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- W101660498 abstract "Prediction of hydrologic response is particularly difficult in alpine regions where data are sparse and the spatial variability of both precipitation and physical controls on runoff generation is considerable. Moreover, alpine catchments are frequently affected by small scale flash floods, which are usually responsible for shallow landsliding and debris flow triggering. Therefore, improving the understanding of the rainfall-runoff processes occurring in these regions represents a relevant scientific topic for hydrologists and operators involved in hydro-geological risk mitigation. Studies undertook in small experimental areas where rainfall and discharge measures and additional hydrological variables are recorded, can address this issue. In this work, soil moisture and water table data are used along with the commonly used rainfall runoff and temperature variables in order to investigate the hydrologic behaviour of the Vauz creek basin (1.9 km) located in the central-eastern Italian Alps. Beside this, two micro subcatchments (Bridge Creek catchment and Larch Creek catchment, of area 0.11 and 0.032 km, respectively) were analyzed in order to investigate the influence of spatial and temporal dynamics of soil moisture and water table on runoff response at different scales. Soil water content and groundwater level have been continuously monitored in the snow-free period (from May to September) since summer 2005 with a sub-hourly time resolution." @default.
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- W101660498 date "2010-05-01" @default.
- W101660498 modified "2023-09-27" @default.
- W101660498 title "Use of soil moisture and water table data for rainfall-runoff modelling in alpine catchments" @default.
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