In August 2011, a large rainstorm event triggered several slope type debris flows on the steep LIA moraine deposits of the Gepatschferner. Since there are high resolution Ground-based LIDAR data available before and after the event, erosion and accumulation of the single debris flows could be quantified very accurately. Beside the quantification of the sediment yield of this event, the DEM of difference calculated from the two LiDAR epochs allows for the identification and detailed mapping of process areas of the debris flows. Using the ground-based LIDAR DEM and the mapped starting zones of the event, the process areas of the debris flows were modelled using a 2D friction model. The model was calibrated and validated by the detailed maps o...
In-situ measurements of debris-flow properties are crucial for understanding their movement mechanis...
The Flims rockslide, located in the eastern Swiss Alps, is the largest postglacial landslide in Euro...
The description and quantification of landscape changes as modulated by geomorphic processes, at dif...
The future development of debris flow processes regarding frequency and magnitude in terms of climat...
A methodology of magnitude estimates for debris flow events is described using airborne LiDAR data. ...
More detailed field measurements are required for a better understanding of surging debris flows. In...
In the year 2007, enhanced rockfall activity was observed within the scarp of a 500 BP rockslide in ...
This study describes an example of analysis of morphological changes by using high resolution DEMs d...
Mathematical modelling is a common approach when\ud assessing debris-flow hazards. In this study on ...
On 4th November 2010, a debris flow detached from a large debris cover accumulated above the lowermo...
The frequency of debris flow events caused by severe rainstorms has increased in Korea. LiDAR provid...
On 4 August 2015, a very high intensity storm, 31.5 mm in 20 min (94.5 mm/h), hit the massif of Moun...
An active landslide in Doren, Austria, has been studied by multitemporal airborne and terrestrial la...
Four occurred events of debris flows are documented and modeled by back-analysis. The four debris fl...
The geomorphological change detection through the comparison of repeated topographic surveys is a re...
In-situ measurements of debris-flow properties are crucial for understanding their movement mechanis...
The Flims rockslide, located in the eastern Swiss Alps, is the largest postglacial landslide in Euro...
The description and quantification of landscape changes as modulated by geomorphic processes, at dif...
The future development of debris flow processes regarding frequency and magnitude in terms of climat...
A methodology of magnitude estimates for debris flow events is described using airborne LiDAR data. ...
More detailed field measurements are required for a better understanding of surging debris flows. In...
In the year 2007, enhanced rockfall activity was observed within the scarp of a 500 BP rockslide in ...
This study describes an example of analysis of morphological changes by using high resolution DEMs d...
Mathematical modelling is a common approach when\ud assessing debris-flow hazards. In this study on ...
On 4th November 2010, a debris flow detached from a large debris cover accumulated above the lowermo...
The frequency of debris flow events caused by severe rainstorms has increased in Korea. LiDAR provid...
On 4 August 2015, a very high intensity storm, 31.5 mm in 20 min (94.5 mm/h), hit the massif of Moun...
An active landslide in Doren, Austria, has been studied by multitemporal airborne and terrestrial la...
Four occurred events of debris flows are documented and modeled by back-analysis. The four debris fl...
The geomorphological change detection through the comparison of repeated topographic surveys is a re...
In-situ measurements of debris-flow properties are crucial for understanding their movement mechanis...
The Flims rockslide, located in the eastern Swiss Alps, is the largest postglacial landslide in Euro...
The description and quantification of landscape changes as modulated by geomorphic processes, at dif...