the disturbance amplitude by reducing, through virtual temperature effects, the stability of the atmosphere. However, if condensation occurs, the wave amplitude is decreased compared with a dry atmosphere with the same effective stability. Finally, it is shown that cloud formation increases the wavelength of the disturbance. | |
publisher | American Meteorological Society | |
title | The Effect of Ambient Stratification and Moisture on the Motion of Atmospheric Undular Bores | |
type | Journal Paper | |
journal volume | 43 | |
journal issue | 2 | |
journal title | Journal of the Atmospheric Sciences | |
identifier doi | 10.1175/1520-0469(1986)043<0171:TEOASA>2.0.CO;2 | |
journal fristpage | 171 | |
journal lastpage | 181 | |
tree | Journal of the Atmospheric Sciences:;1986:;Volume( 043 ):;issue: 002 | |
contenttype | Fulltext |