Last Glacial Maximum precipitation pattern in the Alps inferred from glacier modelling
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 reconstruc...
| Published in: | Geographica Helvetica |
|---|---|
| Main Authors: | , , , |
| Format: | Article in Journal/Newspaper |
| Language: | German English French Italian |
| Published: |
Copernicus Publications
2016
|
| Subjects: | |
| Online Access: | https://doi.org/10.5194/gh-71-173-2016 http://www.geogr-helv.net/71/173/2016/gh-71-173-2016.pdf https://doaj.org/article/82954dc7be964f30b5bfbbc6285258e5 |
| Summary: | 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. |
|---|