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Updated: Jan 8, 2026

Watershed Planning within a Quantitative Scenario Analysis Framework
Published on: July 24, 2016
Climate-driven flood hazard assessment in data-scarce mountainous basins using a GIS-based machine learning and
Shahbaz Khan1, Afed Ullah Khan1,2, Abdullah Alodah3
1Department of Civil Engineering, University of Engineering and Technology Peshawar, Bannu Campus, 28100, Pakistan.
Abstract:
Floods pose increasing risks in mountainous regions such as the Swat River Basin, where climatic variability, glacial influences, and data limitations hinder conventional flood risk assessment. This study introduces a hybrid framework that integrates explainable SHapley Additive exPlanations (SHAP)-based XGBoost for Global Climate Model (GCM) ranking, Random Forest (RF) ensemble modeling, and coupled hydrologic-hydraulic simulations (HEC-HMS-HEC-RAS) for multi-scenario flood hazard mapping. The approach provides an interpretable, data-driven, and physically based method for assessing climate-induced flood hazards in data-scarce basins. Daily precipitation, maximum temperature (Tmax), and minimum temperature (Tmin) data from eleven CMIP6 (Coupled Model Intercomparison Project Phase 6) Global Climate Models (GCMs) were bias-corrected using the linear scaling approach. These GCMs were ranked using XGBoost regression with SHAP interpretation, achieving high predictive accuracy (R2: 0.934/0.926 for precipitation, 0.953/0.949 for Tmax, and 0.947/0.943 for Tmin). A Multi-Model Ensemble built with RF regression further improved performance (R2: 0.74/0.71 for precipitation; 0.97/0.963 for Tmax; 0.965/0.958 for Tmin). These datasets were used to drive the HEC-HMS model, calibrated (1993-2013) and validated (2014-2019) with satisfactory results (NSE: 0.612/0.603; PBIAS: + 3.96%/- 6.75%). Flood frequency analysis using distribution fitting and the VIKOR method identified Log-Logistic (historical), Gumbel (SSP245), and GEV (SSP585) as optimal models. Simulated hydrographs for different return periods were input into a 2D HEC-RAS model to estimate flood depth, extent, and velocity. Flood hazard was quantified using a composite index of depth and velocity. Under SSP585, high to very high hazard zones expanded to 78% of the floodplain for the 100-year event, compared to 69% under historical conditions. This integrated, explainable, and scalable framework enhances climate-driven flood hazard prediction in complex mountainous terrains.
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