METEOROLOGICAL CONDITIONS ASSOCIATED WITH THE DEVELOPMENT OF INSTABILITY LINESSource: Journal of Meteorology:;1958:;volume( 015 ):;issue: 003::page 297Author:Breiland, John G.
DOI: 10.1175/1520-0469(1958)015<0297:MCAWTD>2.0.CO;2Publisher: American Meteorological Society
Abstract: Results obtained from a diagnostic study of instability lines are presented. The results indicate that an instability line is associated with low-level horizontal convergence brought about primarily by the variation of the isentropic upgliding motion associated with a layer of strong, confluent winds in the lower levels of the troposphere.
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| contributor author | Breiland, John G. | |
| date accessioned | 2017-06-09T14:11:55Z | |
| date available | 2017-06-09T14:11:55Z | |
| date copyright | 1958/06/01 | |
| date issued | 1958 | |
| identifier issn | 0095-9634 | |
| identifier other | ams-14445.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4150007 | |
| description abstract | Results obtained from a diagnostic study of instability lines are presented. The results indicate that an instability line is associated with low-level horizontal convergence brought about primarily by the variation of the isentropic upgliding motion associated with a layer of strong, confluent winds in the lower levels of the troposphere. | |
| publisher | American Meteorological Society | |
| title | METEOROLOGICAL CONDITIONS ASSOCIATED WITH THE DEVELOPMENT OF INSTABILITY LINES | |
| type | Journal Paper | |
| journal volume | 15 | |
| journal issue | 3 | |
| journal title | Journal of Meteorology | |
| identifier doi | 10.1175/1520-0469(1958)015<0297:MCAWTD>2.0.CO;2 | |
| journal fristpage | 297 | |
| journal lastpage | 302 | |
| tree | Journal of Meteorology:;1958:;volume( 015 ):;issue: 003 | |
| contenttype | Fulltext |