A comparative frequency analysis of three standardized drought indices in the Poyang Lake basin, China

被引:11
|
作者
Yan, Guixia [1 ]
Wu, Zhiyong [2 ]
Li, Denghua [3 ]
Xiao, Heng [4 ]
机构
[1] Nanjing Univ Informat Sci & Technol, Coll Hydrometeorol, Nanjing, Jiangsu, Peoples R China
[2] Hohai Univ, State Key Lab Hydrol Water Resources & Hydraul En, Coll Hydrol & Water Resources, Nanjing, Jiangsu, Peoples R China
[3] Nanjing Hydraul Res Inst, State Key Lab Hydrol Water Resources & Hydraul En, Nanjing, Jiangsu, Peoples R China
[4] North China Univ Water Resources & Elect Power, Yellow River Inst Sci, Zhengzhou, Henan, Peoples R China
基金
中国国家自然科学基金;
关键词
Drought; Standardized drought index; Copulas; Return period; Poyang Lake basin; RIVER-BASIN; CLIMATE-CHANGE; YANGTZE-RIVER; PRECIPITATION; STREAMFLOW; CATCHMENT; TRENDS;
D O I
10.1007/s11069-017-3133-7
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Regional drought frequency analysis was carried out in the Poyang Lake basin (PLB) from 1960-2014 based on three standardized drought indices: the standardized precipitation index (SPI), the standardized precipitation evapotranspiration index (SPEI) and the standardized Palmer drought index (SPDI). Drought events and characteristics were extracted. A Gumbel-Hougaard (GH) copula was selected to construct the bivariate probability distribution of drought duration and severity, and the joint return periods (T (a) ) were calculated. Results showed that there were 50 (50 and 40) drought events in the past 55 years based on the SPI (SPEI and SPDI), and 9 (8 and 10) of them were severe with T (a) more than 10 years, occurred in the 1960s, the 1970s and the 2000s. Overall, the three drought indices could detect the onset of droughts and performed similarly with regard to drought identification. However, for the SPDI, moisture scarcity was less frequent, but it showed more severe droughts with substantially higher severity and longer duration droughts. The conditional return period (Ts|d) was calculated for the spring drought in 2011, and it was 66a and 54a, respectively, based on the SPI and SPDI, which was consistent with the record. Overall, the SPI, only considering the precipitation, can as effectively as the SPEI and SPDI identify the drought process over the PLB under the present changing climate. However, drought is affected by climate and land-cover changes; thus, it is necessary to integrate the results of drought frequency analysis based on different drought indices to improve the drought risk management.
引用
收藏
页码:353 / 374
页数:22
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