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Updated: Jun 18, 2025

Watershed Planning within a Quantitative Scenario Analysis Framework
Published on: July 24, 2016
Quantifying future water resource vulnerability in a high-mountain third pole river basin under climate change.
Chenhao Chai1, Lei Wang2, Deliang Chen3
1State Key Laboratory of Tibetan Plateau Earth System, Environment and Resources (TPESER), Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China; School of Surveying and Land Information Engineering, Henan Polytechnic University, Jiaozuo 454003, China.
Water resource vulnerability (WRV) is high in the Third Pole's Nujiang-Salween River basin, especially downstream. WRV varies with elevation and is driven by adaptation and climate change.
Area of Science:
- Environmental science
- Hydrology
- Climate change studies
Background:
- Assessing water resource vulnerability (WRV) in global mountains is vital for management and development.
- The Third Pole region's high-mountain transboundary river basins have unclear WRV under climate change.
Purpose of the Study:
- To comprehensively assess WRV in the Nujiang-Salween River (NSR) basin, a Third Pole high-mountain river.
- To understand the spatial patterns and future drivers of WRV in this critical region.
Main Methods:
- Applied a framework including sensitivity, exposure, adaptability, hazard, and water stress indices.
- Considered climate change, socio-economics, government effectiveness, natural disasters, and water supply capacity.
- Analyzed WRV across elevation gradients and future timeframes.
Main Results:
- Downstream areas with intensive human activity show significantly higher WRV than mountain regions.
- WRV exhibits an M-shaped pattern with elevation, peaking between 500-1500m in the NSR basin.
- Near-future WRV is influenced by adaptation, water scarcity, and exposure; far-future WRV is primarily driven by climate change.
Conclusions:
- Downstream human activities and elevation significantly impact WRV in the Third Pole.
- Climate change is a key driver of future WRV, underscoring the need for adaptive strategies.
- Findings improve understanding of WRV in high-mountain transboundary basins under global change.
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