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    Double-Nested Dynamical Downscaling Experiments over the Tibetan Plateau and Their Projection of Climate Change under Two RCP Scenarios 

    Source: Journal of the Atmospheric Sciences:;2012:;Volume( 070 ):;issue: 004:;page 1278
    Author(s): Ji, Zhenming; Kang, Shichang
    Publisher: American Meteorological Society
    Abstract: high-resolution regional climate model is used to simulate climate change over the Tibetan Plateau (TP). The model is driven at the grid spacing of 10 km by nesting the outputs of 50-km-resolution simulations. The results ...
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    Revisiting the Relationship between Observed Warming and Surface Pressure in the Tibetan Plateau 

    Source: Journal of Climate:;2016:;volume( 030 ):;issue: 005:;page 1721
    Author(s): You, Qinglong;Jiang, Zhihong;Moore, G. W. K.;Bao, Yuntao;Kong, Lei;Kang, Shichang
    Publisher: American Meteorological Society
    Abstract: AbstractThe Tibetan Plateau (TP) has an average elevation of over 4000 m and with its surrounding mountains is regarded as Earth?s ?third pole.? As a result of its size and height, climate change in the TP has its own ...
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    ROOF OF THE WORLD: Tibetan Observation and Research Platform 

    Source: Bulletin of the American Meteorological Society:;2008:;volume( 089 ):;issue: 010:;page 1487
    Author(s): Ma, Yaoming; Kang, Shichang; Zhu, Liping; Xu, Baiquing; Tian, Lide; Yao, Tandong
    Publisher: American Meteorological Society
    Abstract: The Tibetan Plateau, with the most prominent and complicated terrain on the globe and an elevation of more than 4,000 m, on average, above sea level, is very important in Asian monsoon circulation and global climate change. ...
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    Projected Changes in Snow Water Equivalent over the Tibetan Plateau under Global Warming of 1.5° and 2°C 

    Source: Journal of Climate:;2020:;volume( 33 ):;issue: 012:;page 5141
    Author(s): You, Qinglong;Wu, Fangying;Wang, Hongguo;Jiang, Zhihong;Pepin, Nick;Kang, Shichang
    Publisher: American Meteorological Society
    Abstract: Snow water equivalent (SWE) is a critical parameter for characterizing snowpack, which has a direct influence on the hydrological cycle, especially over high terrain. In this study, SWE from 18 coupled model simulations ...
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    Recent Third Pole’s Rapid Warming Accompanies Cryospheric Melt and Water Cycle Intensification and Interactions between Monsoon and Environment: Multidisciplinary Approach with Observations, Modeling, and Analysis 

    Source: Bulletin of the American Meteorological Society:;2018:;volume 100:;issue 003:;page 423
    Author(s): Yao, Tandong; Xue, Yongkang; Chen, Deliang; Chen, Fahu; Thompson, Lonnie; Cui, Peng; Koike, Toshio; Lau, William K.-M.; Lettenmaier, Dennis; Mosbrugger, Volker; Zhang, Renhe; Xu, Baiqing; Dozier, Jeff; Gillespie, Thomas; Gu, Yu; Kang, Shichang; Piao, Shil
    Publisher: American Meteorological Society
    Abstract: AbstractThe Third Pole (TP) is experiencing rapid warming and is currently in its warmest period in the past 2,000 years. This paper reviews the latest development in multidisciplinary TP research associated with this ...
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