Articles | Volume 12, issue 8
https://doi.org/10.5194/tc-12-2515-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-12-2515-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
07 Aug 2018
Research article |
| 07 Aug 2018
| 07 Aug 2018
Numerical reconstructions of the flow and basal conditions of the Rhine glacier, European Central Alps, at the Last Glacial Maximum
Department of Earth and Environmental Science, New Mexico Tech,
Socorro, NM, USA
Fabien Gillet-Chaulet
Univ. Grenoble Alpes, CNRS, IRD, Grenoble INP, IGE, Grenoble,
France
Wilfried Haeberli
Department of Geography, University of Zurich, Zurich, Switzerland
Horst Machguth
Department of Geography, University of Zurich, Zurich, Switzerland
Department of Geosciences, University of Fribourg, Fribourg, Switzerland
Urs H. Fischer
Nagra, Wettingen, Switzerland
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- The interplay of Malm carbonate permeability, gravity-driven groundwater flow, and paleoclimate – implications for the geothermal field and potential in the Molasse Basin (southern Germany), a foreland-basin play T. Schintgen & I. Moeck 10.1186/s40517-021-00207-x
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- Sediment yield over glacial cycles: A conceptual model G. Antoniazza & S. Lane 10.1177/0309133321997292
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- Climatic patterns over the European Alps during the LGM derived from inversion of the paleo-ice extent V. Višnjević et al. 10.1016/j.epsl.2020.116185
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22 citations as recorded by crossref.
- Subglacial hydrology from high-resolution ice-flow simulations of the Rhine Glacier during the Last Glacial Maximum: a proxy for glacial erosion D. Cohen et al. 10.5194/egqsj-72-189-2023
- Modelling a paleo valley glacier network using a hybrid model: an assessment with a Stokes ice flow model M. Imhof et al. 10.1017/jog.2019.77
- Evaluating post-glacial bedrock erosion and surface exposure duration by coupling in situ optically stimulated luminescence and 10Be dating B. Lehmann et al. 10.5194/esurf-7-633-2019
- Timing and flow pattern of the Orta Glacier (European Alps) during the Last Glacial Maximum J. Braakhekke et al. 10.1111/bor.12427
- Microsedimentology of tills near Ainet, Austria - were palaeo-ice streams in the European Alps underlain by soft deforming bed zones? J. Reitner & J. Menzies 10.17738/ajes.2020.0005
- Glacial trimlines to identify former ice margins and subglacial thermal boundaries: A review and classification scheme for trimline expression C. Rootes & C. Clark 10.1016/j.earscirev.2020.103355
- Mendrisio, Château‐d'Oex and Sargans geological maps of Switzerland: free online data viewer and downloads D. Nowell 10.1111/gto.12403
- Drilling into a deep buried valley (ICDP DOVE): a 252 m long sediment succession from a glacial overdeepening in northwestern Switzerland S. Schaller et al. 10.5194/sd-32-27-2023
- Modelling last glacial cycle ice dynamics in the Alps J. Seguinot et al. 10.5194/tc-12-3265-2018
- Glacial to periglacial transition at the end of the last ice age in the subtropical semiarid Andes J. García et al. 10.1016/j.geomorph.2024.109379
- Coupled climate-glacier modelling of the last glaciation in the Alps G. Jouvet et al. 10.1017/jog.2023.74
- Reconstructing basal ice flow patterns of the Last Glacial Maximum Rhine glacier (northern Alpine foreland) based on streamlined subglacial landforms S. Kamleitner et al. 10.1002/esp.5733
- Hydromechanical Impacts of Pleistocene Glaciations on Pore Fluid Pressure Evolution, Rock Failure, and Brine Migration Within Sedimentary Basins and the Crystalline Basement Y. Zhang et al. 10.1029/2017WR022464
- Deep learning speeds up ice flow modelling by several orders of magnitude G. Jouvet et al. 10.1017/jog.2021.120
- A data-consistent model of the last glaciation in the Alps achieved with physics-driven AI T. Leger et al. 10.1038/s41467-025-56168-3
- Glacial Erosion Rates Determined at Vorab Glacier: Implications for the Evolution of Limestone Plateaus O. Steinemann et al. 10.3390/geosciences11090356
- Speleothem growth and stable carbon isotopes as proxies of the presence and thermodynamical state of glaciers compared to modelled glacier evolution in the Alps V. Skiba et al. 10.1016/j.quascirev.2023.108403
- The interplay of Malm carbonate permeability, gravity-driven groundwater flow, and paleoclimate – implications for the geothermal field and potential in the Molasse Basin (southern Germany), a foreland-basin play T. Schintgen & I. Moeck 10.1186/s40517-021-00207-x
- Last Glacial Maximum glacier fluctuations on the northern Alpine foreland: Geomorphological and chronological reconstructions from the Rhine and Reuss glacier systems S. Kamleitner et al. 10.1016/j.geomorph.2022.108548
- Sediment yield over glacial cycles: A conceptual model G. Antoniazza & S. Lane 10.1177/0309133321997292
- Modelling alpine glacier geometry and subglacial erosion patterns in response to contrasting climatic forcing F. Magrani et al. 10.1002/esp.5302
- Climatic patterns over the European Alps during the LGM derived from inversion of the paleo-ice extent V. Višnjević et al. 10.1016/j.epsl.2020.116185
1 citations as recorded by crossref.
Latest update: 03 May 2025
Short summary
As part of an integrative study about the safety of repositories for radioactive waste under ice age conditions in Switzerland, we modeled the flow of ice of the Rhine glacier at the Last Glacial Maximum to determine conditions at the ice–bed interface. Results indicate that portions of the ice lobes were at the melting temperature and ice was sliding, two conditions necessary for erosion by glacier. Conditions at the bed of the ice lobes were affected by climate and also by topography.
As part of an integrative study about the safety of repositories for radioactive waste under ice...
