Insights from the Second Tibetan Plateau Scientific Expedition: Unveiling the westerly–monsoon synergy and hydroclimate changes  

作　　者：Chaofan Li Yaoming Ma Tianjun Zhou Riyu Lu 

机构地区：[1]Center for Monsoon System Research,Institute of Atmospheric Physics,Chinese Academy of Sciences,Beijing,China [2]Land-Atmosphere Interaction and Its Climatic Effects Group,State Key Laboratory of Tibetan Plateau Earth System,Environment and Resources(TPESER),Institute of Tibetan Plateau Research,Chinese Academy of Sciences,Beijing,China [3]State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics,Institute of Atmospheric Physics,Chinese Academy of Sciences,Beijing,China [4]College of Hydraulic&Environmental Engineering,China Three Gorges University,Yichang,China [5]College of Earth and Planetary Sciences,University of Chinese Academy of Sciences,Beijing,China [6]College of Atmospheric Sciences,Lanzhou University,Lanzhou,China [7]Qomolangma Atmospheric and Environmental Observation and Research Station,Tingri,China [8]Kathmandu Center for Research and Education,Chinese Academy of Sciences-Tribhuvan University,Beijing,China [9]China-Pakistan Joint Research Center on Earth Sciences,Islamabad,Pakistan

出　　处：《Atmospheric and Oceanic Science Letters》2024年第5期1-2,共2页大气和海洋科学快报（英文版）

摘　　要：The Tibetan Plateau(TP),often referred to as the“Asian Water Tower”,holds vast reserves of glaciers,snow,and permafrost,serving as the crucial source for major rivers that support billions of people across Asia.The TP’s unique geographical positioning fosters significant interplay between the westerly and monsoon systems,the hydroclimate changes on the TP and its interactions with these two major atmospheric circulation systems through both the thermodynamic and dynamic processes,as well as the atmospheric water cycle of the TP.These interactions have far-reaching impacts on the weather and climate of China,Asia,and even the global atmospheric circulation.

关 键 词：TIBETAN Plateau holds 

分 类 号：P467[天文地球—大气科学及气象学]