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    Responses of Westerly Jets over Asia versus North America in the Last Glacial Maximum and Their Attributions 

    Source: Journal of Climate:;2024:;volume( 037 ):;issue: 002:;page 619
    Author(s): Lei, Jing; Shi, Zhengguo; Sha, Yingying; Li, Xinzhou; Xie, Xiaoning
    Publisher: American Meteorological Society
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    Seasonal Variation of the Westerly Jet over Asia in the Last Glacial Maximum: Role of the Tibetan Plateau Heating 

    Source: Journal of Climate:;2021:;volume( 034 ):;issue: 007:;page 2723
    Author(s): Lei, Jing;Shi, Zhengguo;Xie, Xiaoning;Sha, Yingying;Li, Xinzhou;Liu, Xiaodong;An, Zhisheng
    Publisher: American Meteorological Society
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    Global NDVI Patterns in Response to Atmospheric Water Vapor Anomalies over the Indo-Pacific Warm Pool during April–June 

    Source: Journal of Climate:;2018:;volume 032:;issue 004:;page 1167
    Author(s): Wang, Zhaosheng; Huang, Mei; Wang, Rong; Wang, Shaoqiang; Liu, Xiaodong; Xie, Xiaoning; Liu, Zhengjia; Gong, He; Hao, Man
    Publisher: American Meteorological Society
    Abstract: Vertically integrated atmospheric water vapor (VIWV) over the Indo-Pacific warm pool (IPWP) indirectly affects terrestrial vegetation growth (TVG) patterns through atmospheric water vapor transmission. However, their ...
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    Impact of the Tibetan Topography on Downwind Spatial Distribution of Fine Particulate Matter in Winter 

    Source: Journal of Climate:;2023:;volume( 036 ):;issue: 006
    Author(s): Cheng, Xugeng; Liu, Jane; Zhao, Tianliang; Xie, Xiaoning; Chen, Zhixiong; Shi, Zhengguo; Li, Xinzhou; Wang, Hong; Yang, Mengmiao; Tang, Nanjun
    Publisher: American Meteorological Society
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    Impact of the Tibetan Topography on Downwind Spatial Distribution of Fine Particulate Matter in Winter 

    Source: Journal of Climate:;2023:;volume( 036 ):;issue: 006:;page 1561
    Author(s): Cheng, Xugeng; Liu, Jane; Zhao, Tianliang; Xie, Xiaoning; Chen, Zhixiong; Shi, Zhengguo; Li, Xinzhou; Wang, Hong; Yang, Mengmiao; Tang, Nanjun
    Publisher: American Meteorological Society
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