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    Hydrologic Processes Associated with the First Transition of the Asian Summer Monsoon: A Pilot Satellite Study

    Source: Bulletin of the American Meteorological Society:;1998:;volume( 079 ):;issue: 009::page 1871
    Author:
    Lau, K-M.
    ,
    Wu, H-T.
    ,
    Yang, S.
    DOI: 10.1175/1520-0477(1998)079<1871:HPAWTF>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Results of a pilot study of the evolution of large-scale hydrologic processes associated with the first transition of the Asian summer monsoon in conjunction with the launching of the South China Sea Monsoon Experiment (SCSMEX) in May 1998 are presented. SCSMEX is a major international field experiment to study the water and energy cycles of the Asian monsoon region, with the aim toward better understanding and improved prediction of the onset, maintenance, and variability of the monsoon of southern China, Southeast Asia, and the western pacific region. In this paper, the utility of reliable satellite data in revealing characteristics of the South China Sea (SCS) monsoon is emphasized. Using a combination of satellite-estimated rainfall, moisture, surface wind, and sea surface temperature, the authors present some interesting and hitherto unknown features in large-scale atmospheric and oceanic hydrologic processes associated with the fluctuation of the SCS monsoon. Results show that, climatologically, the SCS monsoon occurs during mid-May when a major convection zone shifts from the eastern Indian Ocean?southern Indochina to the SCS. Simultaneous with the SCS monsoon onset is the development of a moist tongue and frontal rainband emanating from the northern SCS, across southern China and the East China Sea to southern Japan, as well as the enhancement of equatorial convection in the western Pacific ITCZ. Analysis of the satellite-derived moisture and rainfall shows that the onset of the SCS monsoon during 1997 was preceded by the development of eastward-propagating supercloud clusters over the Indian Ocean. The satellite data also reveal a strong onset vortex over the SCS and large-scale cooling and warming patterns over the Indian Ocean and western Pacific. These features signal a major shift of the large-scale hydrologic cycle in the ocean?atmosphere system, which underpins the SCS monsoon onset. The paper concludes with a brief discussion of the observational platform of SCSMEX and a call for the use of satellite data, field observations, and models for comprehensive studies of the Asian monsoon.
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      Hydrologic Processes Associated with the First Transition of the Asian Summer Monsoon: A Pilot Satellite Study

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4161542
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    • Bulletin of the American Meteorological Society

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    contributor authorLau, K-M.
    contributor authorWu, H-T.
    contributor authorYang, S.
    date accessioned2017-06-09T14:42:13Z
    date available2017-06-09T14:42:13Z
    date copyright1998/09/01
    date issued1998
    identifier issn0003-0007
    identifier otherams-24827.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4161542
    description abstractResults of a pilot study of the evolution of large-scale hydrologic processes associated with the first transition of the Asian summer monsoon in conjunction with the launching of the South China Sea Monsoon Experiment (SCSMEX) in May 1998 are presented. SCSMEX is a major international field experiment to study the water and energy cycles of the Asian monsoon region, with the aim toward better understanding and improved prediction of the onset, maintenance, and variability of the monsoon of southern China, Southeast Asia, and the western pacific region. In this paper, the utility of reliable satellite data in revealing characteristics of the South China Sea (SCS) monsoon is emphasized. Using a combination of satellite-estimated rainfall, moisture, surface wind, and sea surface temperature, the authors present some interesting and hitherto unknown features in large-scale atmospheric and oceanic hydrologic processes associated with the fluctuation of the SCS monsoon. Results show that, climatologically, the SCS monsoon occurs during mid-May when a major convection zone shifts from the eastern Indian Ocean?southern Indochina to the SCS. Simultaneous with the SCS monsoon onset is the development of a moist tongue and frontal rainband emanating from the northern SCS, across southern China and the East China Sea to southern Japan, as well as the enhancement of equatorial convection in the western Pacific ITCZ. Analysis of the satellite-derived moisture and rainfall shows that the onset of the SCS monsoon during 1997 was preceded by the development of eastward-propagating supercloud clusters over the Indian Ocean. The satellite data also reveal a strong onset vortex over the SCS and large-scale cooling and warming patterns over the Indian Ocean and western Pacific. These features signal a major shift of the large-scale hydrologic cycle in the ocean?atmosphere system, which underpins the SCS monsoon onset. The paper concludes with a brief discussion of the observational platform of SCSMEX and a call for the use of satellite data, field observations, and models for comprehensive studies of the Asian monsoon.
    publisherAmerican Meteorological Society
    titleHydrologic Processes Associated with the First Transition of the Asian Summer Monsoon: A Pilot Satellite Study
    typeJournal Paper
    journal volume79
    journal issue9
    journal titleBulletin of the American Meteorological Society
    identifier doi10.1175/1520-0477(1998)079<1871:HPAWTF>2.0.CO;2
    journal fristpage1871
    journal lastpage1882
    treeBulletin of the American Meteorological Society:;1998:;volume( 079 ):;issue: 009
    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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