In: Swiss Journal of Geosciences, 2015, vol. 108, no. 2-3, p. 225-238
|
In: Geomorphology, 2020, vol. 350, p. 106913
De-glaciating high mountain areas result in new landscapes of bedrock and debris where permafrost can degrade, persist or even newly form in cases, and of new lakes in glacier bed overdeepenings (GBOs) becoming ice-free. These landscapes with new lakes in close neighborhood to over-steepened and perennially frozen slopes are prone to chain reaction processes (e.g. rock-ice avalanches into...
|
In: Geomorphology, 2020, vol. 355, p. 107068
Aosta Valley (Western Alps, Italy) is the region with the largest glacierized area of Italy. Like other high mountain regions, it has shown a significant glacier retreat starting from the end of the ‘Little Ice Age’ that is expected to continue in the future. As a direct consequence of glacier shrinkage, glacier-bed overdeepenings become exposed, offering suitable geomorphological ...
|
In: Swiss Journal of Geosciences, 2014, vol. 107, no. 2-3, p. 337-347
|
In: International Journal of Earth Sciences, 2014, vol. 103, no. 4, p. 1141-1161
|
In: Swiss Journal of Geosciences, 2014, vol. 107, no. 2-3, p. 309-336
|
In: The Cryosphere, 2018, vol. 12, no. 8, p. 2515–2544
At the Last Glacial Maximum (LGM), the Rhine glacier in the Swiss Alps covered an area of about 16000km2. As part of an integrative study about the safety of repositories for radioactive waste under ice age conditions in Switzerland, we modeled the Rhine glacier using a thermodynamically coupled three-dimensional, transient Stokes flow and heat transport model down to a horizontal resolution...
|
In: Bulletin of Volcanology, 2007, vol. 69, no. 6, p. 581-608
|
In: Swiss Journal of Geosciences, 2009, vol. 102, no. 1, p. 57-75
|
In: International Journal of Earth Sciences, 2011, vol. 100, no. 5, p. 1147-1162
|