Quantifying future water resource vulnerability in a high-mountain third pole river basin under climate change

被引:0
|
作者
Chai, Chenhao [1 ,2 ]
Wang, Lei [1 ,3 ]
Chen, Deliang [4 ]
Zhou, Jing [1 ]
Li, Ning [1 ]
Liu, Hu [1 ,3 ]
机构
[1] Chinese Acad Sci, Inst Tibetan Plateau Res, State Key Lab Tibetan Plateau Earth Syst Environm, Beijing 100101, Peoples R China
[2] Henan Polytech Univ, Sch Surveying & Land Informat Engn, Jiaozuo 454003, Peoples R China
[3] Univ Chinese Acad Sci, Beijing 100101, Peoples R China
[4] Univ Gothenburg, Dept Earth Sci, S-40530 Gothenburg, Sweden
基金
中国国家自然科学基金;
关键词
Water resources vulnerability; Third pole; Climate change; Nujiang-salween river; SPATIOTEMPORAL ANALYSIS; INTEGRATED MODEL; SCARCITY;
D O I
10.1016/j.jenvman.2024.121954
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Understanding the water resource vulnerability (WRV) in global mountain regions under climate change is crucial for water resources management and socio-economic development. However, the WRV in the highmountain Third Pole region (with quite a few transboundary river basins) remains largely unclear. Here, we have applied a comprehensive assessment framework of WRV to a Third Pole high-mountain river basin (Nujiang-Salween River, NSR) and its dependent downstream. The framework consisted of sensitivity, exposure, adaptability, hazard, and water stress indices, considering climate change, socio-economics, government effectiveness, natural disasters, and water supply capacity of the target river basin. Our results indicate that the downstream area (with intensive human activities) often exhibited significantly higher WRV than the mountain region; while the WRV shows an M-shaped change with increasing elevation, with the highest vulnerability occurring in a relatively low elevation range (e.g., 500-1500 m for the NSR basin). In the near future, we find that the spatial pattern of WRV in the basin is alternately influenced by adaptation, water scarcity, and exposure; whereas climate change serves as the main driver affecting the WRV in the far future. These findings enhance our understanding of the WRV in high-mountain transboundary basins of the Third Pole under global change.
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页数:13
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