UNREST IN THE UPPER STRATOSPHERE OVER THE CARIBBEAN SEA DURING JANUARY 1960

dc.contributor.author	Riehl, Herbert
dc.contributor.author	Higgs, Ralph
dc.date.accessioned	2017-06-09T14:12:27Z
dc.date.available	2017-06-09T14:12:27Z
dc.date.copyright	1960/10/01
dc.date.issued	1960
dc.identifier.issn	0095-9634
dc.identifier.other	ams-14668.pdf
dc.identifier.uri	http://onlinelibrary.yabesh.ir/handle/yetl/4150254
dc.description.abstract	Wind observations were taken at a network of stations around the Caribbean from 100,000 to 120,000 ft altitude in January 1960. After an initial period of strong but variable easterly winds, a large disturbance emanated from the equatorial zone with structure similar to what is observed in the low troposphere during the hurricane season. The history of this equatorial shearline is described.
dc.publisher	American Meteorological Society
dc.title	UNREST IN THE UPPER STRATOSPHERE OVER THE CARIBBEAN SEA DURING JANUARY 1960
dc.type	Journal Paper
dc.journal.volume	17
dc.journal.issue	5
dc.journal.title	Journal of Meteorology
dc.identifier.doi	10.1175/1520-0469(1960)017<0555:UITUSO>2.0.CO;2
dc.journal.fristpage	555
dc.journal.lastpage	561
dc.tree	Journal of Meteorology:;1960:;volume( 017 ):;issue: 005
dc.contenttype	Fulltext