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Updated: May 30, 2025

Watershed Planning within a Quantitative Scenario Analysis Framework
Published on: July 24, 2016
Assessing river discharge dynamics through relative surface water extent changes in river basins.
Feng Mao1, Margaret Shanafield2, Val Ouellet3
1Institute for Global Sustainable Development, School for Cross-faculty Studies, University of Warwick, Coventry CV4 7AL, UK.
Changes in river surface water extent effectively monitor river discharge, offering a simple method for ungauged basins. This approach reveals distinct relationships between water extent and river flow in hilly versus flat terrains.
Area of Science:
- Hydrology
- Remote Sensing
- Water Resource Management
Background:
- River discharge monitoring is crucial but limited by sparse stream gauging data.
- Existing remote sensing methods for river discharge often involve complex processing.
- There is a need for accessible methods to understand river flow dynamics.
Purpose of the Study:
- To introduce a simple, effective, and robust methodology for understanding river discharge.
- To assess the relationship between surface water extent and river discharge dynamics.
- To apply the methodology to Australian rivers as a case study.
Main Methods:
- Utilizing changes in relative surface water extent within river basins.
- Analyzing Australian river basins with varying topography (hilly and flat).
- Developing a novel approach to estimate river discharge from satellite-derived water extent.
Main Results:
- Relative surface water extent effectively captures river discharge dynamics.
- A linear relationship was found between surface water extent and discharge in hilly basins.
- A quadratic relationship was observed between surface water extent and discharge in flat basins.
Conclusions:
- The new methodology provides a simple yet robust way to monitor river flows, especially in ungauged basins.
- The findings highlight the potential of surface water extent as a proxy for river discharge.
- This approach can enhance regional and local understanding of water dynamics.
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