Full Stokes modeling of marine ice sheets: influence of the grid size
Using the finite-element code Elmer, we show that the full Stokes modeling of the ice-sheet/ice-shelf transition we propose can give consistent predictions of grounding-line migration. Like other marine ice-sheet models our approach is highly sensitive to the chosen mesh resolution. However, with a...
Published in: | Annals of Glaciology |
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International Glaciological Society
2009
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ftoskarbordeaux:oai:oskar-bordeaux.fr:20.500.12278/28991 2023-05-15T16:40:21+02:00 Full Stokes modeling of marine ice sheets: influence of the grid size DURAND, Gaël GAGLIARDINI, Olivier ZWINGER, Thomas LE MEUR, Emmanuel HINDMARSH, Richard C.A. 2009 https://oskar-bordeaux.fr/handle/20.500.12278/28991 https://doi.org/10.3189/172756409789624283 en eng International Glaciological Society 0260-3055 https://oskar-bordeaux.fr/handle/20.500.12278/28991 doi:10.3189/172756409789624283 http://creativecommons.org/licenses/by/ Planète et Univers [physics]/Sciences de la Terre/Glaciologie Article de revue 2009 ftoskarbordeaux https://doi.org/10.3189/172756409789624283 2021-05-11T22:29:11Z Using the finite-element code Elmer, we show that the full Stokes modeling of the ice-sheet/ice-shelf transition we propose can give consistent predictions of grounding-line migration. Like other marine ice-sheet models our approach is highly sensitive to the chosen mesh resolution. However, with a grid size down to <5 km in the vicinity of the grounding line, predictions start to be robust because: (1) whatever the grid size (<5 km) the steady-state grounding-line position is sensibly the same (6 km standard deviation), and (2) with a grid-size refinement in the vicinity of the grounding line (200 m), the steady-state solution is independent of the applied perturbation in fluidity, provided this perturbation remains monotonic. Dynamique des glaciers côtiers et rôle sur le bilan de masse global de l'Antarctique zone atelier du glacier de l'Astrolabe, Terre Adélie Other/Unknown Material Ice Sheet Ice Shelf OSKAR Bordeaux (Open Science Knowledge ARchive) Terre Adélie ENVELOPE(139.000,139.000,-67.000,-67.000) Terre-Adélie ENVELOPE(138.991,138.991,-59.999,-59.999) Annals of Glaciology 50 52 109 114 |
institution |
Open Polar |
collection |
OSKAR Bordeaux (Open Science Knowledge ARchive) |
op_collection_id |
ftoskarbordeaux |
language |
English |
topic |
Planète et Univers [physics]/Sciences de la Terre/Glaciologie |
spellingShingle |
Planète et Univers [physics]/Sciences de la Terre/Glaciologie DURAND, Gaël GAGLIARDINI, Olivier ZWINGER, Thomas LE MEUR, Emmanuel HINDMARSH, Richard C.A. Full Stokes modeling of marine ice sheets: influence of the grid size |
topic_facet |
Planète et Univers [physics]/Sciences de la Terre/Glaciologie |
description |
Using the finite-element code Elmer, we show that the full Stokes modeling of the ice-sheet/ice-shelf transition we propose can give consistent predictions of grounding-line migration. Like other marine ice-sheet models our approach is highly sensitive to the chosen mesh resolution. However, with a grid size down to <5 km in the vicinity of the grounding line, predictions start to be robust because: (1) whatever the grid size (<5 km) the steady-state grounding-line position is sensibly the same (6 km standard deviation), and (2) with a grid-size refinement in the vicinity of the grounding line (200 m), the steady-state solution is independent of the applied perturbation in fluidity, provided this perturbation remains monotonic. Dynamique des glaciers côtiers et rôle sur le bilan de masse global de l'Antarctique zone atelier du glacier de l'Astrolabe, Terre Adélie |
format |
Other/Unknown Material |
author |
DURAND, Gaël GAGLIARDINI, Olivier ZWINGER, Thomas LE MEUR, Emmanuel HINDMARSH, Richard C.A. |
author_facet |
DURAND, Gaël GAGLIARDINI, Olivier ZWINGER, Thomas LE MEUR, Emmanuel HINDMARSH, Richard C.A. |
author_sort |
DURAND, Gaël |
title |
Full Stokes modeling of marine ice sheets: influence of the grid size |
title_short |
Full Stokes modeling of marine ice sheets: influence of the grid size |
title_full |
Full Stokes modeling of marine ice sheets: influence of the grid size |
title_fullStr |
Full Stokes modeling of marine ice sheets: influence of the grid size |
title_full_unstemmed |
Full Stokes modeling of marine ice sheets: influence of the grid size |
title_sort |
full stokes modeling of marine ice sheets: influence of the grid size |
publisher |
International Glaciological Society |
publishDate |
2009 |
url |
https://oskar-bordeaux.fr/handle/20.500.12278/28991 https://doi.org/10.3189/172756409789624283 |
long_lat |
ENVELOPE(139.000,139.000,-67.000,-67.000) ENVELOPE(138.991,138.991,-59.999,-59.999) |
geographic |
Terre Adélie Terre-Adélie |
geographic_facet |
Terre Adélie Terre-Adélie |
genre |
Ice Sheet Ice Shelf |
genre_facet |
Ice Sheet Ice Shelf |
op_relation |
0260-3055 https://oskar-bordeaux.fr/handle/20.500.12278/28991 doi:10.3189/172756409789624283 |
op_rights |
http://creativecommons.org/licenses/by/ |
op_doi |
https://doi.org/10.3189/172756409789624283 |
container_title |
Annals of Glaciology |
container_volume |
50 |
container_issue |
52 |
container_start_page |
109 |
op_container_end_page |
114 |
_version_ |
1766030740529610752 |