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    Weather and Equatorial Waves Over Southeast Asia During the Summer Monsoon

    Source: Journal of Applied Meteorology:;1973:;volume( 012 ):;issue: 002::page 281
    Author:
    Conover, John H.
    DOI: 10.1175/1520-0450(1973)012<0281:WAEWOS>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Analysis 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.
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      Weather and Equatorial Waves Over Southeast Asia During the Summer Monsoon

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4228500
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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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    DSpace software copyright © 2002-2015  DuraSpace
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