The strengthening East Asia summer monsoon since the early 1990s

被引:86
作者
Liu HaiWen [1 ,2 ,3 ]
Zhou TianJun [2 ]
Zhu YuXiang [4 ]
Lin YiHua [2 ]
机构
[1] Chengdu Univ Informat Technol, Coll Atmospher Sci, Plateau Atmosphere & Environm Key Lab Sichuan Pro, Chengdu 610225, Peoples R China
[2] Chinese Acad Sci, Inst Atmospher Phys, State Key Lab Numer Modeling Atmospher Sci & Geop, Beijing 100029, Peoples R China
[3] Chongqing Inst Meteorol Sci, Chongqing 401147, Peoples R China
[4] China Meteorol Adm Training Ctr, Beijing 100081, Peoples R China
来源
CHINESE SCIENCE BULLETIN | 2012年 / 57卷 / 13期
基金
中国国家自然科学基金;
关键词
East Asia summer monsoon; precipitation; interdecadal change; land-sea thermal contrast; NCEP-NCAR REANALYSIS; SEA-LEVEL PRESSURE; SURFACE-TEMPERATURE; CLIMATIC JUMP; RAINY-SEASON; NORTH CHINA; VARIABILITY; RAINFALL; CONTRAST; HEIGHT;
D O I
10.1007/s11434-012-4991-8
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Previous studies have documented a weakening tendency of the East Asian summer monsoon (EASM) since the end of the 1970s. In this study, we report that the EASM has been recovering since the early 1990s, although its strength is still less than in previous decades (averaged over the period 1965-1980). Following the recovery of the EASM, there has been a tendency in the last decade toward northward-moving rainbands and excessive rainfall in the Huaihe River valley (110A degrees-120A degrees E, 30A degrees-35A degrees N). There is evidence suggesting that the strengthening EASM since the early 1990s is linked to interdecadal change of land-sea thermal contrast.
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页码:1553 / 1558
页数:6
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