FastIsostasy.jl - Accelerated computation of glacial isostatic adjustment ...

<!--!introduction!--> Glacial isostatic adjustment (GIA) represents an important negative feedback on ice-sheet dynamics. The magnitude and time scale of GIA primarily depend on the upper mantle viscosity and the lithosphere thickness. These parameters have been found to vary strongly over the...

Full description

Bibliographic Details
Main Authors: Swierczek-Jereczek, Jan, Montoya, Marisa, Robinson, Alexander, Alvarez-Solas, Jorge
Format: Article in Journal/Newspaper
Language:unknown
Published: GFZ German Research Centre for Geosciences 2023
Subjects:
Online Access:https://dx.doi.org/10.57757/iugg23-0500
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5015941
id ftdatacite:10.57757/iugg23-0500
record_format openpolar
spelling ftdatacite:10.57757/iugg23-0500 2023-06-11T04:06:58+02:00 FastIsostasy.jl - Accelerated computation of glacial isostatic adjustment ... Swierczek-Jereczek, Jan Montoya, Marisa Robinson, Alexander Alvarez-Solas, Jorge 2023 https://dx.doi.org/10.57757/iugg23-0500 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5015941 unknown GFZ German Research Centre for Geosciences Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Oral ConferencePaper Article 2023 ftdatacite https://doi.org/10.57757/iugg23-0500 2023-05-02T10:12:30Z <!--!introduction!--> Glacial isostatic adjustment (GIA) represents an important negative feedback on ice-sheet dynamics. The magnitude and time scale of GIA primarily depend on the upper mantle viscosity and the lithosphere thickness. These parameters have been found to vary strongly over the Antarctic continent, showing ranges of 10^18 - 10^23 Pa s for the viscosity and 30 - 250 km for the lithospheric thickness. Recent studies show that capturing these spatial dependencies are of significant importance for the long-term evolution of the Antarctic Ice Sheet (AIS). However, 3D GIA models are computationally expensive and sometimes require an iterative coupling for the ice sheet and the solid-Earth solutions to converge. As a consequence, their use remains limited, potentially leading to errors in the simulated ice-sheet response and associated sea-level rise projections. Here, we propose to tackle this problem by generalising the work of Bueler et al. (2007) and Coulon et al. (2021). FastIsostasy ... : The 28th IUGG General Assembly (IUGG2023) (Berlin 2023) ... Article in Journal/Newspaper Antarc* Antarctic Ice Sheet DataCite Metadata Store (German National Library of Science and Technology) Antarctic The Antarctic
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language unknown
description <!--!introduction!--> Glacial isostatic adjustment (GIA) represents an important negative feedback on ice-sheet dynamics. The magnitude and time scale of GIA primarily depend on the upper mantle viscosity and the lithosphere thickness. These parameters have been found to vary strongly over the Antarctic continent, showing ranges of 10^18 - 10^23 Pa s for the viscosity and 30 - 250 km for the lithospheric thickness. Recent studies show that capturing these spatial dependencies are of significant importance for the long-term evolution of the Antarctic Ice Sheet (AIS). However, 3D GIA models are computationally expensive and sometimes require an iterative coupling for the ice sheet and the solid-Earth solutions to converge. As a consequence, their use remains limited, potentially leading to errors in the simulated ice-sheet response and associated sea-level rise projections. Here, we propose to tackle this problem by generalising the work of Bueler et al. (2007) and Coulon et al. (2021). FastIsostasy ... : The 28th IUGG General Assembly (IUGG2023) (Berlin 2023) ...
format Article in Journal/Newspaper
author Swierczek-Jereczek, Jan
Montoya, Marisa
Robinson, Alexander
Alvarez-Solas, Jorge
spellingShingle Swierczek-Jereczek, Jan
Montoya, Marisa
Robinson, Alexander
Alvarez-Solas, Jorge
FastIsostasy.jl - Accelerated computation of glacial isostatic adjustment ...
author_facet Swierczek-Jereczek, Jan
Montoya, Marisa
Robinson, Alexander
Alvarez-Solas, Jorge
author_sort Swierczek-Jereczek, Jan
title FastIsostasy.jl - Accelerated computation of glacial isostatic adjustment ...
title_short FastIsostasy.jl - Accelerated computation of glacial isostatic adjustment ...
title_full FastIsostasy.jl - Accelerated computation of glacial isostatic adjustment ...
title_fullStr FastIsostasy.jl - Accelerated computation of glacial isostatic adjustment ...
title_full_unstemmed FastIsostasy.jl - Accelerated computation of glacial isostatic adjustment ...
title_sort fastisostasy.jl - accelerated computation of glacial isostatic adjustment ...
publisher GFZ German Research Centre for Geosciences
publishDate 2023
url https://dx.doi.org/10.57757/iugg23-0500
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5015941
geographic Antarctic
The Antarctic
geographic_facet Antarctic
The Antarctic
genre Antarc*
Antarctic
Ice Sheet
genre_facet Antarc*
Antarctic
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/iugg23-0500
_version_ 1768379297403240448