THE MEAN UPPER-WIND CIRCULATION AROUND MONSOON DEPRESSIONS IN INDIA

dc.contributor.author	Mulky, G. R.
dc.contributor.author	Banerji, A. K.
dc.date.accessioned	2017-06-09T14:12:16Z
dc.date.available	2017-06-09T14:12:16Z
dc.date.copyright	1960/02/01
dc.date.issued	1960
dc.identifier.issn	0095-9634
dc.identifier.other	ams-14588.pdf
dc.identifier.uri	http://onlinelibrary.yabesh.ir/handle/yetl/4150165
dc.description.abstract	All available rawin observations taken within 400 mi from the centers of monsoon depressions in the Indian area have been used to obtain a picture of the average upper-wind circulation around the depressions. Cyclonic circulation is found to persist in the southwestern sector up to a height of 9 km, while in the other sectors it disappears at lower levels. Rainfall patterns associated with the depressions have been compared with the circulation in the upper levels. The inflow and outflow of air from the system have been assessed. The application of the concept of ?steering? has been examined.
dc.publisher	American Meteorological Society
dc.title	THE MEAN UPPER-WIND CIRCULATION AROUND MONSOON DEPRESSIONS IN INDIA
dc.type	Journal Paper
dc.journal.volume	17
dc.journal.issue	1
dc.journal.title	Journal of Meteorology
dc.identifier.doi	10.1175/1520-0469(1960)017<0008:TMUWCA>2.0.CO;2
dc.journal.fristpage	8
dc.journal.lastpage	14
dc.tree	Journal of Meteorology:;1960:;volume( 017 ):;issue: 001
dc.contenttype	Fulltext