Simulation of the Antarctic Ice Sheet over last glacial cycle with the coupled solid Earth – ice sheet model PISM-VILMA

The Antarctic Ice Sheet is the largest but also the most uncertain potential contributor to future sea level rise. Understanding involved feedback mechanisms require physically-based models. Confidence in future projections can be improved by models that reproduce past ice sheet changes and present...

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Main Authors: Albrecht, T., Bagge, M., Winkelmann, R., Klemann, V.
Format: Conference Object
Language:English
Published: 2023
Subjects:
Online Access:https://gfzpublic.gfz-potsdam.de/pubman/item/item_5020303
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spelling ftgfzpotsdam:oai:gfzpublic.gfz-potsdam.de:item_5020303 2024-01-14T10:02:21+01:00 Simulation of the Antarctic Ice Sheet over last glacial cycle with the coupled solid Earth – ice sheet model PISM-VILMA Albrecht, T. Bagge, M. Winkelmann, R. Klemann, V. 2023-07-11 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5020303 eng eng info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-3617 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5020303 XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG) info:eu-repo/semantics/conferenceObject 2023 ftgfzpotsdam https://doi.org/10.57757/IUGG23-3617 2023-12-18T00:44:24Z The Antarctic Ice Sheet is the largest but also the most uncertain potential contributor to future sea level rise. Understanding involved feedback mechanisms require physically-based models. Confidence in future projections can be improved by models that reproduce past ice sheet changes and present change rates. The complex interaction between ice, bedrock and sea level plays an important role for the stability of marine ice sheets with characteristic response time scales varying regionally between years and thousands of years due to the heterogeneous Earth structure underneath Antarctica and the interacting ice sheet dynamics.We have coupled the VIscoelastic Lithosphere and MAntle model (VILMA) to the Parallel Ice Sheet Model (PISM v2.0, www.pism.io) and have run simulations over the last two glacial cycles. In this framework, VILMA considers both, viscoelastic deformations of the solid Earth by considering a three-dimensional mantle-viscosity distribution and a gravitationally self-consistent mass redistribution in the ocean by solving for the sea-level equation. PISM solves for the stress balance for a changing bed topography, which can be updated with coupling intervals up to 1 year in view of fast changes in ice sheet flow and grounding line dynamics.Here, we show results of coupled PISM-VILMA simulations scored against a database of geological constraints around Antarctica (AntICE2), including sea level index points and GPS uplift rates. We discuss the implications of a three-dimensional Earth structure over one-dimensional profiles for Antarctic ice sheet changes. This project is part of the German Climate Modeling Initiative PalMod. Conference Object Antarc* Antarctic Antarctica Ice Sheet GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam) Antarctic The Antarctic
institution Open Polar
collection GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam)
op_collection_id ftgfzpotsdam
language English
description The Antarctic Ice Sheet is the largest but also the most uncertain potential contributor to future sea level rise. Understanding involved feedback mechanisms require physically-based models. Confidence in future projections can be improved by models that reproduce past ice sheet changes and present change rates. The complex interaction between ice, bedrock and sea level plays an important role for the stability of marine ice sheets with characteristic response time scales varying regionally between years and thousands of years due to the heterogeneous Earth structure underneath Antarctica and the interacting ice sheet dynamics.We have coupled the VIscoelastic Lithosphere and MAntle model (VILMA) to the Parallel Ice Sheet Model (PISM v2.0, www.pism.io) and have run simulations over the last two glacial cycles. In this framework, VILMA considers both, viscoelastic deformations of the solid Earth by considering a three-dimensional mantle-viscosity distribution and a gravitationally self-consistent mass redistribution in the ocean by solving for the sea-level equation. PISM solves for the stress balance for a changing bed topography, which can be updated with coupling intervals up to 1 year in view of fast changes in ice sheet flow and grounding line dynamics.Here, we show results of coupled PISM-VILMA simulations scored against a database of geological constraints around Antarctica (AntICE2), including sea level index points and GPS uplift rates. We discuss the implications of a three-dimensional Earth structure over one-dimensional profiles for Antarctic ice sheet changes. This project is part of the German Climate Modeling Initiative PalMod.
format Conference Object
author Albrecht, T.
Bagge, M.
Winkelmann, R.
Klemann, V.
spellingShingle Albrecht, T.
Bagge, M.
Winkelmann, R.
Klemann, V.
Simulation of the Antarctic Ice Sheet over last glacial cycle with the coupled solid Earth – ice sheet model PISM-VILMA
author_facet Albrecht, T.
Bagge, M.
Winkelmann, R.
Klemann, V.
author_sort Albrecht, T.
title Simulation of the Antarctic Ice Sheet over last glacial cycle with the coupled solid Earth – ice sheet model PISM-VILMA
title_short Simulation of the Antarctic Ice Sheet over last glacial cycle with the coupled solid Earth – ice sheet model PISM-VILMA
title_full Simulation of the Antarctic Ice Sheet over last glacial cycle with the coupled solid Earth – ice sheet model PISM-VILMA
title_fullStr Simulation of the Antarctic Ice Sheet over last glacial cycle with the coupled solid Earth – ice sheet model PISM-VILMA
title_full_unstemmed Simulation of the Antarctic Ice Sheet over last glacial cycle with the coupled solid Earth – ice sheet model PISM-VILMA
title_sort simulation of the antarctic ice sheet over last glacial cycle with the coupled solid earth – ice sheet model pism-vilma
publishDate 2023
url https://gfzpublic.gfz-potsdam.de/pubman/item/item_5020303
geographic Antarctic
The Antarctic
geographic_facet Antarctic
The Antarctic
genre Antarc*
Antarctic
Antarctica
Ice Sheet
genre_facet Antarc*
Antarctic
Antarctica
Ice Sheet
op_source XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
op_relation info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-3617
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5020303
op_doi https://doi.org/10.57757/IUGG23-3617
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