METEOROLOGICAL CONDITIONS ASSOCIATED WITH THE DEVELOPMENT OF INSTABILITY LINES

dc.contributor.author	Breiland, John G.
dc.date.accessioned	2017-06-09T14:11:55Z
dc.date.available	2017-06-09T14:11:55Z
dc.date.copyright	1958/06/01
dc.date.issued	1958
dc.identifier.issn	0095-9634
dc.identifier.other	ams-14445.pdf
dc.identifier.uri	http://onlinelibrary.yabesh.ir/handle/yetl/4150007
dc.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.
dc.publisher	American Meteorological Society
dc.title	METEOROLOGICAL CONDITIONS ASSOCIATED WITH THE DEVELOPMENT OF INSTABILITY LINES
dc.type	Journal Paper
dc.journal.volume	15
dc.journal.issue	3
dc.journal.title	Journal of Meteorology
dc.identifier.doi	10.1175/1520-0469(1958)015<0297:MCAWTD>2.0.CO;2
dc.journal.fristpage	297
dc.journal.lastpage	302
dc.tree	Journal of Meteorology:;1958:;volume( 015 ):;issue: 003
dc.contenttype	Fulltext