Increasing numerical stability of mountain valley glacier simulations: implementation and testing of free-surface stabilization in Elmer/Ice

This paper concerns a numerical stabilization method for free-surface ice flow called the free-surface stabilization algorithm (FSSA). In the current study, the FSSA is implemented into the numerical ice-flow software Elmer/Ice and tested on synthetic two-dimensional (2D) glaciers, as well as on the...

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Main Authors: Löfgren, André, Zwinger, Thomas, Råback, Peter, Helanow, Christian, Ahlkrona, Josefin
Format: Text
Language:English
Published: 2023
Subjects:
Online Access:https://doi.org/10.5194/egusphere-2023-1507
https://egusphere.copernicus.org/preprints/2023/egusphere-2023-1507/
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spelling ftcopernicus:oai:publications.copernicus.org:egusphere113018 2023-09-05T13:19:39+02:00 Increasing numerical stability of mountain valley glacier simulations: implementation and testing of free-surface stabilization in Elmer/Ice Löfgren, André Zwinger, Thomas Råback, Peter Helanow, Christian Ahlkrona, Josefin 2023-08-09 application/pdf https://doi.org/10.5194/egusphere-2023-1507 https://egusphere.copernicus.org/preprints/2023/egusphere-2023-1507/ eng eng doi:10.5194/egusphere-2023-1507 https://egusphere.copernicus.org/preprints/2023/egusphere-2023-1507/ eISSN: Text 2023 ftcopernicus https://doi.org/10.5194/egusphere-2023-1507 2023-08-14T16:24:20Z This paper concerns a numerical stabilization method for free-surface ice flow called the free-surface stabilization algorithm (FSSA). In the current study, the FSSA is implemented into the numerical ice-flow software Elmer/Ice and tested on synthetic two-dimensional (2D) glaciers, as well as on the real-world glacier of Midtre Lovénbreen, Svalbard. For the synthetic 2D cases it is found that the FSSA method increases the largest stable time-step size at least by a factor of ten for the case of a gently sloping ice surface (3°), and by at least a factor of five for cases of moderately to steeply inclined surfaces (6° to 12°) . Furthermore, the FSSA method increases the overall accuracy for all surface slopes. The largest stable time-step size is found to be smallest for the case of a low sloping surface, despite having overall smaller velocities. For Midtre Lovénbreen the FSSA method doubles the largest stable time-step size, however, the accuracy is in this case slightly lowered in the deeper parts of the glacier, while it increases near edges. The implication is that the non-FSSA method might be more accurate at predicting glacier thinning, while the FSSA method is more suitable for predicting future glacier extent. A possible application of the larger time-step sizes allowed for by the FSSA is for spin-up simulations, where relatively fast changing climate data can be incorporated on short time scales, while the slowly changing velocity field is updated over larger time scales. Text glacier Svalbard Copernicus Publications: E-Journals Svalbard
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description This paper concerns a numerical stabilization method for free-surface ice flow called the free-surface stabilization algorithm (FSSA). In the current study, the FSSA is implemented into the numerical ice-flow software Elmer/Ice and tested on synthetic two-dimensional (2D) glaciers, as well as on the real-world glacier of Midtre Lovénbreen, Svalbard. For the synthetic 2D cases it is found that the FSSA method increases the largest stable time-step size at least by a factor of ten for the case of a gently sloping ice surface (3°), and by at least a factor of five for cases of moderately to steeply inclined surfaces (6° to 12°) . Furthermore, the FSSA method increases the overall accuracy for all surface slopes. The largest stable time-step size is found to be smallest for the case of a low sloping surface, despite having overall smaller velocities. For Midtre Lovénbreen the FSSA method doubles the largest stable time-step size, however, the accuracy is in this case slightly lowered in the deeper parts of the glacier, while it increases near edges. The implication is that the non-FSSA method might be more accurate at predicting glacier thinning, while the FSSA method is more suitable for predicting future glacier extent. A possible application of the larger time-step sizes allowed for by the FSSA is for spin-up simulations, where relatively fast changing climate data can be incorporated on short time scales, while the slowly changing velocity field is updated over larger time scales.
format Text
author Löfgren, André
Zwinger, Thomas
Råback, Peter
Helanow, Christian
Ahlkrona, Josefin
spellingShingle Löfgren, André
Zwinger, Thomas
Råback, Peter
Helanow, Christian
Ahlkrona, Josefin
Increasing numerical stability of mountain valley glacier simulations: implementation and testing of free-surface stabilization in Elmer/Ice
author_facet Löfgren, André
Zwinger, Thomas
Råback, Peter
Helanow, Christian
Ahlkrona, Josefin
author_sort Löfgren, André
title Increasing numerical stability of mountain valley glacier simulations: implementation and testing of free-surface stabilization in Elmer/Ice
title_short Increasing numerical stability of mountain valley glacier simulations: implementation and testing of free-surface stabilization in Elmer/Ice
title_full Increasing numerical stability of mountain valley glacier simulations: implementation and testing of free-surface stabilization in Elmer/Ice
title_fullStr Increasing numerical stability of mountain valley glacier simulations: implementation and testing of free-surface stabilization in Elmer/Ice
title_full_unstemmed Increasing numerical stability of mountain valley glacier simulations: implementation and testing of free-surface stabilization in Elmer/Ice
title_sort increasing numerical stability of mountain valley glacier simulations: implementation and testing of free-surface stabilization in elmer/ice
publishDate 2023
url https://doi.org/10.5194/egusphere-2023-1507
https://egusphere.copernicus.org/preprints/2023/egusphere-2023-1507/
geographic Svalbard
geographic_facet Svalbard
genre glacier
Svalbard
genre_facet glacier
Svalbard
op_source eISSN:
op_relation doi:10.5194/egusphere-2023-1507
https://egusphere.copernicus.org/preprints/2023/egusphere-2023-1507/
op_doi https://doi.org/10.5194/egusphere-2023-1507
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