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    Quasi-Biweekly Oscillation over the South China Sea in Late Summer: Propagation Dynamics and Energetics

    Source: Journal of Climate:;2017:;volume( 030 ):;issue: 011::page 4103
    Author:
    Wang, Xu;Chen, Guanghua
    DOI: 10.1175/JCLI-D-16-0533.1
    Publisher: American Meteorological Society
    Abstract: AbstractThe propagation dynamics and energetics of the quasi-biweekly oscillation (QBWO) over the South China Sea (SCS) in late summer [August?September (AS)] are investigated in this study. The QBWO originates from east of the Philippines and has a northwestward propagation. After arriving to the east of the SCS, the QBWO shifts to a westward migration and dominates over the SCS. The analyses of the vorticity budget suggest that the meridional wind anomaly could control the spatial migration of the vorticity anomaly through the ?-effect term and further influences the movement of the convection anomaly. It implies that the meridional wind is a crucial factor to drive the propagation of the QBWO. The energetics of the QBWO is investigated to understand the maintenance of the QBWO, which indicates that the convection anomaly could affect the circulation anomaly through the energy conversions to maintain the QBWO.
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      Quasi-Biweekly Oscillation over the South China Sea in Late Summer: Propagation Dynamics and Energetics

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4246034
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    contributor authorWang, Xu;Chen, Guanghua
    date accessioned2018-01-03T11:00:50Z
    date available2018-01-03T11:00:50Z
    date copyright2/16/2017 12:00:00 AM
    date issued2017
    identifier otherjcli-d-16-0533.1.pdf
    identifier urihttp://138.201.223.254:8080/yetl1/handle/yetl/4246034
    description abstractAbstractThe propagation dynamics and energetics of the quasi-biweekly oscillation (QBWO) over the South China Sea (SCS) in late summer [August?September (AS)] are investigated in this study. The QBWO originates from east of the Philippines and has a northwestward propagation. After arriving to the east of the SCS, the QBWO shifts to a westward migration and dominates over the SCS. The analyses of the vorticity budget suggest that the meridional wind anomaly could control the spatial migration of the vorticity anomaly through the ?-effect term and further influences the movement of the convection anomaly. It implies that the meridional wind is a crucial factor to drive the propagation of the QBWO. The energetics of the QBWO is investigated to understand the maintenance of the QBWO, which indicates that the convection anomaly could affect the circulation anomaly through the energy conversions to maintain the QBWO.
    publisherAmerican Meteorological Society
    titleQuasi-Biweekly Oscillation over the South China Sea in Late Summer: Propagation Dynamics and Energetics
    typeJournal Paper
    journal volume30
    journal issue11
    journal titleJournal of Climate
    identifier doi10.1175/JCLI-D-16-0533.1
    journal fristpage4103
    journal lastpage4112
    treeJournal of Climate:;2017:;volume( 030 ):;issue: 011
    contenttypeFulltext
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