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contributor authorWexler, Raymond
date accessioned2017-06-09T14:11:16Z
date available2017-06-09T14:11:16Z
date copyright1955/08/01
date issued1955
identifier issn0095-9634
identifier otherams-14185.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4149718
description abstractA radar study of the streamers of 25 February 1954 at Cambridge, Mass., indicates that horizontal bands of rain are produced by the action of wind shear on the precipitation particles. It is suggested that a ?generating layer,? responsible for the streamer formation, consists of a cumuliform cloud configuration within which ice crystals grow rapidly both by sublimation and by riming.
publisherAmerican Meteorological Society
titleRADAR ANALYSIS OF PRECIPITATION STREAMERS OBSERVED 25 FEBRUARY 1954
typeJournal Paper
journal volume12
journal issue4
journal titleJournal of Meteorology
identifier doi10.1175/1520-0469(1955)012<0391:RAOPSO>2.0.CO;2
journal fristpage391
journal lastpage393
treeJournal of Meteorology:;1955:;volume( 012 ):;issue: 004
contenttypeFulltext


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