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Geographica Helvetica
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Volume 71, issue 3
Geogr. Helv., 71, 173-187, 2016
https://doi.org/10.5194/gh-71-173-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
Geogr. Helv., 71, 173-187, 2016
https://doi.org/10.5194/gh-71-173-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Standard article 17 Aug 2016

Standard article | 17 Aug 2016

Last Glacial Maximum precipitation pattern in the Alps inferred from glacier modelling

Patrick Becker, Julien Seguinot, Guillaume Jouvet, and Martin Funk Patrick Becker et al.
  • Versuchsanstalt für Wasserbau, Hydrologie und Glaziologie, ETH Zürich, 8093 Zürich, Switzerland

Abstract. During the Last Glacial Maximum (LGM), glaciers in the Alps reached a maximum extent, and broad sections of the foreland were covered by ice. In this study, we simulated the alpine ice cap using a glacier flow model to constrain the prevailing precipitation pattern with a geomorphological reconstruction of ice extent. For this purpose we forced the model using different temperature cooling and precipitation reduction factors. The use of the present-day precipitation pattern led to a systematic overestimation of the ice cover on the northern part of the Alps relative to the southern part. To reproduce the LGM ice cap, a more severe decrease in precipitation in the north than in the south was required. This result supports a southwesterly advection of atmospheric moisture to the Alps, sustained by a southward shift of the North Atlantic storm track during the LGM.

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