Flash Flood Risk Assessment in Arid Regions

Summary

Flash floods in arid regions arise from intense, short-duration rainfall over low-infiltration catchments, often resulting in rapid runoff through networked wadis and ephemeral channels. Risk assessment combines geomorphological analysis, hydrological and hydraulic modelling, remote sensing and field measurements to delineate hazard zones, predict flood magnitudes and velocities, and evaluate exposure of infrastructure and communities. Digital elevation models and morphometric parameters characterise basin shape, slope and drainage density, informing the spatial distribution of runoff pathways. Hydrological models translate rainfall inputs into runoff volumes and peak discharges, while hydraulic simulations estimate inundation extents and depths. Integration of socio-economic factors and stakeholder knowledge supports vulnerability mapping and the design of early warning systems. Recent advances emphasise transferable workflows for data-scarce environments, coupling satellite-derived topography and land-cover data with open-source and commercial modelling platforms. Practical applications include urban planning guidelines, infrastructure resilience measures such as embankments and retention basins, and community engagement strategies for timely response. This multidisciplinary approach underpins global efforts to mitigate flash flood impacts in water-limited landscapes.

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Flash Flood Risk Assessment in Arid Regions publication trend

The graph below shows the total number of articles in flash flood risk assessment in arid regions across all publications each year (not limited to Nature Index journals).

Technical terms

Digital Elevation Model (DEM): A gridded representation of terrain elevation used to derive catchment geometry and flow pathways.

Geographic Information System (GIS): Software environment for integrating spatial datasets such as topography, land cover and hydrography.

Hydrological modelling: Simulation of rainfall–runoff processes to predict runoff volumes and peak discharges in catchments.

Hydraulic modelling: Computation of water flow dynamics to estimate flood depths, velocities and inundation extents.

Morphometric analysis: Quantitative assessment of basin form and drainage network parameters such as slope, shape and density.

Return period: Statistical average interval between events of a given magnitude, expressed in years.

HEC-HMS: A hydrologic modelling system developed by the US Army Corps of Engineers for rainfall–runoff simulation.

HEC-RAS: A hydraulic modelling tool by the US Army Corps of Engineers for river flow and floodplain inundation analysis.

References

  1. Flash flood prediction in Southwest Saudi Arabia using GIS technique and surface water models. Applied Water Science (2024).
  2. Vulnerability assessment of flash floods in Wadi Dahab Basin, Egypt. Environmental Earth Sciences (2020).
  3. Flash Flood Hazard Using Optical, Radar, and Stereo-Pair Derived DEM: Eastern Desert, Egypt. Remote Sensing (2018).
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