globalchange  > 影响、适应和脆弱性
DOI: 10.1007/s00382-017-4002-5
Scopus记录号: 2-s2.0-85033497111
论文题名:
Interdecadal change on the relationship between the mid-summer temperature in South China and atmospheric circulation and sea surface temperature
作者: Chen R.; Wen Z.; Lu R.
刊名: Climate Dynamics
ISSN: 9307575
出版年: 2018
卷: 51, 期:2018-05-06
起始页码: 2113
结束页码: 2126
语种: 英语
英文关键词: Interannual variation ; Interdecadal change ; Mid-summer temperature ; South China
Scopus关键词: air temperature ; annual variation ; atmospheric circulation ; climate change ; decadal variation ; high pressure ; sea surface temperature ; summer ; teleconnection ; temperature anomaly ; China ; Korea ; Lake Baikal ; Russian Federation ; Urals
英文摘要: South China suffers from high temperature frequently in mid-summer and this study aims to explore the interdecadal change of interannual variation of the mid-summer temperature in South China. It is revealed that the relationship between South China temperature and atmospheric circulation and sea surface temperature anomaly (SSTA) experiences an interdecadal change around the early 1990s. Before the early 1990s, warmer summer in South China is associated with the mid-latitude teleconnection featured by higher pressure over the Ural Mountains and the Korean Peninsula and lower pressure around the Lake Baikal. South China is located at the southern flank of an anomalous high pressure. After the early 1990s, South China temperature is prominently influenced by the tropical SSTA, and meanwhile the mid-latitude teleconnection becomes much weaker. Warmer summer is associated with higher pressure centered over South China and the El Niño to La Niña transition phase. The higher pressure influencing South China is located more southwards after the early 1990s, and it is favored by the tropical SSTA. The warmer SST in summer over the western tropical Pacific enhances the local convection and triggers an anomalous local Hadley cell with stronger subsidence over South China, directly leading to higher pressure over South China. Moreover, the colder SST over the central–eastern Pacific induces an anomalous Walker circulation and further strengthens the convection over the western tropical Pacific, exerting an indirect impact on the higher pressure over South China. The relative role of the western Pacific warming and central–eastern Pacific cooling is verified by CAM4 simulations. The intimate relationship between the tropical SSTA and South China temperature occurs during the El Niño to La Niña transition phase, which is the case after the early 1990s and suggests higher predictability for South China temperature in the recent decades. © 2017, Springer-Verlag GmbH Germany, part of Springer Nature.
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/109135
Appears in Collections:影响、适应和脆弱性
气候变化事实与影响

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作者单位: Center for Monsoon and Environment Research/Guangdong Province Key Laboratory for Climate Change and Natural Disaster Studies/School of Atmospheric Sciences, Sun Yat-sen University, Guangzhou, 510275, China; Institute of Atmospheric Sciences, Fudan University, Shanghai, China; State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, 100029, China; University of the Chinese Academy of Sciences, Beijing, 100049, China; Jiangsu Collaborative Innovation Center for Climate Change, Nanjing, China

Recommended Citation:
Chen R.,Wen Z.,Lu R.. Interdecadal change on the relationship between the mid-summer temperature in South China and atmospheric circulation and sea surface temperature[J]. Climate Dynamics,2018-01-01,51(2018-05-06)
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