On the Linkage between the Extreme Drought and Pluvial Patterns in China and the Large-Scale Atmospheric Circulation

被引:11
|
作者
Zhang, Zengxin [1 ,2 ]
Jin, Qiu [1 ]
Chen, Xi [3 ]
Xu, Chong-Yu [4 ,5 ]
Jiang, Shanshan [1 ]
机构
[1] Nanjing Forestry Univ, Coll Biol & Environm, Joint Innovat Ctr Modern Forestry Studies, Nanjing 210037, Jiangsu, Peoples R China
[2] State Ocean Adm, Inst 2, State Key Lab Satellite Ocean Environm Dynam, Hangzhou 310012, Zhejiang, Peoples R China
[3] Hohai Univ, State Key Lab Hydrol Water Resources & Hydraul En, Nanjing 210098, Jiangsu, Peoples R China
[4] Wuhan Univ, State Key Lab ofWater Resources & Hydropower Engn, Wuhan 430072, Peoples R China
[5] Univ Oslo, Dept Geosci, N-0316 Oslo, Norway
基金
中国国家自然科学基金;
关键词
EMPIRICAL ORTHOGONAL FUNCTIONS; SUMMER MONSOON; ASIAN MONSOON; 20TH-CENTURY DROUGHT; INDIAN MONSOON; YANGTZE-RIVER; PRECIPITATION; FLOODS; ANOMALIES; MOISTURE;
D O I
10.1155/2016/8010638
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
China is a nation that is affected by a multitude of natural disasters, including droughts and floods. In this paper, the variations of extreme drought and pluvial patterns and their relations to the large-scale atmospheric circulation have been analyzed based on monthly precipitation data from 483 stations during the period 1958-2010 in China. The results show the following: (1) the extreme drought and pluvial events in China increase significantly during that period. During 1959-1966 timeframe, more droughts occur in South China and more pluvial events are found in North China (DSC-PNC pattern); as for the period 1997-2003 (PSC-DNC pattern), the situation is the opposite. (2) There are good relationships among the extreme drought and pluvial events and the Western Pacific Subtropical High, meridional atmospheric moisture flux, atmospheric moisture content, and summer precipitation. (3) A cyclone atmospheric circulation anomaly occurs in North China, followed by an obvious negative height anomaly and a southern wind anomaly at 850 hPa and 500 hPa for the DSC-PNC pattern during the summer, and a massive ascending airflow from South China extends to North China at similar to 50 degrees N. As for the PSC-DNC pattern, the situation contrasts sharply with the DSC-PNC pattern.
引用
收藏
页数:12
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