Spatiotemporal variations of precipitation regimes across Yangtze River Basin, China

被引:50
作者
Zhang, Qiang [1 ,2 ,3 ,4 ]
Peng, Juntai [1 ,2 ,3 ,4 ]
Xu, Chong-Yu [5 ]
Singh, Vijay P. [6 ,7 ]
机构
[1] Sun Yat Sen Univ, Dept Water Resources & Environm, Guangzhou 510275, Guangdong, Peoples R China
[2] Sun Yat Sen Univ, Key Lab Water Cycle & Water Secur Southern China, Guangdong High Educ Inst, Guangzhou 510275, Guangdong, Peoples R China
[3] Sun Yat Sen Univ, Sch Geog & Planning, Guangzhou 510275, Guangdong, Peoples R China
[4] Sun Yat Sen Univ, Guangdong Key Lab Urbanizat & Geosimulat, Guangzhou 510275, Guangdong, Peoples R China
[5] Univ Oslo, Dept Geosci, N-0316 Oslo, Norway
[6] Texas A&M Univ, Dept Biol & Agr Engn, College Stn, TX 77843 USA
[7] Texas A&M Univ, Dept Civil & Environm Engn, College Stn, TX 77843 USA
基金
中国国家自然科学基金;
关键词
EXTREMES; CLIMATE; INTENSIFICATION; FLOODS; SCALE; TREND;
D O I
10.1007/s00704-013-0916-y
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Daily precipitation data during the period of 1960 to 2005 from 147 rain gauging stations over the Yangtze River Basin are analyzed to investigate precipitation variations based on precipitation indices and also consecutive rainfall regimes in both space and time. Results indicate decreasing annual/monthly mean precipitation. Distinct decreases in rainfall days are observed over most parts of the Yangtze River Basin, but precipitation intensity is increasing over most parts of the Yangtze River Basin, particularly the lower Yangtze River Basin. Besides, durations of precipitation regimes are shortening; however, the fractional contribution of short-lasting precipitation regimes to the total precipitation amount is increasing. In this sense, the precipitation processes in the Yangtze River Basin are dominated by precipitation regimes of shorter durations. These results indicate intensified hydrological cycle reflected by shortening precipitation regimes. This finding is different from that in Europe where the intensifying precipitation changes are reflected mainly by lengthening precipitation regimes, implying different regional responses of hydrological cycle to climate changes. The results of this study will be of considerable relevance in basin-scale water resources management, human mitigation of natural hazards, and in understanding regional hydrological responses to changing climate at regional scales.
引用
收藏
页码:703 / 712
页数:10
相关论文
共 24 条
[1]   Atmospheric warming and the amplification of precipitation extremes [J].
Allan, Richard P. ;
Soden, Brian J. .
SCIENCE, 2008, 321 (5895) :1481-1484
[2]  
[Anonymous], 1975, J. Econ
[3]  
[Anonymous], 1966, 79 WMO
[4]   Intensification of extreme European summer precipitation in a warmer climate [J].
Christensen, OB ;
Christensen, JH .
GLOBAL AND PLANETARY CHANGE, 2004, 44 (1-4) :107-117
[5]   Global warming benefits the small in aquatic ecosystems [J].
Daufresne, Martin ;
Lengfellner, Kathrin ;
Sommer, Ulrich .
PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA, 2009, 106 (31) :12788-12793
[6]   Climate extremes: Observations, modeling, and impacts [J].
Easterling, DR ;
Meehl, GA ;
Parmesan, C ;
Changnon, SA ;
Karl, TR ;
Mearns, LO .
SCIENCE, 2000, 289 (5487) :2068-2074
[7]   A modified Mann-Kendall trend test for autocorrelated data [J].
Hamed, KH ;
Rao, AR .
JOURNAL OF HYDROLOGY, 1998, 204 (1-4) :182-196
[8]  
Kendall M., 1955, RANK CORRELATION MET
[9]   Trends in rainfall amount and number of rainy days in river basins of India (1951-2004) [J].
Kumar, Vijay ;
Jain, Sharad K. .
HYDROLOGY RESEARCH, 2011, 42 (04) :290-306
[10]   NONPARAMETRIC TESTS AGAINST TREND [J].
Mann, Henry B. .
ECONOMETRICA, 1945, 13 (03) :245-259