CGCM projections of heavy rainfall events in China

被引:110
作者
Chen, Huopo [1 ,2 ,3 ]
Sun, Jianqi [1 ,2 ]
Chen, Xiaoli [4 ]
Zhou, Wen [5 ]
机构
[1] Chinese Acad Sci, Inst Atmospher Phys, Nansen Zhu Int Res Ctr NZC, Beijing 100029, Peoples R China
[2] Chinese Acad Sci, CCRC, Beijing 100029, Peoples R China
[3] Chinese Acad Sci, Grad Univ, Beijing 100029, Peoples R China
[4] Minist Environm Protect, Environm Dev Ctr, Beijing, Peoples R China
[5] City Univ Hong Kong, Sch Energy & Environm, Hong Kong, Hong Kong, Peoples R China
基金
中国国家自然科学基金;
关键词
projection; heavy rainfall; China; water vapour transportation; atmosphere stratification; ASIAN SUMMER MONSOON; DAILY PRECIPITATION; EXTREME PRECIPITATION; VARIABILITY; CLIMATE; TEMPERATURE; OSCILLATION; CIRCULATION; INSTABILITY; SIMULATION;
D O I
10.1002/joc.2278
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
This paper discusses projections of heavy rainfall events in China during the 21st century based on daily precipitation data from the Fourth Assessment Report's (AR4) Coupled General Circulation Models (CGCM). Results show that all three experimental scenarios (scenarios A2, A1B, and B1) project consistent changes in frequency and intensity of heavy rainfall at the end of 21st century. In the regions of Northeast China and North China, there are no significant changes in frequency but there are remarkable increases in intensity of heavy rainfall, indicating that enhanced intensity is the main contributor to increased ratios of heavy rainfall to total annual precipitation in these regions. In regions of the lower reaches of Yangtze River and South China, increases in the amount of heavy rainfall are closely associated with increased frequency and increased intensity. Projected frequencies of heavy rainfall at the end of 21st century increase by 30.9 similar to 56.6% in the Yangtze River and 35.9 similar to 50.2% in South China compared to the period of 19801999, and projected intensities increase by 1.0 similar to 5.7% and 2.8 similar to 6.3%, respectively. Additionally, the ratios of heavy rainfall to total annual precipitation increase by 2.3 similar to 5.4% in the Yangtze River and 1.8 similar to 3.8% in South China. The significant increases of heavy rainfall ratios indicate that as the climate warms, heavy rainfall events are expected to increase at rates that are much faster than increases in total precipitation amounts, indicating that China will experience increased amounts of flooding. These results are substantially consistent among the three IPCC (Intergovernmental Panel on Climate Change) scenarios.
引用
收藏
页码:441 / 450
页数:10
相关论文
共 39 条
[31]  
Wang HJ, 2001, ADV ATMOS SCI, V18, P376
[32]  
WANG HJ, 1993, SCI CHINA SER B, V36, P451
[33]   Variability of Northeast China River Break-up Date [J].
Wang Huijun ;
Sun Jianqi .
ADVANCES IN ATMOSPHERIC SCIENCES, 2009, 26 (04) :701-706
[34]   Downscaling and projection of winter extreme daily precipitation over North America [J].
Wang, Jiafeng ;
Zhang, Xuebin .
JOURNAL OF CLIMATE, 2008, 21 (05) :923-937
[35]   Mid-Holocene East Asian summer climate as simulated by the PMIP2 models [J].
Wang Tao ;
Wang Huijun ;
Jiang Dabang .
PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY, 2010, 288 (1-4) :93-102
[36]   Response of the ocean, climate and terrestrial carbon cycle to Holocene freshwater discharge after 8 kyr BP [J].
Wang, Y ;
Mysak, LA .
GEOPHYSICAL RESEARCH LETTERS, 2005, 32 (15) :1-4
[37]   Changes of climate extremes in China [J].
Zhai, PM ;
Sun, AJ ;
Ren, FM ;
Liu, XN ;
Gao, B ;
Zhang, Q .
CLIMATIC CHANGE, 1999, 42 (01) :203-218
[38]   A future climate scenario of regional changes in extreme climate events over China using the PRECIS climate model [J].
Zhang, Yong ;
Xu, Yinlong ;
Dong, Wenjie ;
Cao, Lijuan ;
Sparrow, Michael .
GEOPHYSICAL RESEARCH LETTERS, 2006, 33 (24)
[39]   Recent changes in the summer precipitation pattern in East China and the background circulation [J].
Zhu, Yali ;
Wang, Huijun ;
Zhou, Wen ;
Ma, Jiehua .
CLIMATE DYNAMICS, 2011, 36 (7-8) :1463-1473