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    Impacts of Different Types of El Niño on the East Asian Climate: Focus on ENSO Cycles

    Source: Journal of Climate:;2012:;volume( 025 ):;issue: 021::page 7702
    Author:
    Yuan, Yuan
    ,
    Yang, Song
    DOI: 10.1175/JCLI-D-11-00576.1
    Publisher: American Meteorological Society
    Abstract: sing multiple datasets and a partial correlation method, the authors analyze the different impacts of eastern Pacific (EP) and central Pacific (CP) El Niño on East Asian climate, focusing on the features from El Niño developing summer to El Niño decaying summer. Unlike the positive?negative?positive (+/?/+) anomalous precipitation pattern over East Asia and the equatorial Pacific during EP El Niño, an anomalous ?/+/? rainfall pattern appears during CP El Niño. The anomalous dry conditions over southeastern China and the northwestern Pacific during CP El Niño seem to result from the anomalous low-level anticyclone over southern China and the South China Sea, which is located more westward than the Philippine Sea anticyclone during EP El Niño. The continuous anomalous sinking motion over southeastern China, as part of the anomalous Walker circulation associated with CP El Niño, also contributes to these dry conditions.During the developing summer, the impact of CP El Niño on East Asian climate is more significant than the influence of EP El Niño. During the decaying summer, however, EP El Niño exerts a stronger influence on East Asia, probably due to the long-lasting anomalous warming over the tropical Indian Ocean accompanying EP El Niño.Temperatures over portions of East Asia and the northwestern Pacific tend to be above normal during EP El Niño but below normal from the developing autumn to the next spring during CP El Niño. A possible reason is the weakened (enhanced) East Asian winter monsoon related to EP (CP) El Niño.
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      Impacts of Different Types of El Niño on the East Asian Climate: Focus on ENSO Cycles

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4221977
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    contributor authorYuan, Yuan
    contributor authorYang, Song
    date accessioned2017-06-09T17:05:26Z
    date available2017-06-09T17:05:26Z
    date copyright2012/11/01
    date issued2012
    identifier issn0894-8755
    identifier otherams-79221.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4221977
    description abstractsing multiple datasets and a partial correlation method, the authors analyze the different impacts of eastern Pacific (EP) and central Pacific (CP) El Niño on East Asian climate, focusing on the features from El Niño developing summer to El Niño decaying summer. Unlike the positive?negative?positive (+/?/+) anomalous precipitation pattern over East Asia and the equatorial Pacific during EP El Niño, an anomalous ?/+/? rainfall pattern appears during CP El Niño. The anomalous dry conditions over southeastern China and the northwestern Pacific during CP El Niño seem to result from the anomalous low-level anticyclone over southern China and the South China Sea, which is located more westward than the Philippine Sea anticyclone during EP El Niño. The continuous anomalous sinking motion over southeastern China, as part of the anomalous Walker circulation associated with CP El Niño, also contributes to these dry conditions.During the developing summer, the impact of CP El Niño on East Asian climate is more significant than the influence of EP El Niño. During the decaying summer, however, EP El Niño exerts a stronger influence on East Asia, probably due to the long-lasting anomalous warming over the tropical Indian Ocean accompanying EP El Niño.Temperatures over portions of East Asia and the northwestern Pacific tend to be above normal during EP El Niño but below normal from the developing autumn to the next spring during CP El Niño. A possible reason is the weakened (enhanced) East Asian winter monsoon related to EP (CP) El Niño.
    publisherAmerican Meteorological Society
    titleImpacts of Different Types of El Niño on the East Asian Climate: Focus on ENSO Cycles
    typeJournal Paper
    journal volume25
    journal issue21
    journal titleJournal of Climate
    identifier doi10.1175/JCLI-D-11-00576.1
    journal fristpage7702
    journal lastpage7722
    treeJournal of Climate:;2012:;volume( 025 ):;issue: 021
    contenttypeFulltext
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