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    THE DEVELOPMENT AND DECAY OF THE 100-MB. SUMMERTIME ANTICYCLONE OVER SOUTHERN ASIA

    Source: Monthly Weather Review:;1963:;volume( 091 ):;issue: 001::page 3
    Author:
    MASON, RALPH B.
    ,
    ANDERSON, CALVIN E.
    DOI: 10.1175/1520-0493(1963)091<0003:TDADOT>2.3.CO;2
    Publisher: American Meteorological Society
    Abstract: The south Asian summer anticyclone is discussed with the aid of constant pressure charts, cross-sections, and graphs. The maximum anticyclonic circulation and the core of the subtropical easterly jet occurs close to the 100-mb. surface. Occasionally, this High migrates from its favored position over the Tibetan Plateau westward to the Caspian Sea. A Fourier analysis of the 100-mb. heights at 30° N. indicates that the longitudinal positioning of wave number one is a manifestation of the Asian anticyclone. An attempt to relate the appearance and variations in the surface southwest monsoon with the development of the high-level summertime circulation suggests that a direct vertical relationship is not straightforward and further study is needed to determine the exact nature of the linkage.
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      THE DEVELOPMENT AND DECAY OF THE 100-MB. SUMMERTIME ANTICYCLONE OVER SOUTHERN ASIA

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4197692
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    contributor authorMASON, RALPH B.
    contributor authorANDERSON, CALVIN E.
    date accessioned2017-06-09T15:57:12Z
    date available2017-06-09T15:57:12Z
    date copyright1963/01/01
    date issued1963
    identifier issn0027-0644
    identifier otherams-57364.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4197692
    description abstractThe south Asian summer anticyclone is discussed with the aid of constant pressure charts, cross-sections, and graphs. The maximum anticyclonic circulation and the core of the subtropical easterly jet occurs close to the 100-mb. surface. Occasionally, this High migrates from its favored position over the Tibetan Plateau westward to the Caspian Sea. A Fourier analysis of the 100-mb. heights at 30° N. indicates that the longitudinal positioning of wave number one is a manifestation of the Asian anticyclone. An attempt to relate the appearance and variations in the surface southwest monsoon with the development of the high-level summertime circulation suggests that a direct vertical relationship is not straightforward and further study is needed to determine the exact nature of the linkage.
    publisherAmerican Meteorological Society
    titleTHE DEVELOPMENT AND DECAY OF THE 100-MB. SUMMERTIME ANTICYCLONE OVER SOUTHERN ASIA
    typeJournal Paper
    journal volume91
    journal issue1
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1963)091<0003:TDADOT>2.3.CO;2
    journal fristpage3
    journal lastpage12
    treeMonthly Weather Review:;1963:;volume( 091 ):;issue: 001
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
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