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contributor authorHolroyd, Edmond W.
date accessioned2017-06-09T13:58:44Z
date available2017-06-09T13:58:44Z
date copyright1982/04/01
date issued1982
identifier issn0021-8952
identifier otherams-10253.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4145350
description abstractA study of the influence of mountain-generated cumulonimbus systems on the rainfall of the northern Great Plains, using daily rainfalls and satellite images, has shown the seasonal variations and areal extent of the rain swaths. Rainfall from these systems is greatest during June and July. The greatest rainfalls occur ?400 km northeast from the eastern boundaries of the mountains; the rain then decreases to beyond 1000 km.
publisherAmerican Meteorological Society
titleSome Observations on Mountain-Generated Cumulonimbus Rainfall on the Northern Great Plains
typeJournal Paper
journal volume21
journal issue4
journal titleJournal of Applied Meteorology
identifier doi10.1175/1520-0450(1982)021<0560:SOOMGC>2.0.CO;2
journal fristpage560
journal lastpage565
treeJournal of Applied Meteorology:;1982:;volume( 021 ):;issue: 004
contenttypeFulltext


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