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contributor authorYin, Maung Tun
date accessioned2017-06-09T14:10:07Z
date available2017-06-09T14:10:07Z
date copyright1949/12/01
date issued1949
identifier issn0095-9634
identifier otherams-13725.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4149207
description abstractA comparison of the mean winter and summer flow patterns at 8 km in the vicinity of India shows that a trough located to the east of India in winter has shifted westward by summer. A study of the onset of the summer monsoon during 1946 shows that this movement is comparatively rapid and coincides with the ?burst of the monsoon? over India. The movement of the trough is explained as being due to changes in the long-wave pattern brought about by the presence of the Himalayan mountain complex combined with seasonal variations in the latitude of the circumpolar jet stream of the northern hemisphere.
publisherAmerican Meteorological Society
titleSYNOPTIC-AEROLOGIC STUDY OF THE ONSET OF THE SUMMER MONSOON OVER INDIA AND BURMA
typeJournal Paper
journal volume6
journal issue6
journal titleJournal of Meteorology
identifier doi10.1175/1520-0469(1949)006<0393:SASOTO>2.0.CO;2
journal fristpage393
journal lastpage400
treeJournal of Meteorology:;1949:;volume( 006 ):;issue: 006
contenttypeFulltext


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