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contributor authorConover, John H.
date accessioned2017-06-09T17:25:45Z
date available2017-06-09T17:25:45Z
date copyright1973/03/01
date issued1973
identifier issn0021-8952
identifier otherams-8509.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4228500
description abstractAnalysis of wind, pressure and cloudiness patterns shows that the weather of Southeast Asia during the southwest monsoon relates best to westward-moving equatorial waves. These waves are basically the same as those found over the western Pacific by other investigators although they are often not perceived without special analysis as they move through the vigorous monsoonal circulation. They are characterized by average wavelength of 3100 km, average period of 5½ days or speed of 6.5 m sec?1, a deep cool center from the surface to about the 300-mb level, and a deep band of convergence and cloudiness which feeds into the center from the southwest and south. Relatively good weather with lower amounts of cloudiness and areal precipitation coverage is normally found in the area of synoptic-scale subsidence between waves.
publisherAmerican Meteorological Society
titleWeather and Equatorial Waves Over Southeast Asia During the Summer Monsoon
typeJournal Paper
journal volume12
journal issue2
journal titleJournal of Applied Meteorology
identifier doi10.1175/1520-0450(1973)012<0281:WAEWOS>2.0.CO;2
journal fristpage281
journal lastpage291
treeJournal of Applied Meteorology:;1973:;volume( 012 ):;issue: 002
contenttypeFulltext


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