Steady, shallow ice sheets as obstacle problems: Well-posedness and finite element approximation

We formulate steady, shallow ice sheet flow as an obstacle problem, the unknown being the ice upper surface and the obstacle being the underlying bedrock topography. This generates a free-boundary defining the ice sheet extent. The obstacle problem is written as a variational inequality subject to t...

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Published in:SIAM Journal on Applied Mathematics
Main Authors: Jouvet, G., Bueler, E.
Format: Article in Journal/Newspaper
Language:English
Published: SIAM 2012
Subjects:
Online Access:http://publications.imp.fu-berlin.de/1867/
http://publications.imp.fu-berlin.de/1867/1/Jouvet_Bueler_2012.pdf
https://doi.org/10.1137/110856654
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spelling ftfuberlinimp:oai:biocomputing-berlin.de:1867 2023-05-15T16:29:01+02:00 Steady, shallow ice sheets as obstacle problems: Well-posedness and finite element approximation Jouvet, G. Bueler, E. 2012 application/pdf http://publications.imp.fu-berlin.de/1867/ http://publications.imp.fu-berlin.de/1867/1/Jouvet_Bueler_2012.pdf https://doi.org/10.1137/110856654 en eng SIAM http://publications.imp.fu-berlin.de/1867/1/Jouvet_Bueler_2012.pdf Jouvet, G. and Bueler, E. (2012) Steady, shallow ice sheets as obstacle problems: Well-posedness and finite element approximation. SIAM J. Appl. Math., 72 (4). pp. 1292-1314. ISSN 0036-1399 Numerical Analysis Article PeerReviewed 2012 ftfuberlinimp https://doi.org/10.1137/110856654 2022-07-10T14:27:19Z We formulate steady, shallow ice sheet flow as an obstacle problem, the unknown being the ice upper surface and the obstacle being the underlying bedrock topography. This generates a free-boundary defining the ice sheet extent. The obstacle problem is written as a variational inequality subject to the positive-ice-thickness constraint. The corresponding PDE is a highly nonlinear elliptic equation which generalizes the $p$-Laplacian equation. Our formulation also permits variable ice softness, basal sliding, and elevation-dependent surface mass balance. Existence and uniqueness are shown in restricted cases which we may reformulate as a convex minimization problem. In the general case we show existence by applying a fixed point argument. Using continuity results from that argument, we construct a numerical solution by solving a sequence of obstacle $p$-Laplacian-like problems by finite element approximation. As a real application, we compute the steady-state shape of the Greenland ice sheet in a steady present-day climate. Article in Journal/Newspaper Greenland Ice Sheet fu_mi_publications (Repository - Freie Universität Berlin, Math Department Greenland SIAM Journal on Applied Mathematics 72 4 1292 1314
institution Open Polar
collection fu_mi_publications (Repository - Freie Universität Berlin, Math Department
op_collection_id ftfuberlinimp
language English
topic Numerical Analysis
spellingShingle Numerical Analysis
Jouvet, G.
Bueler, E.
Steady, shallow ice sheets as obstacle problems: Well-posedness and finite element approximation
topic_facet Numerical Analysis
description We formulate steady, shallow ice sheet flow as an obstacle problem, the unknown being the ice upper surface and the obstacle being the underlying bedrock topography. This generates a free-boundary defining the ice sheet extent. The obstacle problem is written as a variational inequality subject to the positive-ice-thickness constraint. The corresponding PDE is a highly nonlinear elliptic equation which generalizes the $p$-Laplacian equation. Our formulation also permits variable ice softness, basal sliding, and elevation-dependent surface mass balance. Existence and uniqueness are shown in restricted cases which we may reformulate as a convex minimization problem. In the general case we show existence by applying a fixed point argument. Using continuity results from that argument, we construct a numerical solution by solving a sequence of obstacle $p$-Laplacian-like problems by finite element approximation. As a real application, we compute the steady-state shape of the Greenland ice sheet in a steady present-day climate.
format Article in Journal/Newspaper
author Jouvet, G.
Bueler, E.
author_facet Jouvet, G.
Bueler, E.
author_sort Jouvet, G.
title Steady, shallow ice sheets as obstacle problems: Well-posedness and finite element approximation
title_short Steady, shallow ice sheets as obstacle problems: Well-posedness and finite element approximation
title_full Steady, shallow ice sheets as obstacle problems: Well-posedness and finite element approximation
title_fullStr Steady, shallow ice sheets as obstacle problems: Well-posedness and finite element approximation
title_full_unstemmed Steady, shallow ice sheets as obstacle problems: Well-posedness and finite element approximation
title_sort steady, shallow ice sheets as obstacle problems: well-posedness and finite element approximation
publisher SIAM
publishDate 2012
url http://publications.imp.fu-berlin.de/1867/
http://publications.imp.fu-berlin.de/1867/1/Jouvet_Bueler_2012.pdf
https://doi.org/10.1137/110856654
geographic Greenland
geographic_facet Greenland
genre Greenland
Ice Sheet
genre_facet Greenland
Ice Sheet
op_relation http://publications.imp.fu-berlin.de/1867/1/Jouvet_Bueler_2012.pdf
Jouvet, G. and Bueler, E. (2012) Steady, shallow ice sheets as obstacle problems: Well-posedness and finite element approximation. SIAM J. Appl. Math., 72 (4). pp. 1292-1314. ISSN 0036-1399
op_doi https://doi.org/10.1137/110856654
container_title SIAM Journal on Applied Mathematics
container_volume 72
container_issue 4
container_start_page 1292
op_container_end_page 1314
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