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    Imprint of the Pacific Decadal Oscillation on the South China Sea Throughflow Variability

    Source: Journal of Climate:;2013:;volume( 026 ):;issue: 024::page 9797
    Author:
    Yu, Kai
    ,
    Qu, Tangdong
    DOI: 10.1175/JCLI-D-12-00785.1
    Publisher: American Meteorological Society
    Abstract: nalysis of the 62-yr hindcast outputs from an eddy-resolving ocean general circulation model reveals a prominent decadal variability in the upper-layer (0?745 m) Luzon Strait transport (LST), a key component of the South China Sea throughflow. This variability is in phase with the basin-scale wind stress anomalies associated with the Pacific decadal oscillation (PDO). A composite analysis shows that during the positive phase of the PDO, the Aleutian low and its related positive wind stress curl anomalies intrude southward, reducing the trade winds and enhancing the westerly wind anomalies in the tropical North Pacific. In response, the North Equatorial Current bifurcation shifts northward, resulting in a weaker Kuroshio east of Luzon and consequently a stronger South China Sea throughflow in the upper 745 m.
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      Imprint of the Pacific Decadal Oscillation on the South China Sea Throughflow Variability

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4222689
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    contributor authorYu, Kai
    contributor authorQu, Tangdong
    date accessioned2017-06-09T17:07:56Z
    date available2017-06-09T17:07:56Z
    date copyright2013/12/01
    date issued2013
    identifier issn0894-8755
    identifier otherams-79862.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4222689
    description abstractnalysis of the 62-yr hindcast outputs from an eddy-resolving ocean general circulation model reveals a prominent decadal variability in the upper-layer (0?745 m) Luzon Strait transport (LST), a key component of the South China Sea throughflow. This variability is in phase with the basin-scale wind stress anomalies associated with the Pacific decadal oscillation (PDO). A composite analysis shows that during the positive phase of the PDO, the Aleutian low and its related positive wind stress curl anomalies intrude southward, reducing the trade winds and enhancing the westerly wind anomalies in the tropical North Pacific. In response, the North Equatorial Current bifurcation shifts northward, resulting in a weaker Kuroshio east of Luzon and consequently a stronger South China Sea throughflow in the upper 745 m.
    publisherAmerican Meteorological Society
    titleImprint of the Pacific Decadal Oscillation on the South China Sea Throughflow Variability
    typeJournal Paper
    journal volume26
    journal issue24
    journal titleJournal of Climate
    identifier doi10.1175/JCLI-D-12-00785.1
    journal fristpage9797
    journal lastpage9805
    treeJournal of Climate:;2013:;volume( 026 ):;issue: 024
    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
    yabeshDSpacePersian