Meteorological Drought Monitoring in Northeastern China Using Multiple Indices

被引:19
|
作者
Li, Fengping [1 ,2 ]
Li, Hongyan [1 ]
Lu, Wenxi [1 ]
Zhang, Guangxin [3 ]
Kim, Joo-Cheol [4 ]
机构
[1] Jilin Univ, Coll New Energy & Environm, Minist Educ, Key Lab Groundwater Resources & Environm, Changchun 130021, Jilin, Peoples R China
[2] Hohai Univ, State Key Lab Hydrol Water Resources & Hydraul En, Nanjing 210098, Jiangsu, Peoples R China
[3] Chinese Acad Sci, Northeast Inst Geog & Agroecol, Changchun 130102, Jilin, Peoples R China
[4] Chungnam Natl Univ, Int Water Resources Res Inst, Daejeon 34134, South Korea
基金
中国国家自然科学基金;
关键词
precipitation-based drought indices (DIs); Standardized Precipitation Index (SPI); Effective Drought Index (EDI); Z-Score; Wuyuer River Basin; STANDARDIZED PRECIPITATION INDEX; SONGHUA RIVER-BASIN; AGRICULTURAL DROUGHT; CALIFORNIA DROUGHT; SONGNEN PLAIN; EVENTS; WATER; QUANTIFICATION; TEMPERATURE; VARIABILITY;
D O I
10.3390/w11010072
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Drought monitoring is one of the significant issues of water resources assessment. Multiple drought indices (DIs), including Percent of Normal (PN), Standardized Precipitation Index (SPI), statistical Z-Score, and Effective Drought Index (EDI) at 18 different timesteps were employed to evaluate the drought condition in Wuyuer River Basin (WRB), Northeast China. Daily precipitation data of 50 years (1960-2010) from three meteorological stations were used in this study. We found DIs with intermediate time steps (7 to 18 months) to have the highest predictive values for identifying droughts. And DIs exhibited a better similarity in the 12-month timestep. Among all the DIs, EDI exhibited the best correlation with other DIs for various timesteps. When further comparing with historical droughts, Z-Score, SPI, and EDI were found more sensitive to multi-monthly cumulative precipitation changes (r(2) > 0.55) with respect to monthly precipitation changes (r(2) 0.10), while EDI was more preferable when only monthly precipitation data were available. These results indicated that various indices for different timesteps should be investigated in drought monitoring in WRB, especially the intermediate timesteps should be considered.
引用
收藏
页数:17
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