Coupled climate-glacier modelling of the last glaciation in the Alps

Our limited knowledge of the climate prevailing over Europe during former glaciations is the main obstacle to reconstruct the past evolution of the ice coverage over the Alps by numerical modelling. To address this challenge, we perform a two-step modelling approach: First, a regional climate model...

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Published in:Journal of Glaciology
Main Authors: Guillaume Jouvet, Denis Cohen, Emmanuele Russo, Jonathan Buzan, Christoph C. Raible, Wilfried Haeberli, Sarah Kamleitner, Susan Ivy-Ochs, Michael A. Imhof, Jens K. Becker, Angela Landgraf, Urs H. Fischer
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press
Subjects:
Online Access:https://doi.org/10.1017/jog.2023.74
https://doaj.org/article/012a3edf744c4462aea7bc63582f3b11
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spelling ftdoajarticles:oai:doaj.org/article:012a3edf744c4462aea7bc63582f3b11 2023-11-05T03:42:43+01:00 Coupled climate-glacier modelling of the last glaciation in the Alps Guillaume Jouvet Denis Cohen Emmanuele Russo Jonathan Buzan Christoph C. Raible Wilfried Haeberli Sarah Kamleitner Susan Ivy-Ochs Michael A. Imhof Jens K. Becker Angela Landgraf Urs H. Fischer https://doi.org/10.1017/jog.2023.74 https://doaj.org/article/012a3edf744c4462aea7bc63582f3b11 EN eng Cambridge University Press https://www.cambridge.org/core/product/identifier/S0022143023000746/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2023.74 0022-1430 1727-5652 https://doaj.org/article/012a3edf744c4462aea7bc63582f3b11 Journal of Glaciology, Pp 1-15 glacier modelling moraine paleoclimate Environmental sciences GE1-350 Meteorology. Climatology QC851-999 article ftdoajarticles https://doi.org/10.1017/jog.2023.74 2023-10-08T00:36:00Z Our limited knowledge of the climate prevailing over Europe during former glaciations is the main obstacle to reconstruct the past evolution of the ice coverage over the Alps by numerical modelling. To address this challenge, we perform a two-step modelling approach: First, a regional climate model is used to downscale the time slice simulations of a global earth system model in high resolution, leading to climate snapshots during the Last Glacial Maximum (LGM) and the Marine Isotope Stage 4 (MIS4). Second, we combine these snapshots and a climate signal proxy to build a transient climate over the last glacial period and force the Parallel Ice Sheet Model to simulate the dynamical evolution of glaciers in the Alps. The results show that the extent of modelled glaciers during the LGM agrees with several independent key geological imprints, including moraine-based maximal reconstructed glacial extents, known ice transfluences and trajectories of erratic boulders of known origin and deposition. Our results highlight the benefit of multiphysical coupled climate and glacier transient modelling over simpler approaches to help reconstruct paleo glacier fluctuations in agreement with traces they have left on the landscape. Article in Journal/Newspaper Ice Sheet Journal of Glaciology Directory of Open Access Journals: DOAJ Articles Journal of Glaciology 1 15
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic glacier modelling
moraine
paleoclimate
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
spellingShingle glacier modelling
moraine
paleoclimate
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
Guillaume Jouvet
Denis Cohen
Emmanuele Russo
Jonathan Buzan
Christoph C. Raible
Wilfried Haeberli
Sarah Kamleitner
Susan Ivy-Ochs
Michael A. Imhof
Jens K. Becker
Angela Landgraf
Urs H. Fischer
Coupled climate-glacier modelling of the last glaciation in the Alps
topic_facet glacier modelling
moraine
paleoclimate
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
description Our limited knowledge of the climate prevailing over Europe during former glaciations is the main obstacle to reconstruct the past evolution of the ice coverage over the Alps by numerical modelling. To address this challenge, we perform a two-step modelling approach: First, a regional climate model is used to downscale the time slice simulations of a global earth system model in high resolution, leading to climate snapshots during the Last Glacial Maximum (LGM) and the Marine Isotope Stage 4 (MIS4). Second, we combine these snapshots and a climate signal proxy to build a transient climate over the last glacial period and force the Parallel Ice Sheet Model to simulate the dynamical evolution of glaciers in the Alps. The results show that the extent of modelled glaciers during the LGM agrees with several independent key geological imprints, including moraine-based maximal reconstructed glacial extents, known ice transfluences and trajectories of erratic boulders of known origin and deposition. Our results highlight the benefit of multiphysical coupled climate and glacier transient modelling over simpler approaches to help reconstruct paleo glacier fluctuations in agreement with traces they have left on the landscape.
format Article in Journal/Newspaper
author Guillaume Jouvet
Denis Cohen
Emmanuele Russo
Jonathan Buzan
Christoph C. Raible
Wilfried Haeberli
Sarah Kamleitner
Susan Ivy-Ochs
Michael A. Imhof
Jens K. Becker
Angela Landgraf
Urs H. Fischer
author_facet Guillaume Jouvet
Denis Cohen
Emmanuele Russo
Jonathan Buzan
Christoph C. Raible
Wilfried Haeberli
Sarah Kamleitner
Susan Ivy-Ochs
Michael A. Imhof
Jens K. Becker
Angela Landgraf
Urs H. Fischer
author_sort Guillaume Jouvet
title Coupled climate-glacier modelling of the last glaciation in the Alps
title_short Coupled climate-glacier modelling of the last glaciation in the Alps
title_full Coupled climate-glacier modelling of the last glaciation in the Alps
title_fullStr Coupled climate-glacier modelling of the last glaciation in the Alps
title_full_unstemmed Coupled climate-glacier modelling of the last glaciation in the Alps
title_sort coupled climate-glacier modelling of the last glaciation in the alps
publisher Cambridge University Press
url https://doi.org/10.1017/jog.2023.74
https://doaj.org/article/012a3edf744c4462aea7bc63582f3b11
genre Ice Sheet
Journal of Glaciology
genre_facet Ice Sheet
Journal of Glaciology
op_source Journal of Glaciology, Pp 1-15
op_relation https://www.cambridge.org/core/product/identifier/S0022143023000746/type/journal_article
https://doaj.org/toc/0022-1430
https://doaj.org/toc/1727-5652
doi:10.1017/jog.2023.74
0022-1430
1727-5652
https://doaj.org/article/012a3edf744c4462aea7bc63582f3b11
op_doi https://doi.org/10.1017/jog.2023.74
container_title Journal of Glaciology
container_start_page 1
op_container_end_page 15
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