Modified drought propagation under a changing environment: A case study in the Dongting Lake basin, China

被引:2
作者
Jin, Lina [1 ,2 ]
Peng, Tao [1 ,2 ]
Fan, Tianyi [3 ]
Singh, Vijay P. [4 ,5 ,6 ]
Lin, Qingxia [1 ,2 ]
Dong, Xiaohua [1 ,2 ]
Liu, Ji [1 ,2 ]
Guo, Jiali [1 ,2 ]
Yu, Dan [1 ,2 ]
Wang, Gaoxu [2 ,7 ]
机构
[1] Minist Educ, Hubei Prov Key Lab Construct & Management Hydropow, Yichang, Peoples R China
[2] Minist Educ, Engn Res Ctr Ecoenvironm Three Gorges Reservoir Re, Yichang, Peoples R China
[3] Hunan Prov Water Resources & Hydropower Survey Des, Changsha 410007, Peoples R China
[4] Texas A&M Univ, Dept Biol & Agr Engn, College Stn, TX 77843 USA
[5] Texas A&M Univ, Zachry Dept Civil & Environm Engn, College Stn, TX 77843 USA
[6] UAE Univ, Natl Water & Energy Ctr, Al Ain, U Arab Emirates
[7] Nanjing Hydraul Res Inst, State Key Lab Hydrol Water Resources & Hydraul Eng, Nanjing 210029, Peoples R China
基金
中国国家自然科学基金;
关键词
Meteorological drought; Hydrological drought; Environmental change; Drought propagation; Dongting Lake basin; HYDROLOGICAL DROUGHT; CLIMATE-CHANGE; YANGTZE-RIVER; MIDDLE REACHES; PRECIPITATION; RUNOFF; QUANTIFY; IMPACTS; TRENDS;
D O I
10.1016/j.ejrh.2024.101986
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
Study region: Four sub-basins of the Dongting Lake basin (DLB), China. Study focus: The "pre-post-disturbance" method was employed to assess the impact of environmental variation on propagation from meteorological drought (MD) to hydrological drought (HD) in the DLB. The study period was split into two sub-periods (i.e, the baseline and impacted periods) via breakpoints of annual runoff series. Additionally, we calculated the drought propagation characteristics in different periods using the run theory. Furthermore, based on copula function and conditional probability analysis, the transmission threshold of MD triggering HD was determined. New hydrological insights for the region: (i) Compared with the baseline period, the severity of HD in the Li River (LR) and Yuan River (YR) increased by 0.5 % and 1.3 % during the impacted period, respectively, while that in the Zi River (ZR) and Xiang River (XR) decreased by -25.9 % and -31.6 %, respectively; (ii) Human activities have weakened the correlation between HD and MD, resulting in various patterns of propagation time in different sub-basins and seasons; (iii) As a whole, propagation threshold from MD to HD became larger during the impacted period, with an average change rate from 0.9 % to 195.5 %.
引用
收藏
页数:17
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