Articles | Volume 12, issue 10
https://doi.org/10.5194/tc-12-3265-2018
© 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-12-3265-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Modelling last glacial cycle ice dynamics in the Alps
Julien Seguinot
CORRESPONDING AUTHOR
Laboratory of Hydraulics, Hydrology and Glaciology, ETH Zürich, Zurich, Switzerland
Arctic Research Center, Hokkaido University, Sapporo, Japan
Susan Ivy-Ochs
Laboratory of Ion Beam Physics, ETH Zürich, Zurich, Switzerland
Guillaume Jouvet
Laboratory of Hydraulics, Hydrology and Glaciology, ETH Zürich, Zurich, Switzerland
Matthias Huss
Laboratory of Hydraulics, Hydrology and Glaciology, ETH Zürich, Zurich, Switzerland
Martin Funk
Laboratory of Hydraulics, Hydrology and Glaciology, ETH Zürich, Zurich, Switzerland
Frank Preusser
Institute of Earth and Environmental Sciences, University of Freiburg, Freiburg, Germany
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Discussed (final revised paper)
Latest update: 20 Nov 2024
Short summary
About 25 000 years ago, Alpine glaciers filled most of the valleys and even extended onto the plains. In this study, with help from traces left by glaciers on the landscape, we use a computer model that contains knowledge of glacier physics based on modern observations of Greenland and Antarctica and laboratory experiments on ice, and one of the fastest computers in the world, to attempt a reconstruction of the evolution of Alpine glaciers through time from 120 000 years ago to today.
About 25 000 years ago, Alpine glaciers filled most of the valleys and even extended onto the...