A Note on Orographically Induced Instabilities in Two-Layer ModelsSource: Journal of the Atmospheric Sciences:;1983:;Volume( 040 ):;issue: 002::page 500Author:Källén, Erland
DOI: 10.1175/1520-0469(1983)040<0500:ANOOII>2.0.CO;2Publisher: American Meteorological Society
Abstract: In a low-order, two-layer model with orographic and zonal thermal and momentum forcing, two different types of orographically induced instabilities exist. One is of a barotropic nature with a westerly flow in the bottom layer, while the other one is close to a baroclinic instability of the basic long wave and has a very weak westerly or easterly bottom layer flow.
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| contributor author | Källén, Erland | |
| date accessioned | 2017-06-09T14:23:41Z | |
| date available | 2017-06-09T14:23:41Z | |
| date copyright | 1983/02/01 | |
| date issued | 1983 | |
| identifier issn | 0022-4928 | |
| identifier other | ams-18522.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4154537 | |
| description abstract | In a low-order, two-layer model with orographic and zonal thermal and momentum forcing, two different types of orographically induced instabilities exist. One is of a barotropic nature with a westerly flow in the bottom layer, while the other one is close to a baroclinic instability of the basic long wave and has a very weak westerly or easterly bottom layer flow. | |
| publisher | American Meteorological Society | |
| title | A Note on Orographically Induced Instabilities in Two-Layer Models | |
| type | Journal Paper | |
| journal volume | 40 | |
| journal issue | 2 | |
| journal title | Journal of the Atmospheric Sciences | |
| identifier doi | 10.1175/1520-0469(1983)040<0500:ANOOII>2.0.CO;2 | |
| journal fristpage | 500 | |
| journal lastpage | 505 | |
| tree | Journal of the Atmospheric Sciences:;1983:;Volume( 040 ):;issue: 002 | |
| contenttype | Fulltext |