This study evaluates and compares two-dimensional (2D) numerical models of different complexities by testing them on a floodplain inundation event that occurred on the Secchia River (Italy). We test 2D capabilities of LISFLOOD-FP and HEC-RAS (5.0.3), implemented using various grid sizes (25–100 m) based on 1-m DEM resolution. As expected, the best results were shown by the higher-resolution grids (25 m) for both models, which is justified by the complex terrain of the area. However, the coarser resolution simulations (50 and 100 m) performed virtually identically compared to the high-resolution simulations. Nevertheless, the spatial distribution of flood characteristics varies: the 50 and 100 m results of LISFLOOD-FP and HEC-RAS misestimated flood extent and water depth in selected control areas (built-up zones). We suggest that the specific terrain of the area can cause ambiguities in large-scale modelling, while providing plausible results in terms of the overall model performance.

Shustikova I., Domeneghetti A., Neal J.C., Bates P., Castellarin A. (2019). Comparing 2D capabilities of HEC-RAS and LISFLOOD-FP on complex topography. HYDROLOGICAL SCIENCES JOURNAL, 64(14), 1769-1782 [10.1080/02626667.2019.1671982].

Comparing 2D capabilities of HEC-RAS and LISFLOOD-FP on complex topography

Shustikova I.
Membro del Collaboration Group
;
Domeneghetti A.
Membro del Collaboration Group
;
Castellarin A.
Membro del Collaboration Group
2019

Abstract

This study evaluates and compares two-dimensional (2D) numerical models of different complexities by testing them on a floodplain inundation event that occurred on the Secchia River (Italy). We test 2D capabilities of LISFLOOD-FP and HEC-RAS (5.0.3), implemented using various grid sizes (25–100 m) based on 1-m DEM resolution. As expected, the best results were shown by the higher-resolution grids (25 m) for both models, which is justified by the complex terrain of the area. However, the coarser resolution simulations (50 and 100 m) performed virtually identically compared to the high-resolution simulations. Nevertheless, the spatial distribution of flood characteristics varies: the 50 and 100 m results of LISFLOOD-FP and HEC-RAS misestimated flood extent and water depth in selected control areas (built-up zones). We suggest that the specific terrain of the area can cause ambiguities in large-scale modelling, while providing plausible results in terms of the overall model performance.
2019
Shustikova I., Domeneghetti A., Neal J.C., Bates P., Castellarin A. (2019). Comparing 2D capabilities of HEC-RAS and LISFLOOD-FP on complex topography. HYDROLOGICAL SCIENCES JOURNAL, 64(14), 1769-1782 [10.1080/02626667.2019.1671982].
Shustikova I.; Domeneghetti A.; Neal J.C.; Bates P.; Castellarin A.
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11585/711160
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