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    A Far-Reaching Footprint of the Tropical Pacific Meridional Mode on the Summer Rainfall over the Yellow River Loop Valley

    Source: Journal of Climate:;2010:;volume( 024 ):;issue: 010::page 2585
    Author:
    Li, Chun
    ,
    Wu, Lixin
    ,
    Chang, Ping
    DOI: 10.1175/2010JCLI3844.1
    Publisher: American Meteorological Society
    Abstract: ver thousands of years, the vicissitudes of the Yellow River and surrounding geographic environment form a unique river loop in northwestern China, namely, the Yellow River Loop Valley. Results from both observations and a climate model indicate that the summer rainfall over the Yellow River Loop Valley region can be remotely controlled by sea surface temperature fluctuations in the eastern subtropical North Pacific. This far-reaching teleconnection is achieved by an atmospheric wave train emanating from the eastern subtropical North Pacific, with a long traveling journey from the western to the Eastern Hemisphere. Furthermore, it is found that the SST forcing pattern resembles the Tropical Pacific Meridional Mode, a mode characterized by an interhemispheric temperature gradient and shift of the intertropical convergence zone in the eastern tropical Pacific.
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      A Far-Reaching Footprint of the Tropical Pacific Meridional Mode on the Summer Rainfall over the Yellow River Loop Valley

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4212555
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    contributor authorLi, Chun
    contributor authorWu, Lixin
    contributor authorChang, Ping
    date accessioned2017-06-09T16:36:07Z
    date available2017-06-09T16:36:07Z
    date copyright2011/05/01
    date issued2010
    identifier issn0894-8755
    identifier otherams-70741.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4212555
    description abstractver thousands of years, the vicissitudes of the Yellow River and surrounding geographic environment form a unique river loop in northwestern China, namely, the Yellow River Loop Valley. Results from both observations and a climate model indicate that the summer rainfall over the Yellow River Loop Valley region can be remotely controlled by sea surface temperature fluctuations in the eastern subtropical North Pacific. This far-reaching teleconnection is achieved by an atmospheric wave train emanating from the eastern subtropical North Pacific, with a long traveling journey from the western to the Eastern Hemisphere. Furthermore, it is found that the SST forcing pattern resembles the Tropical Pacific Meridional Mode, a mode characterized by an interhemispheric temperature gradient and shift of the intertropical convergence zone in the eastern tropical Pacific.
    publisherAmerican Meteorological Society
    titleA Far-Reaching Footprint of the Tropical Pacific Meridional Mode on the Summer Rainfall over the Yellow River Loop Valley
    typeJournal Paper
    journal volume24
    journal issue10
    journal titleJournal of Climate
    identifier doi10.1175/2010JCLI3844.1
    journal fristpage2585
    journal lastpage2598
    treeJournal of Climate:;2010:;volume( 024 ):;issue: 010
    contenttypeFulltext
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