Ice sheet – solid earth feedback during the last glacial cycle in Antarctica and Greenland ...

<!--!introduction!--> The solid earth influences ice sheet dynamics by controlling bedrock deformation and hence surface elevation and grounding line position. These in turn determine surface and basal melt. Ice-sheet models typically include models to compute bedrock deformation with a consta...

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Main Authors: van Calcar, Caroline, Van Der Wal, Wouter, Kempenaar, Gydo, Barletta, Valentina, van de Wal, Roderik
Format: Conference Object
Language:English
Published: GFZ German Research Centre for Geosciences 2023
Subjects:
Online Access:https://dx.doi.org/10.57757/iugg23-3121
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5020579
id ftdatacite:10.57757/iugg23-3121
record_format openpolar
spelling ftdatacite:10.57757/iugg23-3121 2023-07-23T04:15:23+02:00 Ice sheet – solid earth feedback during the last glacial cycle in Antarctica and Greenland ... van Calcar, Caroline Van Der Wal, Wouter Kempenaar, Gydo Barletta, Valentina van de Wal, Roderik 2023 https://dx.doi.org/10.57757/iugg23-3121 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5020579 en eng GFZ German Research Centre for Geosciences Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Article ConferencePaper Oral 2023 ftdatacite https://doi.org/10.57757/iugg23-3121 2023-07-03T22:13:54Z <!--!introduction!--> The solid earth influences ice sheet dynamics by controlling bedrock deformation and hence surface elevation and grounding line position. These in turn determine surface and basal melt. Ice-sheet models typically include models to compute bedrock deformation with a constant mantle viscosity (or similar parameter), whereas mantle viscosity can vary strongly underneath the ice sheets. Here we use a recently developed model that couples an ice-sheet model (ANICE) to a finite-element based GIA model that includes 3D variations in viscosity derived from seismic measurements. We investigate the effect of mantle viscosity variations on the evolution of the last glacial ice sheets in Antarctica and Greenland. In Antarctica, the main feedback mechanism is the effect of bedrock elevation on local sea level and grounding line position. In particular, uplifting bedrock in marine ice sheets reduces ice sheet loss during deglaciation. Results show a grounding line position that is 500 km more ... : The 28th IUGG General Assembly (IUGG2023) (Berlin 2023) ... Conference Object Antarc* Antarctica Greenland Ice Sheet DataCite Metadata Store (German National Library of Science and Technology) Greenland
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
description <!--!introduction!--> The solid earth influences ice sheet dynamics by controlling bedrock deformation and hence surface elevation and grounding line position. These in turn determine surface and basal melt. Ice-sheet models typically include models to compute bedrock deformation with a constant mantle viscosity (or similar parameter), whereas mantle viscosity can vary strongly underneath the ice sheets. Here we use a recently developed model that couples an ice-sheet model (ANICE) to a finite-element based GIA model that includes 3D variations in viscosity derived from seismic measurements. We investigate the effect of mantle viscosity variations on the evolution of the last glacial ice sheets in Antarctica and Greenland. In Antarctica, the main feedback mechanism is the effect of bedrock elevation on local sea level and grounding line position. In particular, uplifting bedrock in marine ice sheets reduces ice sheet loss during deglaciation. Results show a grounding line position that is 500 km more ... : The 28th IUGG General Assembly (IUGG2023) (Berlin 2023) ...
format Conference Object
author van Calcar, Caroline
Van Der Wal, Wouter
Kempenaar, Gydo
Barletta, Valentina
van de Wal, Roderik
spellingShingle van Calcar, Caroline
Van Der Wal, Wouter
Kempenaar, Gydo
Barletta, Valentina
van de Wal, Roderik
Ice sheet – solid earth feedback during the last glacial cycle in Antarctica and Greenland ...
author_facet van Calcar, Caroline
Van Der Wal, Wouter
Kempenaar, Gydo
Barletta, Valentina
van de Wal, Roderik
author_sort van Calcar, Caroline
title Ice sheet – solid earth feedback during the last glacial cycle in Antarctica and Greenland ...
title_short Ice sheet – solid earth feedback during the last glacial cycle in Antarctica and Greenland ...
title_full Ice sheet – solid earth feedback during the last glacial cycle in Antarctica and Greenland ...
title_fullStr Ice sheet – solid earth feedback during the last glacial cycle in Antarctica and Greenland ...
title_full_unstemmed Ice sheet – solid earth feedback during the last glacial cycle in Antarctica and Greenland ...
title_sort ice sheet – solid earth feedback during the last glacial cycle in antarctica and greenland ...
publisher GFZ German Research Centre for Geosciences
publishDate 2023
url https://dx.doi.org/10.57757/iugg23-3121
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5020579
geographic Greenland
geographic_facet Greenland
genre Antarc*
Antarctica
Greenland
Ice Sheet
genre_facet Antarc*
Antarctica
Greenland
Ice Sheet
op_rights Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_doi https://doi.org/10.57757/iugg23-3121
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