Development of a viscoelastic model of ice shelf dynamics
Climate Change has already caused large losses on natural occurring ice in the last decades and continues to do so. Antarctica, the largest source of land ice, contains an equivalent of several tens of meters of sea water level rise, which is induced not only by melting but also by out flow into ice...
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ftccsdartic:oai:HAL:tel-04099198v1 2023-12-17T10:22:12+01:00 Development of a viscoelastic model of ice shelf dynamics Développement d'un modèle visco-élastique de la réponse dynamique des plateformes de glace Zimmermann, Astrid Margit Institut des Géosciences de l’Environnement (IGE) Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Université Grenoble Alpes (UGA)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP ) Université Grenoble Alpes (UGA) Université Grenoble Alpes 2020-. University of Swansea (Swansea (GB)) Emmanuel Lemeur Stephen Cornford 2023-01-25 https://theses.hal.science/tel-04099198 https://theses.hal.science/tel-04099198/document https://theses.hal.science/tel-04099198/file/ZIMMERMANN_2023_archivage.pdf en eng HAL CCSD NNT: 2023GRALU004 tel-04099198 https://theses.hal.science/tel-04099198 https://theses.hal.science/tel-04099198/document https://theses.hal.science/tel-04099198/file/ZIMMERMANN_2023_archivage.pdf info:eu-repo/semantics/OpenAccess https://theses.hal.science/tel-04099198 Glaciology. Université Grenoble Alpes [2020-.]; University of Swansea (Swansea (GB)), 2023. English. ⟨NNT : 2023GRALU004⟩ Rheology Snow study Modelling Antarctica Antarctique Modélisation Nivologie Travail de terrain [SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology info:eu-repo/semantics/doctoralThesis Theses 2023 ftccsdartic 2023-11-18T23:48:26Z Climate Change has already caused large losses on natural occurring ice in the last decades and continues to do so. Antarctica, the largest source of land ice, contains an equivalent of several tens of meters of sea water level rise, which is induced not only by melting but also by out flow into ice shelves, the floating tongues of glaciers. In the last decades with recorded longer melt seasons and warming water in Antarctica, ice shelves are thinning and breaking up. With that, speed up of shelf inflowing glaciers are recorded, highlighting the buttressing force ice shelves have on glaciers and therefore their importance to the Antarctic Ice Sheet.Many factors play a roll in the integrity of ice shelves, besides melting on the surface and from below, waves, tides and pressure imbalances at the calving front (buoyancy force) induce bending moments on short time scales.While ice is mainly studied as purely viscous, elastic or even plastic material. Certain ice shelf behaviour, like the tidal deformation near the grounding line or drainage of melt ponds, can only be sufficiently simulated with an viscoelastic model - representing the viscous thinning of ice as well as short term elastic bending deformations.Viscoelastic studies of ice so far have used commercial proprietary software, which require expensive licences and often lack inside in the used algorithms or flexibility to adapt the code as needed.In this thesis a viscoelastic model was developed in the open source FEM C++ environment Rheolef. Le changement climatique a engendré des pertes considérables pour les glaces continentales au cours de ces dernières décennies et perdure toujours aujourd'hui. L'Antarctique, la plus grande réserve de glace naturelle recèle à lui seul l'équivalent d'une hausse potentielle du niveau marin mondial de plusieurs dizaines de m, laquelle résulte non seulement de la fonte mais aussi de l'écoulement de la glace au travers les plateformes flottantes des glaciers émissaires, les 'ice shelves'. Depuis les dernières décennies ... Doctoral or Postdoctoral Thesis Antarc* Antarctic Antarctica Antarctique* Ice Shelf Ice Shelves Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) Antarctic The Antarctic |
institution |
Open Polar |
collection |
Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) |
op_collection_id |
ftccsdartic |
language |
English |
topic |
Rheology Snow study Modelling Antarctica Antarctique Modélisation Nivologie Travail de terrain [SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology |
spellingShingle |
Rheology Snow study Modelling Antarctica Antarctique Modélisation Nivologie Travail de terrain [SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology Zimmermann, Astrid Margit Development of a viscoelastic model of ice shelf dynamics |
topic_facet |
Rheology Snow study Modelling Antarctica Antarctique Modélisation Nivologie Travail de terrain [SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology |
description |
Climate Change has already caused large losses on natural occurring ice in the last decades and continues to do so. Antarctica, the largest source of land ice, contains an equivalent of several tens of meters of sea water level rise, which is induced not only by melting but also by out flow into ice shelves, the floating tongues of glaciers. In the last decades with recorded longer melt seasons and warming water in Antarctica, ice shelves are thinning and breaking up. With that, speed up of shelf inflowing glaciers are recorded, highlighting the buttressing force ice shelves have on glaciers and therefore their importance to the Antarctic Ice Sheet.Many factors play a roll in the integrity of ice shelves, besides melting on the surface and from below, waves, tides and pressure imbalances at the calving front (buoyancy force) induce bending moments on short time scales.While ice is mainly studied as purely viscous, elastic or even plastic material. Certain ice shelf behaviour, like the tidal deformation near the grounding line or drainage of melt ponds, can only be sufficiently simulated with an viscoelastic model - representing the viscous thinning of ice as well as short term elastic bending deformations.Viscoelastic studies of ice so far have used commercial proprietary software, which require expensive licences and often lack inside in the used algorithms or flexibility to adapt the code as needed.In this thesis a viscoelastic model was developed in the open source FEM C++ environment Rheolef. Le changement climatique a engendré des pertes considérables pour les glaces continentales au cours de ces dernières décennies et perdure toujours aujourd'hui. L'Antarctique, la plus grande réserve de glace naturelle recèle à lui seul l'équivalent d'une hausse potentielle du niveau marin mondial de plusieurs dizaines de m, laquelle résulte non seulement de la fonte mais aussi de l'écoulement de la glace au travers les plateformes flottantes des glaciers émissaires, les 'ice shelves'. Depuis les dernières décennies ... |
author2 |
Institut des Géosciences de l’Environnement (IGE) Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Université Grenoble Alpes (UGA)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP ) Université Grenoble Alpes (UGA) Université Grenoble Alpes 2020-. University of Swansea (Swansea (GB)) Emmanuel Lemeur Stephen Cornford |
format |
Doctoral or Postdoctoral Thesis |
author |
Zimmermann, Astrid Margit |
author_facet |
Zimmermann, Astrid Margit |
author_sort |
Zimmermann, Astrid Margit |
title |
Development of a viscoelastic model of ice shelf dynamics |
title_short |
Development of a viscoelastic model of ice shelf dynamics |
title_full |
Development of a viscoelastic model of ice shelf dynamics |
title_fullStr |
Development of a viscoelastic model of ice shelf dynamics |
title_full_unstemmed |
Development of a viscoelastic model of ice shelf dynamics |
title_sort |
development of a viscoelastic model of ice shelf dynamics |
publisher |
HAL CCSD |
publishDate |
2023 |
url |
https://theses.hal.science/tel-04099198 https://theses.hal.science/tel-04099198/document https://theses.hal.science/tel-04099198/file/ZIMMERMANN_2023_archivage.pdf |
geographic |
Antarctic The Antarctic |
geographic_facet |
Antarctic The Antarctic |
genre |
Antarc* Antarctic Antarctica Antarctique* Ice Shelf Ice Shelves |
genre_facet |
Antarc* Antarctic Antarctica Antarctique* Ice Shelf Ice Shelves |
op_source |
https://theses.hal.science/tel-04099198 Glaciology. Université Grenoble Alpes [2020-.]; University of Swansea (Swansea (GB)), 2023. English. ⟨NNT : 2023GRALU004⟩ |
op_relation |
NNT: 2023GRALU004 tel-04099198 https://theses.hal.science/tel-04099198 https://theses.hal.science/tel-04099198/document https://theses.hal.science/tel-04099198/file/ZIMMERMANN_2023_archivage.pdf |
op_rights |
info:eu-repo/semantics/OpenAccess |
_version_ |
1785544747984617472 |