Debris-Flow Monitoring and Geomorphic Change Detection Combining Laser Scanning and Fast Photogrammetric Surveys in the Moscardo Catchment (Eastern Italian Alps)

摘要

Monitoring debris-flow prone catchments and collecting field data is of extreme importance for improving the knowledge and therefore the management of such hazardous phenomena. High resolution Digital Elevation Models (DEMs) have recently established as an important tool for the study of geo-hydrological and geomorphological processes.udMonitoring surface changes over time allows to analyze sediment dynamics from several points of view, ranging from the accounting of volumetric changes to nu-merical modeling, to the correlation of morphometric indexes with different com-ponents of geo-hydrological processes. The present study examines the Moscardo Torrent, a small alpine stream in the Eastern Italian Alps which is characterized by a high occurrence of debris-flows.udThe original monitoring instrumentation, which made it possible to record hydro-graphs of 15 debris-flow events in the years 1989-1998, was renewed, allowing to record three debris-flows in the years 2011-2012.udSurface morphology of three areas exposed to debris-flow dynamics was sur-veyed across the recorded debris-flow events by means of Terrestrial Laser Scan-ning (TLS), and 0.2 m DEMs of Differences (DoDs) were calculated. During the third TLS campaign, close range digital photogrammetric images were acquired in order to directly compare 3d surface representation with the high–resolution DEMs derived by TLS