The Characteristics and Evaluation of Future Droughts across China through the CMIP6 Multi-Model Ensemble

被引:33
|
作者
Ma, Zice [1 ]
Sun, Peng [1 ]
Zhang, Qiang [2 ,3 ]
Zou, Yifan [1 ]
Lv, Yinfeng [1 ]
Li, Hu [1 ]
Chen, Donghua [1 ]
机构
[1] Anhui Normal Univ, Sch Geog & Tourism, Wuhu 241002, Peoples R China
[2] Beijing Normal Univ, Acad Disaster Reduct & Emergency Management, Fac Geog Sci, Beijing 100875, Peoples R China
[3] Beijing Normal Univ, Key Lab Environm Change & Nat Disaster, Minist Educ, Beijing 100875, Peoples R China
基金
中国国家自然科学基金;
关键词
drought assessment; drought characteristics; standardized precipitation evapotranspiration index; CMIP6; models; SSP scenarios; China; PEARL RIVER-BASIN; METEOROLOGICAL DROUGHTS; CLIMATE; PRECIPITATION; FLOOD; TEMPERATURE;
D O I
10.3390/rs14051097
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Understanding historical and future drought patterns is crucial to acclimation and the mitigation of drought. The negative impact of China's droughts on the social economy has attracted attention; however, there is still no comprehensive or long-term monitoring pattern for future droughts. Here we evaluated the precipitation and temperature simulation capability of Coupled Model Intercomparison Project Phase 6 (CMIP6) and evaluated the temporal and spatial pattern of droughts during 1961-2099 across China. The results show that the multi-model ensemble mean (MME) is more representative of the observed precipitation and temperatures across China than the single climate model. China experienced an overall drying trend in the historical period. After 1991, the drought frequency (DF), drought duration (DD), and drought intensity (DI) in the northwest of the Inland River Basin and in the Yangtze River Basin increased significantly. Compared with the historical period, China will suffer more frequent drought events, although the DD and DI will be weakened under SSP1-2.6 and SSP2-4.5, while China will experience longer DD and more serious drought events under SSP3-7.0 and SSP5-8.5. The Hai River Basin and Huai River Basin are expected to have more serious drought trends in summer. Compared with historical periods, the drought trend will increase by 2.9-5.7 times and 1.1-4.2 times, respectively. The results can be used for decision making regarding future drought control.
引用
收藏
页数:23
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