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Earth Surface Dynamics An interactive open-access journal of the European Geosciences Union
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Volume 4, issue 1
Earth Surf. Dynam., 4, 159–174, 2016
https://doi.org/10.5194/esurf-4-159-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
Earth Surf. Dynam., 4, 159–174, 2016
https://doi.org/10.5194/esurf-4-159-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 02 Feb 2016

Research article | 02 Feb 2016

Basal shear stress under alpine glaciers: insights from experiments using the iSOSIA and Elmer/Ice models

C. F. Brædstrup et al.

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Adhikari, S., and Marshall, S. J.: Influence of high-order mechanics on simulation of glacier response to climate change: insights from Haig Glacier, Canadian Rocky Mountains, The Cryosphere, 7, 1527–1541, https://doi.org/10.5194/tc-7-1527-2013, 2013.
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Anderson, R. S., Molnar, P., and Kessler, M. A.: Features of glacial valley profiles simply explained, J. Geophys. Res.-Earth, 111, F01004, https://doi.org/10.1029/2005JF000344, 2006.
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Short summary
When studying long-term glacial landscape evolution one must make simplifying assumptions about the nature of glacial flow. In this study we show that for two different numerical models such simplifications are mostly unimportant in the setting of glacial landscape evolution. Following this we find that glacial erosion is most intense in the early stages of glaciation and its effects are reduced with time due to flow patterns in the ice removing areas of highest resistance to flow.
When studying long-term glacial landscape evolution one must make simplifying assumptions about...
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