Drought evolution, severity and trends in mainland China over 1961-2013

被引:254
作者
Yao, Ning [1 ,2 ]
Li, Yi [1 ,2 ]
Lei, Tianjie [3 ]
Peng, Lingling [1 ,2 ]
机构
[1] Northwest Agr & Forestry Univ, Coll Water Resources & Architectural Engn, Yangling 712100, Shaanxi, Peoples R China
[2] Northwest Agr & Forestry Univ, Inst Water Saving Agr Arid Areas China, Yangling 712100, Shaanxi, Peoples R China
[3] China Inst Water Resources & Hydropower Res IWHR, Beijing 100038, Peoples R China
基金
中国国家自然科学基金;
关键词
Drought index; Historical extreme drought event; Trend test; Timescale; REFERENCE CROP EVAPOTRANSPIRATION; POTENTIAL EVAPOTRANSPIRATION; ENERGY-BALANCE; TEMPORAL VARIATIONS; EVAPORATIVE DEMAND; SOIL-MOISTURE; ARIDITY INDEX; PRECIPITATION; CLIMATE; SENSITIVITY;
D O I
10.1016/j.scitotenv.2017.10.327
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Droughts have destructive impacts on crop yields and water supplies, and researching droughts is vital for societal stability and human life. This work aimed to assess the spatiotemporal evolution of droughts in mainland China over 1961-2013 using four drought indices. These indices were the percentage of precipitation anomaly (Pa), standard precipitation index (SPI), standard precipitation evapotranspiration index (SPEI) and evaporative demand drought index (EDDI) at multiple timescales ranging from 1-week to 24-month. The variations of the SPI, SPEI and EDDI were compared with historical severe or extreme droughts. The general increases of the Pa, SPI and SPEI, and general decrease of the EDDI, consistently implied an overall relief of drought conditions over 1961-2013. The different drought indices revealed historical drought conditions, including the national extreme droughts in 1961, 1965, 1972, 1978, 1986, 1988, 1992, 1994, 1997, 1999 and 2000, but various drought severity levels were classified for each drought event since the classification standards differed. Although the SPI and SPEI performed better than the EDDI and there were higher correlations between the SPI and the SPEI, all the indices were regional-or station-specific and have identified historical severe or extreme drought events. At shorter timescales, the EDDI revealed earlier onsets and ends of flash droughts, unlike those indicated by the SPI and SPEI. The comparison of the different indices based on the historical drought events confirmed the uses of the Pa, SPI and SPEI for determining continuous droughts and that of the EDDI for identifying flash droughts. (C) 2017 Elsevier B.V. All rights reserved.
引用
收藏
页码:73 / 89
页数:17
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