Baroclinic Instability in a Fluid with Three LayersSource: Journal of the Atmospheric Sciences:;1977:;Volume( 034 ):;issue: 008::page 1224Author:Davey, M. K.
DOI: 10.1175/1520-0469(1977)034<1224:BIIAFW>2.0.CO;2Publisher: American Meteorological Society
Abstract: A three-layer model is used to study the effect of curvature in the vertical profile of the horizontal velocity on the linear baroclinic instability of a simple quasi-geostrophic flow. Potential vorticity is conserved and the ?-effect is included. The results indicate that the range of unstable wavelengths increases as the curvature is increased from zero. For a given physical state, there may be more than one critical wavelength for which the waves are marginally stable. Growth rates for ? = 0 and the structure of the fastest growing waves are given. A comparison is made between two-layer, three-layer and continuous systems.
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contributor author | Davey, M. K. | |
date accessioned | 2017-06-09T14:19:39Z | |
date available | 2017-06-09T14:19:39Z | |
date copyright | 1977/08/01 | |
date issued | 1977 | |
identifier issn | 0022-4928 | |
identifier other | ams-17333.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4153216 | |
description abstract | A three-layer model is used to study the effect of curvature in the vertical profile of the horizontal velocity on the linear baroclinic instability of a simple quasi-geostrophic flow. Potential vorticity is conserved and the ?-effect is included. The results indicate that the range of unstable wavelengths increases as the curvature is increased from zero. For a given physical state, there may be more than one critical wavelength for which the waves are marginally stable. Growth rates for ? = 0 and the structure of the fastest growing waves are given. A comparison is made between two-layer, three-layer and continuous systems. | |
publisher | American Meteorological Society | |
title | Baroclinic Instability in a Fluid with Three Layers | |
type | Journal Paper | |
journal volume | 34 | |
journal issue | 8 | |
journal title | Journal of the Atmospheric Sciences | |
identifier doi | 10.1175/1520-0469(1977)034<1224:BIIAFW>2.0.CO;2 | |
journal fristpage | 1224 | |
journal lastpage | 1234 | |
tree | Journal of the Atmospheric Sciences:;1977:;Volume( 034 ):;issue: 008 | |
contenttype | Fulltext |