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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Main Author: Zimmermann, Astrid Margit
Other Authors: 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
Language:English
Published: HAL CCSD 2023
Subjects:
Online Access:https://theses.hal.science/tel-04099198
https://theses.hal.science/tel-04099198/document
https://theses.hal.science/tel-04099198/file/ZIMMERMANN_2023_archivage.pdf
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spelling 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
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