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...
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Online Access: | https://doi.org/10.5194/gh-71-173-2016 https://gh.copernicus.org/articles/71/173/2016/ |
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fttriple:oai:gotriple.eu:Ezb3upJQYaBgZYWqwuGma 2023-05-15T16:38:08+02:00 Last Glacial Maximum precipitation pattern in the Alps inferred from glacier modelling Becker, Patrick Seguinot, Julien Jouvet, Guillaume Funk, Martin 2018-01-15 https://doi.org/10.5194/gh-71-173-2016 https://gh.copernicus.org/articles/71/173/2016/ en eng Copernicus Publications doi:10.5194/gh-71-173-2016 10670/1.nz9v3r 0016-7312 2194-8798 https://gh.copernicus.org/articles/71/173/2016/ undefined Geographica Helvetica - geography eISSN: 2194-8798 geo envir Text https://vocabularies.coar-repositories.org/resource_types/c_18cf/ Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2018 fttriple https://doi.org/10.5194/gh-71-173-2016 2023-01-22T19:13:21Z 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. Article in Journal/Newspaper Ice cap North Atlantic Unknown Geographica Helvetica 71 3 173 187 |
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geo envir Becker, Patrick Seguinot, Julien Jouvet, Guillaume Funk, Martin Last Glacial Maximum precipitation pattern in the Alps inferred from glacier modelling |
topic_facet |
geo envir |
description |
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. |
format |
Article in Journal/Newspaper |
author |
Becker, Patrick Seguinot, Julien Jouvet, Guillaume Funk, Martin |
author_facet |
Becker, Patrick Seguinot, Julien Jouvet, Guillaume Funk, Martin |
author_sort |
Becker, Patrick |
title |
Last Glacial Maximum precipitation pattern in the Alps inferred from glacier modelling |
title_short |
Last Glacial Maximum precipitation pattern in the Alps inferred from glacier modelling |
title_full |
Last Glacial Maximum precipitation pattern in the Alps inferred from glacier modelling |
title_fullStr |
Last Glacial Maximum precipitation pattern in the Alps inferred from glacier modelling |
title_full_unstemmed |
Last Glacial Maximum precipitation pattern in the Alps inferred from glacier modelling |
title_sort |
last glacial maximum precipitation pattern in the alps inferred from glacier modelling |
publisher |
Copernicus Publications |
publishDate |
2018 |
url |
https://doi.org/10.5194/gh-71-173-2016 https://gh.copernicus.org/articles/71/173/2016/ |
genre |
Ice cap North Atlantic |
genre_facet |
Ice cap North Atlantic |
op_source |
Geographica Helvetica - geography eISSN: 2194-8798 |
op_relation |
doi:10.5194/gh-71-173-2016 10670/1.nz9v3r 0016-7312 2194-8798 https://gh.copernicus.org/articles/71/173/2016/ |
op_rights |
undefined |
op_doi |
https://doi.org/10.5194/gh-71-173-2016 |
container_title |
Geographica Helvetica |
container_volume |
71 |
container_issue |
3 |
container_start_page |
173 |
op_container_end_page |
187 |
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1766028420116905984 |