On the finite element approximation of a semicoercive stokes variational inequality arising in glaciology

Stokes variational inequalities arise in the formulation of glaciological problems involving contact. We consider the problem of a two-dimensional marine ice sheet with a grounding line, although the analysis presented here is extendable to other contact problems in glaciology, such as that of subgl...

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Published in:SIAM Journal on Numerical Analysis
Main Authors: de Diego, G, Farrell, P, Hewitt, I
Format: Article in Journal/Newspaper
Language:English
Published: Society for Industrial and Applied Mathematics 2022
Subjects:
Online Access:https://doi.org/10.1137/21M1437640
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spelling ftuloxford:oai:ora.ox.ac.uk:uuid:c607888d-f850-4ca2-99f9-19607bff6435 2023-05-15T16:41:01+02:00 On the finite element approximation of a semicoercive stokes variational inequality arising in glaciology de Diego, G Farrell, P Hewitt, I 2022-11-11 https://doi.org/10.1137/21M1437640 https://ora.ox.ac.uk/objects/uuid:c607888d-f850-4ca2-99f9-19607bff6435 eng eng Society for Industrial and Applied Mathematics doi:10.1137/21M1437640 https://ora.ox.ac.uk/objects/uuid:c607888d-f850-4ca2-99f9-19607bff6435 https://doi.org/10.1137/21M1437640 info:eu-repo/semantics/openAccess Journal article 2022 ftuloxford https://doi.org/10.1137/21M1437640 2023-03-16T23:06:11Z Stokes variational inequalities arise in the formulation of glaciological problems involving contact. We consider the problem of a two-dimensional marine ice sheet with a grounding line, although the analysis presented here is extendable to other contact problems in glaciology, such as that of subglacial cavitation. The analysis of this problem and its discretisation is complicated by the nonlinear rheology commonly used for modelling ice, the enforcement of a friction boundary condition given by a power law, and the presence of rigid modes in the velocity space, which render the variational inequality semicoercive. In this work, we consider a mixed formulation of this variational inequality involving a Lagrange multiplier and provide an analysis of its finite element approximation. Error estimates in the presence of rigid modes are obtained by means of a specially-built projection operator onto the subspace of rigid modes and a Korn-type inequality. These proofs rely on the fact that the subspace of rigid modes is at most one-dimensional, a property which is a consequence of the two-dimensionality of the domain. Numerical results are reported to validate the error estimates. Article in Journal/Newspaper Ice Sheet ORA - Oxford University Research Archive Korn ENVELOPE(159.267,159.267,58.408,58.408) Lagrange ENVELOPE(-62.597,-62.597,-64.529,-64.529) SIAM Journal on Numerical Analysis 61 1 1 25
institution Open Polar
collection ORA - Oxford University Research Archive
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language English
description Stokes variational inequalities arise in the formulation of glaciological problems involving contact. We consider the problem of a two-dimensional marine ice sheet with a grounding line, although the analysis presented here is extendable to other contact problems in glaciology, such as that of subglacial cavitation. The analysis of this problem and its discretisation is complicated by the nonlinear rheology commonly used for modelling ice, the enforcement of a friction boundary condition given by a power law, and the presence of rigid modes in the velocity space, which render the variational inequality semicoercive. In this work, we consider a mixed formulation of this variational inequality involving a Lagrange multiplier and provide an analysis of its finite element approximation. Error estimates in the presence of rigid modes are obtained by means of a specially-built projection operator onto the subspace of rigid modes and a Korn-type inequality. These proofs rely on the fact that the subspace of rigid modes is at most one-dimensional, a property which is a consequence of the two-dimensionality of the domain. Numerical results are reported to validate the error estimates.
format Article in Journal/Newspaper
author de Diego, G
Farrell, P
Hewitt, I
spellingShingle de Diego, G
Farrell, P
Hewitt, I
On the finite element approximation of a semicoercive stokes variational inequality arising in glaciology
author_facet de Diego, G
Farrell, P
Hewitt, I
author_sort de Diego, G
title On the finite element approximation of a semicoercive stokes variational inequality arising in glaciology
title_short On the finite element approximation of a semicoercive stokes variational inequality arising in glaciology
title_full On the finite element approximation of a semicoercive stokes variational inequality arising in glaciology
title_fullStr On the finite element approximation of a semicoercive stokes variational inequality arising in glaciology
title_full_unstemmed On the finite element approximation of a semicoercive stokes variational inequality arising in glaciology
title_sort on the finite element approximation of a semicoercive stokes variational inequality arising in glaciology
publisher Society for Industrial and Applied Mathematics
publishDate 2022
url https://doi.org/10.1137/21M1437640
https://ora.ox.ac.uk/objects/uuid:c607888d-f850-4ca2-99f9-19607bff6435
long_lat ENVELOPE(159.267,159.267,58.408,58.408)
ENVELOPE(-62.597,-62.597,-64.529,-64.529)
geographic Korn
Lagrange
geographic_facet Korn
Lagrange
genre Ice Sheet
genre_facet Ice Sheet
op_relation doi:10.1137/21M1437640
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https://doi.org/10.1137/21M1437640
op_rights info:eu-repo/semantics/openAccess
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container_title SIAM Journal on Numerical Analysis
container_volume 61
container_issue 1
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