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Demonstrates a novel method for estimating groundwater recharge in arid regions, implying significant reductions in uncertainty.
Groundwater recharge estimation in arid regions is challenged by data scarcity and high uncertainty. This study presents a Physics-Informed Bayesian Neural Network (PI-BNN) to quantify groundwater recharge and its uncertainty in the South Al Batinah (SAB) Basin, northern Oman. The PI-BNN was applied within a soil-moisture mass balance framework using 34 years (1990–2023) of monthly FLDAS remote sensing data, embedding the water balance equation directly into the training loss function through nine physics-informed penalty terms. Results were compared against Latin Hypercube Sampling (LHS) using the same inputs. Recharge is highly seasonal and episodic, peaking in December (~5–6 mm/month) with moderate values in February–March and July, and negligible recharge during dry months. Annual recharge is estimated at approximately 16 mm/yr (PI-BNN) and 7–11 mm/yr (LHS). Precipitation variability accounts for more than 70% of recharge uncertainty during wet months. The PI-BNN reduces uncertainty bounds by approximately 50% compared to independent LHS while maintaining physically consistent estimates. An ablation experiment confirms that the physics-informed constraints, rather than the Bayesian architecture alone, drive physically plausible recharge recovery. The proposed methodology offers a robust and transferable framework for recharge estimation in data-scarce arid environments.
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Khan et al. (2026) studied this question.
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