Catchment modeling evaluates erosion susceptibility in Northern Italy, suggesting effective approaches for assessment.
This study focuses on three catchments located in the Oltrepò Pavese area of Northern Italy, a hilly landscape characterized by steep slopes, clay-marl lithologies, and extensive agricultural and viticultural land use. The region is prone to rainfall-induced soil erosion, making it an ideal setting to compare erosion modeling approaches. We evaluate the complementary use of the empirical Revised Universal Soil Loss Equation (RUSLE), which provides long-term average erosion estimates, and a two-dimensional Rain-on-Grid (RoG) hydrodynamic model, which simulates event-based runoff dynamics and sediment transport capacity. These models were applied using harmonized inputs to assess their spatial agreement in identifying erosion-prone areas and compared with erosion inventory zones mapped after a major storm in 2009. Despite operating at different temporal scales, the two approaches showed over 50% spatial overlap in detecting erosion-prone areas, particularly on steep slopes with concentrated runoff. RoG reproduced the mapped 2009 erosion zones more effectively than RUSLE, highlighting the dominant role of short-duration, high-intensity runoff-driven processes, while RUSLE better captured land-cover effects. Because validation is based on a single event with a different return period and includes processes not simulated by RoG, results should be interpreted as spatial-pattern agreement rather than quantitative predictive performance. The integrated use of both models offers a practical and transferable framework for data-scarce catchments. • RUSLE and RoG-based approaches showed significant overlap in erosion-prone areas. • RUSLE provides long-term trends, while RoG-based approach captures event-based dynamics. • RoG-based approach improves erosion assessment in data-scarce regions. • Integrating both approaches enhances erosion-prone hotspots prediction.
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Ravazzolo et al. (2026) studied this question.
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