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contributor authorWexler, Raymond
date accessioned2017-06-09T14:09:45Z
date available2017-06-09T14:09:45Z
date copyright1947/02/01
date issued1947
identifier issn0095-9634
identifier otherams-13567.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4149031
description abstractThe theory of radar storm detection is briefly stated and applied to detection of the frontal storm of 18 June 1946. The precipitation pattern associated with the front is found to be a series of overlapping line squalls each about 100 miles in length. The mean rain intensity along the front is computed with the aid of radar theory.
publisherAmerican Meteorological Society
titleRADAR DETECTION OF A FRONTAL STORM 18 JUNE 1946
typeJournal Paper
journal volume4
journal issue1
journal titleJournal of Meteorology
identifier doi10.1175/1520-0469(1947)004<0038:RDOAFS>2.0.CO;2
journal fristpage38
journal lastpage44
treeJournal of Meteorology:;1947:;volume( 004 ):;issue: 001
contenttypeFulltext


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