Spatio-temporal variations of precipitation extremes in Xinjiang, China

被引:135
|
作者
Zhang, Qiang [1 ,2 ]
Singh, Vijay P. [3 ,4 ]
Li, Jianfeng [1 ,2 ]
Jiang, Fengqing [5 ]
Bai, Yungang [6 ]
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 So China, Guangdong High Educ Inst, Guangzhou 510275, Guangdong, Peoples R China
[3] Texas A&M Univ, Dept Biol & Agr Engn, College Stn, TX 77843 USA
[4] Texas A&M Univ, Dept Civil & Environm Engn, College Stn, TX 77843 USA
[5] Chinese Acad Sci, Xinjiang Inst Ecol & Geog, Xinjiang 830011, Peoples R China
[6] Xinjiang Res Inst Water Resources & Hydropower, Xinjiang 830049, Peoples R China
基金
中国国家自然科学基金;
关键词
Extreme precipitation regimes; Joint distribution; Copula function; Arid and semi-arid regions; Xinjiang; PEARL RIVER-BASIN; CHANGING PROPERTIES; COPULA; TRENDS; DISTRIBUTIONS; VARIABILITY; EVENTS; MAXIMA; MODELS; FLOODS;
D O I
10.1016/j.jhydrol.2012.02.038
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
This study aims to study joint probabilities and changing characteristics of precipitation extremes, as well as the implications of these changes in Xinjiang. Daily rainfall data from 53 stations across Xinjiang. China, covering a period of 1957-2009 were collected. Using eight precipitation indices, probabilistic characteristics of precipitation extremes were analyzed based on Copulas. The K-S method was employed to select appropriate marginal probability distributions for determining quantiles, and the Akaike Information Criterion (AIC) was used to select copulas. Results indicate the following: (1) North Xinjiang is wetter than south Xinjiang; (2) More concurrent strong and weak precipitation extremes are observed in the areas along Tianshan Mountains, and in eastern parts of the Xinjiang than those in western parts of the Xinjiang; (3) After 1980, the Xinjiang region is exhibiting a wetting tendency, and the heavy precipitation extremes tend to occur more severely and frequently; and also the possibilities of concurrent strong and weak precipitation extremes altered in a distinct pattern; (4) Tianshan Mountains can be taken as the demarcation for the occurrences of floods and droughts and the risk of droughts and floods across the Xinjiang region is expected to increase. (C) 2012 Elsevier B.V. All rights reserved.
引用
收藏
页码:7 / 18
页数:12
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