Archivio Istituzionale della RicercaThis study explores how the partial contributing area effect due to snow accumulation, on the one hand, and the basin runoff coefficient, on the other hand, shape the flood frequency curve in high elevation areas. To this end, the geomorphoclimatic model FloodAlp is used. The influence of the parametrization of the basin’s hypsometric features within the model is widely investigated and the runoff coefficients for more than 100 gauged basins in north-western Italy are calibrated.
Taratura del modello FloodAlp su bacini dell'arco alpino nord-occidentale / Demateis Raveri, Marco; Evangelista, Giulia; Monforte, Irene. - In: L'ACQUA. - ISSN 1125-1255. - ELETTRONICO. - 4:(2023), pp. 99-108.
Taratura del modello FloodAlp su bacini dell'arco alpino nord-occidentale
Demateis Raveri, Marco;Evangelista, Giulia;Monforte, Irene
2023
Abstract
This study explores how the partial contributing area effect due to snow accumulation, on the one hand, and the basin runoff coefficient, on the other hand, shape the flood frequency curve in high elevation areas. To this end, the geomorphoclimatic model FloodAlp is used. The influence of the parametrization of the basin’s hypsometric features within the model is widely investigated and the runoff coefficients for more than 100 gauged basins in north-western Italy are calibrated.
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https://hdl.handle.net/11583/2981044