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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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 |
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Open Polar |
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fu_mi_publications (Repository - Freie Universität Berlin, Math Department |
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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 |
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SIAM Journal on Applied Mathematics |
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72 |
container_issue |
4 |
container_start_page |
1292 |
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1314 |
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1766018702633861120 |