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作 者:Yuepeng HU Botao ZHOU Huijun WANG Dapeng ZHANG
机构地区:[1]Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters/Key Laboratory of Meteorological Disaster,Ministry of Education/Joint International Research Laboratory of Climate and Environment Change,Nanjing University of Information Science and Technology,Nanjing,210044,China [2]School of Atmospheric Sciences,Nanjing University of Information Science and Technology,Nanjing,210044,China
出 处:《Science China Earth Sciences》2024年第2期420-431,共12页中国科学(地球科学英文版)
基 金:supported by the National Natural Science Foundation of China(Grant No.42025502)。
摘 要:From summer to autumn in 2022,a severe drought lasted in southern China,posing serious effects on economic growth and ecological systems.This study explored the atmospheric circulations accounting for this persistent drought event.It shows that the drought in southern China during the summer of 2022 was strongly linked to the divergence of water vapor flux and descending motions,which were respectively caused by the anomalous anticyclone over the western North Pacific and the northward movement of the East Asian subtropical jet(EASJ).Differently,the atmospheric background responsible for the sustained drought in autumn is manly featured by a cyclonic circulation anomaly over the region from the Bay of Bengal to the South China Sea,which led to decreased moisture and descending motions in southern China.Further investigation suggests that the rarely strong surface warming over northern Eurasia and the extreme La Nina-like pattern over the tropical Pacific jointly resulted in the anomalous anticyclone over the western North Pacific and the northward shift of the EASJ in the summer of 2022,while the cyclonic circulation anomaly prevailing over the region from the Bay of Bengal to the South China Sea in autumn was largely attributed to the extremely negative anomalies of the tropical Indian Ocean sea surface temperature.
关 键 词:Summer-autumn drought Southern China Tropical sea surface temperature Eurasian warming
分 类 号:P467[天文地球—大气科学及气象学]
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