Drivers of East Asian summer monsoon variability:Global oceans and the Tibetan Plateau  

东亚夏季风变率的驱动因子:全球海洋与青藏高原的协同影响

作　　者：Anmin Duan Guoxiong Wu Bin Wang Andrew G.Turner Jun Hu Wenting Hu Ping Zhang Die Hu Yuheng Tang 段安民;吴国雄;Bin Wang;Andrew G.Turner;胡俊;胡文婷;张萍;胡蝶;汤雨恒

机构地区：[1]Center for Marine Meteorology and Climate Change,State Key Laboratory of Marine Environmental Science,College of Ocean and Earth Sciences,Xiamen University,Xiamen 361102,China [2]State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics(LASG),Institute of Atmospheric Physics,Chinese Academy of Sciences,Beijing 100029,China [3]Department of Atmospheric Sciences,School of Ocean and Earth Science and Technology,University of Hawaii,Honolulu 96822,USA [4]Department of Meteorology,University of Reading,Reading RG67BE,UK

出　　处：《Science Bulletin》2024年第16期2487-2490,共4页科学通报（英文版）

基　　金：supported by the National Natural Science Foundation of China(42030602)。

摘　　要：The East Asian summer monsoon(EASM)profoundly influences the hydroclimate,ecosystems,and water resources of a densely populated region in Asia.Anomalous EASM can lead to floods,droughts,significant economic losses,and social disruption in East Asia and Southeast Asia.Unlike the Indian and African monsoons,the EASM is shaped by both tropical and extratropical climate systems,including tropical oceanic modes,cross-equatorial airflows,the Madden-Julian Oscillation,the thermal condition of the Tibetan Plateau,the South Asia High,and the mid-latitude westerly jet.

关 键 词：TIBETAN MONSOON EAST 

分 类 号：P461[天文地球—大气科学及气象学]