This paper deals with the use of time-series of High-Resolution Digital Elevation Models (HR DEMs)obtained from photogrammetry and airborne LiDAR coupled with aerial photos, to analyse the magnitude of recently reactivated large scale earth slides-earth flows located in the northern Apennines of Italy. The landslides underwent complete reactivation beetween 2001 and 2006, causing civil protection emergencies. With the final aim to support hazard assessment and the planning of mitigation measures, high-resolution DEMs are used to identify, quantify and visualize depletion and accumulation in the slope resulting from the reactivation of the mass movements. This information allows to quantify mass wasting, i.e. the amount of landslide material that is wasted during reactivation events due to stream erosion along the slope and at its bottom, resulting in sediment discharge into the local fluvial system, and to assess the total volumetric magnitude of the events. By quantifying and visualising elevation changes at the slope scale, results are also a valuable support for the comprehension of geomorphological process actiong behind the evolution of the analysed landslides.

Estimating mass-wasting processes in active earth slides – earth flows with time-series of High Resolution DEMs from photogrammetry and airborne LiDAR

Sterzai P.
2009-01-01

Abstract

This paper deals with the use of time-series of High-Resolution Digital Elevation Models (HR DEMs)obtained from photogrammetry and airborne LiDAR coupled with aerial photos, to analyse the magnitude of recently reactivated large scale earth slides-earth flows located in the northern Apennines of Italy. The landslides underwent complete reactivation beetween 2001 and 2006, causing civil protection emergencies. With the final aim to support hazard assessment and the planning of mitigation measures, high-resolution DEMs are used to identify, quantify and visualize depletion and accumulation in the slope resulting from the reactivation of the mass movements. This information allows to quantify mass wasting, i.e. the amount of landslide material that is wasted during reactivation events due to stream erosion along the slope and at its bottom, resulting in sediment discharge into the local fluvial system, and to assess the total volumetric magnitude of the events. By quantifying and visualising elevation changes at the slope scale, results are also a valuable support for the comprehension of geomorphological process actiong behind the evolution of the analysed landslides.
File in questo prodotto:
File Dimensione Formato  
20120321155736996.pdf

non disponibili

Tipologia: Altro materiale allegato
Licenza: Non specificato
Dimensione 899.81 kB
Formato Adobe PDF
899.81 kB Adobe PDF   Visualizza/Apri   Richiedi una copia

I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.

Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/20.500.14083/2731
 Attenzione

Attenzione! I dati visualizzati non sono stati sottoposti a validazione da parte dell'ateneo

Citazioni
  • ???jsp.display-item.citation.pmc??? ND
  • Scopus 78
  • ???jsp.display-item.citation.isi??? 70
social impact