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作 者:Rong-Hua Zhang Lu Zhou Chuan Gao Lingjiang Tao 张荣华;周路;高川;陶灵江
机构地区:[1]School of Marine Sciences,Nanjing University of Information Science and Technology,Nanjing 210044,China [2]Key Laboratory of Ocean Observation and Forecasting and Key Laboratory of Ocean Circulation and Waves,Institute of Oceanology,Chinese Academy of Sciences,Qingdao 266071,China [3]University of Chinese Academy of Sciences,Beijing 101408,China [4]Laoshan Laboratory,Qingdao 266237,China
出 处:《Science Bulletin》2024年第15期2323-2327,共5页科学通报(英文版)
基 金:supported by the National Natural Science Foundation of China (42030410, 42176032);Laoshan Laboratory (LSKJ202202402);the Strategic Priority Research Program of the Chinese Academy of Sciences (XDB40000000);the Startup Foundation for Introducing Talent of NUIST。
摘 要:The El Nino-Southern Oscillation (ENSO) is the strongest interannual anomalies affecting weather and climate worldwide. As has been well recognized, ENSO originates from the coupling between the ocean and atmosphere in the tropical Pacific, characterized by a coherent evolution of subsurface temperature anomalies that profoundly impact sea surface temperature (SST) and surface wind fields.
关 键 词:OCEAN ATMOSPHERE INTERANNUAL
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