Not all that flows in creeks is water. Debris flows i.e., surges in which solid particles move together with little water, may occur in steep mountain streams, mainly as a consequence of intense rainfall. Debris flows have a high kinetic energy, and may cause major damage if they encroach buildings, roads and bridges. They are also a primary cause of landslide casualties. The video below shows an example of debris flows.
The low frequency of debris flows (most of the affected streams experience less than one event per year) does not attenuate the hazard, and makes the observation of debris flows particularly difficult. Hence, the experimental measurement of debris flows in adequately equipped monitoring sites is of utmost importance.
Since the early 1990s, we monitor debris-flows in Alpine catchments. The first instrumented catchment was the Moscardo Torrent (Udine), which was followed by the Marderello Torrent (Torino) and the Gadria Creek (Bolzano). In this last site, managed by the Departments of Hydraulic Works and Civil Protection of the Autonomous Province of Bozen-Bolzano, we cooperate with other scientists for the execution of survey campaigns and data analysis.
F. Comiti F, Marchi L, Macconi P, Arattano M, Bertoldi G, Borga M, Brardinoni F, Cavalli M, D’Agostino V, Penna D, Theule J. 2014. A new monitoring station for debris flows in the European Alps: first observations in the Gadria basin. Natural Hazards 73(3), 1175-1198. DOI:10.1007/s11069-014-1088-5.
Marchi L, Arattano M, Deganutti AM. 2002. Ten years of debris-flow monitoring in the Moscardo Torrent (Italian Alps). Geomorphology 46(1-2), 1-17. DOI:10.1016/S0169-555X(01)00162-3.
