The decadal variability and its cause of the extreme drought in China

被引:12
|
作者
Hou Wei [1 ,2 ]
Yang Ping [1 ,2 ]
Feng Guo-Lin [2 ,3 ]
机构
[1] Lanzhou Univ, Dept Atmospher & Sci, Lanzhou 730000, Peoples R China
[2] Chinese Acad Sci, Inst Atmospher Phys, Key Lab Reg Climate Environm Res Temp E Asia, Beijing 100029, Peoples R China
[3] China Meteorol Adm, Natl Climate Ctr, Lab Climate Studies, Beijing 100081, Peoples R China
关键词
drought; ice core; pacific decadal oscillation;
D O I
10.7498/aps.57.3932
中图分类号
O4 [物理学];
学科分类号
0702 ;
摘要
This paper investigates the probability of extreme drought in four regions of China during the 1470-2000 A. D., and analyzes the delta O-18 record in Guliya ice core. By wavelet analysis, we find that the probability of drought in the four regions has the quasi-cycle of 350 a, like the delta O-18 record in Guliya ice core. When the delta O-18 record is high, the temperature of Qinghai-Xizang Plateau is high too, and the probability of drought is low, and vice versa. This paper also analyzes the Pacific decadal oscillation and finds the quasi-cycle of 80 a is weakening but the quasi-cycle of 50a is enhancing. When either of them is strong, the probability of drought is high, and the probability is low when the two quasi-cycles are alternating.
引用
收藏
页码:3932 / 3940
页数:9
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