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

J Environ Manage

State Key Laboratory of Tibetan Plateau Earth System, Environment and Resources (TPESER), Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China; The University of Chinese Academy of Sciences, Beijing 100101, China.

Published: September 2024

AI Article Synopsis

  • Understanding water resource vulnerability (WRV) in mountain regions is essential for managing water resources and socio-economic development, especially under climate change impacts.
  • The study applied a comprehensive assessment framework to the Nujiang-Salween River basin, assessing various factors such as sensitivity, exposure, adaptability, and water stress.
  • Findings revealed that downstream areas experience higher WRV due to human activities, with the most vulnerable elevations found between 500-1500 meters, and indicated that climate change will increasingly impact WRV in the future.

Article Abstract

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 high-mountain 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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Source
http://dx.doi.org/10.1016/j.jenvman.2024.121954DOI Listing

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