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Updated: Oct 6, 2025

Watershed Planning within a Quantitative Scenario Analysis Framework
Published on: July 24, 2016
Application of Entropy Method to Quantify Future Ecological Flow in the Yellow River Basin
Xinru Wang1, Huijuan Cui1,2
1Key Laboratory of Land Surface Patterns and Simulation, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China.
Climate change may increase future water flow in the Yellow River basin, potentially meeting ecological flow needs. However, some stations face continued water stress, impacting ecosystem sustainability.
Area of Science:
- Hydrology
- Climate Science
- Environmental Science
Background:
- Yellow River basin faces decreased precipitation and runoff due to anthropogenic and climate change impacts.
- Sustaining human and ecosystem needs is increasingly pressured by water scarcity.
Purpose of the Study:
- To evaluate future flow conditions in the Yellow River basin and assess their adequacy for ecological flow requirements.
- To analyze the impact of climate change on the Yellow River's ecological flow using hydrological modeling.
Main Methods:
- Applied an entropy-based method to calculate flow duration curves (FDCs) from observed and simulated data.
- Utilized H08 and DBH hydrological models for climate change impact assessment.
- Analyzed decadal FDCs under RCP 2.6 and RCP 8.5 climate change scenarios.
Main Results:
- Simulated FDCs showed good agreement with observed data and each other.
- Future decadal FDCs are predicted to be higher, indicating increased water availability under both RCP scenarios.
- High flows are projected to increase faster than low flows, with Q95 and Q90 values generally exceeding ecological thresholds at most stations.
Conclusions:
- Most Yellow River stations are projected to meet future ecological flow requirements, with minimal threat at Lanzhou, Wubao, Longmen, and Huayuankou.
- Toudaoguai, Sanmanxia, and Tangnaihai stations may still face challenges in satisfying ecological flow demands, indicating localized water stress.
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