An adaptive Newton multigrid method for a model of marine ice sheets
In this paper, we consider a model for the time evolution of marine ice sheets. This model combines the Shallow Ice Approximation (SIA) for the ice deformation, the Shallow Shelf Approximation (SSA) for the basal sliding and the mass conservation principle. At each time step, we solve a generalized...
Main Authors: | , |
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Format: | Report |
Language: | English |
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2012
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Online Access: | https://refubium.fu-berlin.de/handle/fub188/18076 https://doi.org/10.17169/refubium-21788 |
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author | Jouvet, Guillaume Gräser, Carsten |
author_facet | Jouvet, Guillaume Gräser, Carsten |
author_sort | Jouvet, Guillaume |
collection | Freie Universität Berlin: Refubium (FU Berlin) |
description | In this paper, we consider a model for the time evolution of marine ice sheets. This model combines the Shallow Ice Approximation (SIA) for the ice deformation, the Shallow Shelf Approximation (SSA) for the basal sliding and the mass conservation principle. At each time step, we solve a generalized p-Laplace minimization-type problem with obstacle (SIA), a vectorial p-Laplace minimization-type problem (SSA) and a transport equation (mass conservation). The two minimization problems are solved using a truncated nonsmooth Newton multigrid method while the transport equation is solved using a vertex-centred finite volume method. Our approach is combined to a mesh adaptive refinement procedure to face the large gradients of the solution that are expected close to the grounding line which separates the ice sheet and the ice shelf. As applications, we present some simulations of the marine ice sheet model inter- comparison project MISMIP in two and three space dimensions. In particular, we test the ability of our model to reproduce a reversible grounding line after being perturbed in model parameters. |
format | Report |
genre | Ice Sheet Ice Shelf |
genre_facet | Ice Sheet Ice Shelf |
geographic | Laplace |
geographic_facet | Laplace |
id | ftfuberlin:oai:refubium.fu-berlin.de:fub188/18076 |
institution | Open Polar |
language | English |
long_lat | ENVELOPE(141.467,141.467,-66.782,-66.782) |
op_collection_id | ftfuberlin |
op_doi | https://doi.org/10.17169/refubium-21788 |
op_relation | urn:nbn:de:kobv:188-fudocsseries000000000226-9 |
op_rights | http://www.fu-berlin.de/sites/refubium/rechtliches/Nutzungsbedingungen |
publishDate | 2012 |
record_format | openpolar |
spelling | ftfuberlin:oai:refubium.fu-berlin.de:fub188/18076 2025-05-18T14:03:12+00:00 An adaptive Newton multigrid method for a model of marine ice sheets Jouvet, Guillaume Gräser, Carsten 2012 29 S. application/pdf https://refubium.fu-berlin.de/handle/fub188/18076 https://doi.org/10.17169/refubium-21788 eng eng urn:nbn:de:kobv:188-fudocsseries000000000226-9 http://www.fu-berlin.de/sites/refubium/rechtliches/Nutzungsbedingungen ice sheet model ice flow variational inequality nonlinear multigrid method ddc:510 doc-type:preprint 2012 ftfuberlin https://doi.org/10.17169/refubium-21788 2025-04-22T04:03:03Z In this paper, we consider a model for the time evolution of marine ice sheets. This model combines the Shallow Ice Approximation (SIA) for the ice deformation, the Shallow Shelf Approximation (SSA) for the basal sliding and the mass conservation principle. At each time step, we solve a generalized p-Laplace minimization-type problem with obstacle (SIA), a vectorial p-Laplace minimization-type problem (SSA) and a transport equation (mass conservation). The two minimization problems are solved using a truncated nonsmooth Newton multigrid method while the transport equation is solved using a vertex-centred finite volume method. Our approach is combined to a mesh adaptive refinement procedure to face the large gradients of the solution that are expected close to the grounding line which separates the ice sheet and the ice shelf. As applications, we present some simulations of the marine ice sheet model inter- comparison project MISMIP in two and three space dimensions. In particular, we test the ability of our model to reproduce a reversible grounding line after being perturbed in model parameters. Report Ice Sheet Ice Shelf Freie Universität Berlin: Refubium (FU Berlin) Laplace ENVELOPE(141.467,141.467,-66.782,-66.782) |
spellingShingle | ice sheet model ice flow variational inequality nonlinear multigrid method ddc:510 Jouvet, Guillaume Gräser, Carsten An adaptive Newton multigrid method for a model of marine ice sheets |
title | An adaptive Newton multigrid method for a model of marine ice sheets |
title_full | An adaptive Newton multigrid method for a model of marine ice sheets |
title_fullStr | An adaptive Newton multigrid method for a model of marine ice sheets |
title_full_unstemmed | An adaptive Newton multigrid method for a model of marine ice sheets |
title_short | An adaptive Newton multigrid method for a model of marine ice sheets |
title_sort | adaptive newton multigrid method for a model of marine ice sheets |
topic | ice sheet model ice flow variational inequality nonlinear multigrid method ddc:510 |
topic_facet | ice sheet model ice flow variational inequality nonlinear multigrid method ddc:510 |
url | https://refubium.fu-berlin.de/handle/fub188/18076 https://doi.org/10.17169/refubium-21788 |