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Updated: May 29, 2025

Watershed Planning within a Quantitative Scenario Analysis Framework
Published on: July 24, 2016
Assessing climate sensitivity of the Upper Indus Basin using fully distributed, physically-based hydrologic modeling
Hamna Hasan1, Muhammad Zia Ur Rahman Hashmi2, Syed Imran Ahmed3
1Department of Civil Engineering, NED University of Engineering & Technology, Karachi, Pakistan. hamnahasan@neduet.edu.pk.
Climate change is projected to increase water resources in Pakistan's Upper Indus Basin due to greater snowmelt. This could alleviate water stress but also increase flood risks, necessitating improved water management and infrastructure.
Area of Science:
- Hydrology and Climate Science
- Water Resource Management
Background:
- The Upper Indus Basin (UIB) faces potential water scarcity due to climate change impacting snow and glacier melt.
- The region's water resources are critical for Pakistan's downstream areas.
Purpose of the Study:
- To investigate hydrological changes and water resource variability in the UIB under future climate scenarios.
- To project streamflow changes up to the end of the 21st century.
Main Methods:
- Utilized a coupled hydrologic/hydraulic model (MIKE SHE/MIKE HYDRO RIVER) calibrated with streamflow data.
- Employed bias-corrected climate projections from the coordinated regional climate downscaling experiment (CORDEX) for RCP 4.5 and RCP 8.5 scenarios.
Main Results:
- Projected streamflow increases of 86% (RCP 4.5) and 97% (RCP 8.5) by the end of the century.
- Warming trends (2.3-4°C) are expected to significantly boost snowmelt, particularly increasing winter flows by 300% historically.
- Annual average water availability under RCP 8.5 is estimated at 4500 m³/s.
Conclusions:
- Increased water availability may alleviate water stress but poses significant flood risks.
- Enhanced flood defenses and storage are crucial for managing increased water resources and mitigating flood hazards in downstream areas.
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