Surface-water flow and early-warning models
Can physically based surface-water models improve early warning of hydrological hazards?
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About
Last updated: August 2026
About
Surface-water flow links rainfall, topography, river networks, floods, and water availability. Early-warning systems often need to make predictions with incomplete observations and limited computational time. A physically based model can help interpret measurements, assess uncertainty, and anticipate the evolution of hazards.
This project will develop thin-shell approximations for surface-water flow and use observations to calibrate and evaluate early-warning models. It can address catchment-scale floods, inundation, water movement across complex terrain, or the connection between surface water and groundwater.
Research questions
- When do thin-shell flow models provide a useful approximation for catchment-scale water movement?
- Which observations improve model calibration and early warning most effectively?
- How can uncertainty in rainfall, topography, and model parameters be communicated in a prediction?
Methods and data
Projects can use topography, rainfall products, stream gauges, satellite observations, numerical flow models, data assimilation, and uncertainty quantification.
Possible projects
Possible directions include deriving and testing a thin-shell model, evaluating an early-warning workflow for a selected catchment, or coupling surface-water and groundwater models.
Essential background
Useful preparation includes hydrology, fluid mechanics, Earth science, engineering, mathematics, programming, or data analysis.