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    Low-Frequency Equatorial Waves in Vertically Sheared Zonal Flow. Part I: Stable Waves 

    Source: Journal of the Atmospheric Sciences:;1996:;Volume( 053 ):;issue: 003:;page 449
    Author(s): Wang, Bin; Xie, Xiaosu
    Publisher: American Meteorological Society
    Abstract: The mechanism by which a vertically sheared zonal flow affects large-scale, low-frequency equatorial waves is investigated with two-level equatorial,?-plane and spherical coordinates models. Vertical shears couple barolinic ...
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    Low-Frequency Equatorial Waves in Vertically Sheared Zonal Flow. Part II: Unstable Waves 

    Source: Journal of the Atmospheric Sciences:;1996:;Volume( 053 ):;issue: 023:;page 3589
    Author(s): Xie, Xiaosu; Wang, Bin
    Publisher: American Meteorological Society
    Abstract: The stability of equatorial Rossby waves in the presence of mean flow vertical shear and moisture convergence-induced heating is investigated with a primitive equation model on an equatorial ? plane. A vertical shear alone ...
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    A Model for the Boreal Summer Intraseasonal Oscillation 

    Source: Journal of the Atmospheric Sciences:;1997:;Volume( 054 ):;issue: 001:;page 72
    Author(s): Wang, Bin; Xie, Xiaosu
    Publisher: American Meteorological Society
    Abstract: The tropical intraseasonal oscillation (ISO) exhibits pronounced seasonality. The boreal summer ISO is more complex than its winter counterpart due to the coexistence of equatorial eastward, off-equatorial westward, and ...
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    Coupled Modes of the Warm Pool Climate System. Part I: The Role of Air–Sea Interaction in Maintaining Madden–Julian Oscillation 

    Source: Journal of Climate:;1998:;volume( 011 ):;issue: 008:;page 2116
    Author(s): Wang, Bin; Xie, Xiaosu
    Publisher: American Meteorological Society
    Abstract: Over the warm pool of the equatorial Indian and western Pacific Oceans, both the climatological mean state and the processes of atmosphere?ocean interaction differ fundamentally from their counterparts over the cold tongue ...
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    Coupled Modes of the Warm Pool Climate System. Part I: The Role of Air–Sea Interaction in Maintaining Madden–Julian Oscillation 

    Source: Journal of Climate:;1998:;volume( 011 ):;issue: 008:;page 2116
    Author(s): Wang, Bin; Xie, Xiaosu
    Publisher: American Meteorological Society
    Abstract: Over the warm pool of the equatorial Indian and western Pacific Oceans, both the climatological mean state and the processes of atmosphere?ocean interaction differ fundamentally from their counterparts over the cold tongue ...
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    Premonsoon Drought in India Observed from Space 

    Source: Journal of Hydrometeorology:;2016:;Volume( 018 ):;issue: 003:;page 683
    Author(s): Liu, W. Timothy; Xie, Xiaosu
    Publisher: American Meteorological Society
    Abstract: atellite observations between 2007 and 2015 are used to characterize the annual occurrence of the premonsoon drought (PMD), which causes human death and economic hardship in India, and to postulate its scientific causes. ...
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    Ocean–Atmosphere Interaction over Agulhas Extension Meanders 

    Source: Journal of Climate:;2007:;volume( 020 ):;issue: 023:;page 5784
    Author(s): Liu, W. Timothy; Xie, Xiaosu; Niiler, Pearn P.
    Publisher: American Meteorological Society
    Abstract: Many years of high-resolution measurements by a number of space-based sensors and from Lagrangian drifters became available recently and are used to examine the persistent atmospheric imprints of the semipermanent meanders ...
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