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...
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In: Computational Geosciences, 2006, vol. 10, no. 2, p. 161-178
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In: Earth Surface Processes and Landforms, 2016, vol. 41, no. 13, p. 1980–1990
Overdeepenings, i.e. closed topographic depressions with adverse slopes in the direction of flow, are characteristic for glacier beds and glacially sculpted landscapes. Quantitative information about their morphological characteristics, however, has so far hardly been available. The present study provides such information by combining the analysis of (a) numerous bed overdeepenings below...
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