Effects of Northern Hemisphere Annular Mode on terrestrial near-surface wind speed over eastern China from 1979 to 2017OA
Effects of Northern Hemisphere Annular Mode on terrestrial near-surface wind speed over eastern China from 1979 to 2017
Jin-Lin ZHA;Cheng SHEN;Jian WU;De-Ming ZHAO;Wen-Xuan FAN;Hui-Ping JIANG;Cesar AZORIN-MOLINA;Deliang CHEN
Key Laboratory of Atmospheric Environment and Processes in the Boundary Layer Over the Low-Latitude Plateau Region,Department of Atmospheric Science,Yunnan University,Kunming 650091,ChinaKey Laboratory of Regional Climate and Environment for Temperate East Asia,Institute of Atmospheric Physics,Chinese Academy of Sciences,Beijing 100029,ChinaRegional Climate Group,Department of Earth Sciences,University of Gothenburg,Gothenburg 004631,SwedenKey Laboratory of Atmospheric Environment and Processes in the Boundary Layer Over the Low-Latitude Plateau Region,Department of Atmospheric Science,Yunnan University,Kunming 650091,ChinaKey Laboratory of Regional Climate and Environment for Temperate East Asia,Institute of Atmospheric Physics,Chinese Academy of Sciences,Beijing 100029,ChinaKey Laboratory of Atmospheric Environment and Processes in the Boundary Layer Over the Low-Latitude Plateau Region,Department of Atmospheric Science,Yunnan University,Kunming 650091,ChinaInternational Research Center of Big Data for Sustainable Development Goals(CBAS),Beijing 100094,ChinaKey Laboratory of Digital Earth Science,Aerospace Information Research Institute(AIR),Chinese Academy of Sciences,Beijing 100094,China
Near-surface wind speedTemperature gradientPressure gradientNorthern Hemisphere Annular ModeLarge-scale ocean-atmosphere circulations
Near-surface wind speedTemperature gradientPressure gradientNorthern Hemisphere Annular ModeLarge-scale ocean-atmosphere circulations
《气候变化研究进展(英文版)》 2022 (6)
能见度反演气溶胶光学厚度方法的改进
875-883,9
The authors cordially thank the anonymous reviewers and editors for their thorough comments and constructive sug-gestions,which greatly improve the quality of this study.The work was supported by the National Key Research and Development Program of China(2018YFA0606004),Natural Science Foundation of China(42005023,41875178,41865001),Swedish Formas(2019-00509 and 2017-01408),and VR(2021-02163 and 2019-03954).This work is also supported by the High-level Talents Program of Yunnan University,the Program for"Xingdian"Talent of Yunnan Province,the Program for Key Laboratory at the University of Yunnan Province,and the Chinese Jiangsu Collaborative Innovation Center for Climate Change.
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