INTENSIFICATION OF PRECIPITATION BY DIFFERENTIAL ADVECTION

dc.contributor.author	Miller, James E.
dc.date.accessioned	2017-06-09T14:11:18Z
dc.date.available	2017-06-09T14:11:18Z
dc.date.copyright	1955/10/01
dc.date.issued	1955
dc.identifier.issn	0095-9634
dc.identifier.other	ams-14202.pdf
dc.identifier.uri	http://onlinelibrary.yabesh.ir/handle/yetl/4149738
dc.description.abstract	The effect of vertical instability on the intensity of precipitation is illustrated by a theoretical example. This example and others from the literature lead to the hypothesis that instability produced by a process such as advection of cold air over warm, moist air acts on a precipitation system to increase the total amount and to cause high intensities for short periods over small areas. The latter part of the hypothesis is verified by an analysis of 21 rainy periods in the eastern United States.
dc.publisher	American Meteorological Society
dc.title	INTENSIFICATION OF PRECIPITATION BY DIFFERENTIAL ADVECTION
dc.type	Journal Paper
dc.journal.volume	12
dc.journal.issue	5
dc.journal.title	Journal of Meteorology
dc.identifier.doi	10.1175/1520-0469(1955)012<0472:IOPBDA>2.0.CO;2
dc.journal.fristpage	472
dc.journal.lastpage	477
dc.tree	Journal of Meteorology:;1955:;volume( 012 ):;issue: 005
dc.contenttype	Fulltext