Drought evaluation using the GRACE terrestrial water storage deficit over the Yangtze River Basin, China

被引:144
|
作者
Sun, Zhangli [1 ,2 ,3 ,4 ]
Zhu, Xiufang [1 ,2 ,4 ]
Pan, Yaozhong [2 ,3 ,4 ]
Zhang, Jinshui [1 ,2 ,4 ]
Liu, Xianfeng [5 ]
机构
[1] Beijing Normal Univ, State Key Lab Earth Surface Proc & Resource Ecol, Beijing 100875, Peoples R China
[2] Beijing Normal Univ, Key Lab Environm Change & Nat Disaster, Minist Educ, Beijing 100875, Peoples R China
[3] Beijing Normal Univ & Inst Remote Sensing & Digit, State Key Lab Remote Sensing Sci, Beijing 100875, Peoples R China
[4] Beijing Normal Univ, Inst Remote Sensing Sci & Engn, Fac Geog Sci, Beijing 100875, Peoples R China
[5] Shaanxi Normal Univ, Sch Geog & Tourism, Xian 710119, Shaanxi, Peoples R China
关键词
Water storage deficit index; Standardized drought indices; Drought severity; GRACE CSR; DEPLETION; INDEXES; MODEL;
D O I
10.1016/j.scitotenv.2018.03.292
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Droughts are some of the worst natural disasters that bring significant water shortages, economic losses, and adverse social consequences. Gravity Recovery and Climate Experiment (GRACE) satellite data are widely used to characterize and evaluate droughts. In this work, we evaluate drought situations in the Yangtze River Basin (YRB) using the GRACE Texas Center for Space Research (CSR) mascon (mass concentration) data from 2003 to 2015. Drought events are identified by water storage deficits (WSDs) derived from GRACE data, while the drought severity evaluation is based on the water storage deficit index (WSDI), standardized WSD time series, and total water storage deficit (TWSD). The WSDI is subsequently compared with the Palmer drought severity index (PDSI), standardized precipitation index (SPI), standardized precipitation evapotranspiration index (SPEI), and standardized runoff index (SRI). The results indicate the YRB experienced increased wetness during the study period, with WSD values increasing at a rate of 5.20mm/year. Eight drought events are identified, and three major droughts occurred in 2004, 2006, and 2011, with WSDIs of -2.05,-2.38, andn-1.30 and TWSDs of -620.96 mm,-616.81 mm, and -192.44 mm, respectively. Our findings suggest that GRACE CSR mascon data can be used effectively to assess drought features in the YRB and that the WSDI facilitates robust and reliable characterization of droughts over large-scale areas. (C) 2018 Elsevier B.V. All rights reserved.
引用
收藏
页码:727 / 738
页数:12
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