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    Possible Roles of Atlantic Circulations on the Weakening Indian Monsoon Rainfall–ENSO Relationship

    Source: Journal of Climate:;2001:;volume( 014 ):;issue: 011::page 2376
    Author:
    Chang, C-P.
    ,
    Harr, Patrick
    ,
    Ju, Jianhua
    DOI: 10.1175/1520-0442(2001)014<2376:PROACO>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Since the 1970s, the inverse relationship between the Indian monsoon rainfall and the El Niño?Southern Oscillation (ENSO) has weakened considerably. The cause for this breakdown is shown to be most likely the strengthening and poleward shift of the jet stream over the North Atlantic. These changes have led to the recent development of a significant correlation between wintertime western European surface air temperatures and the ensuing monsoon rainfall. This western Europe winter signal extended eastward over most of northern Eurasia and remained evident in spring, such that the effect of the resulting meridional temperature contrast was able to disrupt the influence of ENSO on the monsoon.
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      Possible Roles of Atlantic Circulations on the Weakening Indian Monsoon Rainfall–ENSO Relationship

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4198333
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    contributor authorChang, C-P.
    contributor authorHarr, Patrick
    contributor authorJu, Jianhua
    date accessioned2017-06-09T15:58:38Z
    date available2017-06-09T15:58:38Z
    date copyright2001/06/01
    date issued2001
    identifier issn0894-8755
    identifier otherams-5794.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4198333
    description abstractSince the 1970s, the inverse relationship between the Indian monsoon rainfall and the El Niño?Southern Oscillation (ENSO) has weakened considerably. The cause for this breakdown is shown to be most likely the strengthening and poleward shift of the jet stream over the North Atlantic. These changes have led to the recent development of a significant correlation between wintertime western European surface air temperatures and the ensuing monsoon rainfall. This western Europe winter signal extended eastward over most of northern Eurasia and remained evident in spring, such that the effect of the resulting meridional temperature contrast was able to disrupt the influence of ENSO on the monsoon.
    publisherAmerican Meteorological Society
    titlePossible Roles of Atlantic Circulations on the Weakening Indian Monsoon Rainfall–ENSO Relationship
    typeJournal Paper
    journal volume14
    journal issue11
    journal titleJournal of Climate
    identifier doi10.1175/1520-0442(2001)014<2376:PROACO>2.0.CO;2
    journal fristpage2376
    journal lastpage2380
    treeJournal of Climate:;2001:;volume( 014 ):;issue: 011
    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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