Giovanni Ravazzani, Diego Curti, Marco Mancini, Renzo Rosso
Thursday 2 july 2015
11:45 - 12:00h at Oceania Foyer (level 0)
Themes: (T) Water resources and hydro informatics (WRHI), (ST) Surface and subsurface flow interactions
Parallel session: 11L. Water resources - Flow interactions
The contribution of groundwater to streamflow in Alpine catchments is still poorly understood, despite it may heavily impact hydrological balance and stream habitats. This work presents the results of a field campaign based on heat tracer methods to assess the hyphoreic flow during low flow period of a large Alpine river in Italy. These measurements were employed to validate a distributed hydrological model that can be used to asses river-groundwater interaction in both low and high flow conditions. The results show that groundwater may have a relevant role during low flow period by increasing river discharge and during floods by subtracting direct runoff that is stored in river banks.