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...

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Main Authors: Jouvet, Guillaume, Gräser, Carsten
Format: Report
Language:unknown
Published: Freie Universität Berlin 2012
Subjects:
Online Access:https://dx.doi.org/10.17169/refubium-21788
https://refubium.fu-berlin.de/handle/fub188/18076
id ftdatacite:10.17169/refubium-21788
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spelling ftdatacite:10.17169/refubium-21788 2023-05-15T16:40:15+02:00 An adaptive Newton multigrid method for a model of marine ice sheets Jouvet, Guillaume Gräser, Carsten 2012 https://dx.doi.org/10.17169/refubium-21788 https://refubium.fu-berlin.de/handle/fub188/18076 unknown Freie Universität Berlin http://www.fu-berlin.de/sites/refubium/rechtliches/Nutzungsbedingungen ice sheet model ice flow variational inequality nonlinear multigrid method 500 Naturwissenschaften und Mathematik510 Mathematik Preprint Text article-journal ScholarlyArticle 2012 ftdatacite https://doi.org/10.17169/refubium-21788 2021-11-05T12:55:41Z 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 DataCite Metadata Store (German National Library of Science and Technology) Laplace ENVELOPE(141.467,141.467,-66.782,-66.782)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language unknown
topic ice sheet model
ice flow
variational inequality
nonlinear multigrid method
500 Naturwissenschaften und Mathematik510 Mathematik
spellingShingle ice sheet model
ice flow
variational inequality
nonlinear multigrid method
500 Naturwissenschaften und Mathematik510 Mathematik
Jouvet, Guillaume
Gräser, Carsten
An adaptive Newton multigrid method for a model of marine ice sheets
topic_facet ice sheet model
ice flow
variational inequality
nonlinear multigrid method
500 Naturwissenschaften und Mathematik510 Mathematik
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
author Jouvet, Guillaume
Gräser, Carsten
author_facet Jouvet, Guillaume
Gräser, Carsten
author_sort Jouvet, Guillaume
title 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_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_sort adaptive newton multigrid method for a model of marine ice sheets
publisher Freie Universität Berlin
publishDate 2012
url https://dx.doi.org/10.17169/refubium-21788
https://refubium.fu-berlin.de/handle/fub188/18076
long_lat ENVELOPE(141.467,141.467,-66.782,-66.782)
geographic Laplace
geographic_facet Laplace
genre Ice Sheet
Ice Shelf
genre_facet Ice Sheet
Ice Shelf
op_rights http://www.fu-berlin.de/sites/refubium/rechtliches/Nutzungsbedingungen
op_doi https://doi.org/10.17169/refubium-21788
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