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    Pacific–East Asian Teleconnection: How Does ENSO Affect East Asian Climate?

    Source: Journal of Climate:;2000:;volume( 013 ):;issue: 009::page 1517
    Author:
    Wang, Bin
    ,
    Wu, Renguang
    ,
    Fu, Xiouhua
    DOI: 10.1175/1520-0442(2000)013<1517:PEATHD>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Observational evidence is presented to show a teleconnection between the central Pacific and East Asia during the extreme phases of ENSO cycles. This Pacific?East Asian teleconnection is confined to the lower troposphere. The key system that bridges the warm (cold) events in the eastern Pacific and the weak (strong) East Asian winter monsoons is an anomalous lower-tropospheric anticyclone (cyclone) located in the western North Pacific. The western North Pacific wind anomalies develop rapidly in late fall of the year when a strong warm or cold event matures. The anomalies persist until the following spring or early summer, causing anomalously wet (dry) conditions along the East Asian polar front stretching from southern China northeastward to the east of Japan (Kuroshio extension). Using atmospheric general circulation and intermediate models, the authors show that the anomalous Philippine Sea anticyclone results from a Rossby-wave response to suppressed convective heating, which is induced by both the in situ ocean surface cooling and the subsidence forced remotely by the central Pacific warming. The development of the anticyclone is nearly concurrent with the enhancement of the local sea surface cooling. Both the anticyclone and the cooling region propagate slowly eastward. The development and persistence of the teleconnection is primarily attributed to a positive thermodynamic feedback between the anticyclone and the sea surface cooling in the presence of mean northeasterly trades. The rapid establishment of the Philippine Sea wind and SST anomalies implies the occurrence of extratropical?tropical interactions through cold surge?induced exchanges of surface buoyancy flux. The central Pacific warming plays an essential role in the development of the western Pacific cooling and the wind anomalies by setting up a favorable environment for the anticyclone?SST interaction and midlatitude?tropical interaction in the western North Pacific.
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      Pacific–East Asian Teleconnection: How Does ENSO Affect East Asian Climate?

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4194523
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    • Journal of Climate

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    contributor authorWang, Bin
    contributor authorWu, Renguang
    contributor authorFu, Xiouhua
    date accessioned2017-06-09T15:49:42Z
    date available2017-06-09T15:49:42Z
    date copyright2000/05/01
    date issued2000
    identifier issn0894-8755
    identifier otherams-5451.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4194523
    description abstractObservational evidence is presented to show a teleconnection between the central Pacific and East Asia during the extreme phases of ENSO cycles. This Pacific?East Asian teleconnection is confined to the lower troposphere. The key system that bridges the warm (cold) events in the eastern Pacific and the weak (strong) East Asian winter monsoons is an anomalous lower-tropospheric anticyclone (cyclone) located in the western North Pacific. The western North Pacific wind anomalies develop rapidly in late fall of the year when a strong warm or cold event matures. The anomalies persist until the following spring or early summer, causing anomalously wet (dry) conditions along the East Asian polar front stretching from southern China northeastward to the east of Japan (Kuroshio extension). Using atmospheric general circulation and intermediate models, the authors show that the anomalous Philippine Sea anticyclone results from a Rossby-wave response to suppressed convective heating, which is induced by both the in situ ocean surface cooling and the subsidence forced remotely by the central Pacific warming. The development of the anticyclone is nearly concurrent with the enhancement of the local sea surface cooling. Both the anticyclone and the cooling region propagate slowly eastward. The development and persistence of the teleconnection is primarily attributed to a positive thermodynamic feedback between the anticyclone and the sea surface cooling in the presence of mean northeasterly trades. The rapid establishment of the Philippine Sea wind and SST anomalies implies the occurrence of extratropical?tropical interactions through cold surge?induced exchanges of surface buoyancy flux. The central Pacific warming plays an essential role in the development of the western Pacific cooling and the wind anomalies by setting up a favorable environment for the anticyclone?SST interaction and midlatitude?tropical interaction in the western North Pacific.
    publisherAmerican Meteorological Society
    titlePacific–East Asian Teleconnection: How Does ENSO Affect East Asian Climate?
    typeJournal Paper
    journal volume13
    journal issue9
    journal titleJournal of Climate
    identifier doi10.1175/1520-0442(2000)013<1517:PEATHD>2.0.CO;2
    journal fristpage1517
    journal lastpage1536
    treeJournal of Climate:;2000:;volume( 013 ):;issue: 009
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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