
NAME:
SOWI - Aula
BUILDING:
SOWI
FLOOR:
0
TYPE:
Assembly Hall
CAPACITY:
450
ACCESS:
Only Participants
EQUIPMENT:
Beamer, PC, WLAN (Eduroam), Overhead, Flipchart, Blackboard, Sound System, Handicapped Accessible, Microphones, Light Installation
We have analyzed a number of digital elevation models (DEMs) and orthophotos to reconstruct the pre-event behavior of Birchglacier, the volumes that were involved in the catastrophic collapse, as well as the dynamics of the runout of the rock-ice avalanche. The analysis of the pre-event DEMs shows the unusual behavior of the Birchglacier in the years prior to the event. Between 2011 and 2025, Birchglacier advanced by several tens of meters, thinning up-stream and thickening at the terminus. It is critical to understand how this behavior may have influenced the 2025 collapse.
We also compared pre- and post event DEMs to estimate the volumes, the deposited and eroded amount of material that was involved in the event. From orthophotos we mapped deposit structures that can help reconstruct the dynamics of the event, offering valuable information to calibrate numerical models.

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