Spatial and temporal variability of precipitation concentration index, concentration degree and concentration period in Xinjiang, China

被引:189
|
作者
Li, Xuemei [2 ]
Jiang, Fengqing [1 ]
Li, Lanhai [1 ]
Wang, Guigang [2 ]
机构
[1] Chinese Acad Sci, Xinjiang Inst Ecol & Geog, Key Lab Oasis Ecol & Desert Environm, Urumqi 830011, Xinjiang, Peoples R China
[2] Chinese Acad Sci, Grad Sch, Beijing 100049, Peoples R China
关键词
precipitation concentration index; precipitation concentration degree; precipitation concentration period; Mann-Kendall trend test; wavelet power spectrum analysis; Xinjiang; RIVER-BASIN; CLIMATE-CHANGE; DAILY RAINFALL; TRENDS; STREAMFLOW; MAXIMUM;
D O I
10.1002/joc.2181
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
This paper studied the spatial and temporal variability of the statistical structures of precipitation across Xinjiang, China, by analysing the time series of daily precipitation from 50 weather stations during the period from 1961 to 2008. Three indices precipitation concentration index (CI), precipitation concentration degree (PCD) and precipitation concentration period (PCP) were used to detect precipitation concentrations and the associated spatial patterns. The results show that higher precipitation CI values were mainly observed in Southern Xinjiang, whereas lower precipitation CI values were mostly detected in Northern Xinjiang. The precipitation CI values are noticeably larger in places where both annual total precipitation and number of rainy days are lower. The Mann-Kendall trend test demonstrates that the most parts of Xinjiang are characterized by no significant trends of precipitation CI at the 0.05 significance level. The periodicity characteristic of precipitation CI time series in Xinjiang could be detected by wavelet power spectrum analysis, and significant periods of that in most of Xinjiang were concentrated on 2-5 years band. The results of PCP reveal that rainfall in Xinjiang mostly occurs in summer, and the rainy season arrives earlier in Eastern Xinjiang than Western Xinjiang, whereas the results of PCD indicate that the rainfall in Northern Xinjiang was more dispersed within a year than that in Southern Xinjiang. Copyright (C) 2010 Royal Meteorological Society
引用
收藏
页码:1679 / 1693
页数:15
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