Accurate and stable time stepping in ice sheet modeling

In this paper we introduce adaptive time step control for simulation of evolution of ice sheets. The discretization error in the approximations is estimated using "Milne's device" by comparing the result from two different methods in a predictor-corrector pair. Using a predictor-corre...

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Main Authors: Cheng, Gong, Lötstedt, Per, von Sydow, Lina
Format: Text
Language:unknown
Published: arXiv 2016
Subjects:
Online Access:https://dx.doi.org/10.48550/arxiv.1605.06970
https://arxiv.org/abs/1605.06970
id ftdatacite:10.48550/arxiv.1605.06970
record_format openpolar
spelling ftdatacite:10.48550/arxiv.1605.06970 2023-05-15T16:40:33+02:00 Accurate and stable time stepping in ice sheet modeling Cheng, Gong Lötstedt, Per von Sydow, Lina 2016 https://dx.doi.org/10.48550/arxiv.1605.06970 https://arxiv.org/abs/1605.06970 unknown arXiv https://dx.doi.org/10.1016/j.jcp.2016.10.060 arXiv.org perpetual, non-exclusive license http://arxiv.org/licenses/nonexclusive-distrib/1.0/ Computational Physics physics.comp-ph FOS Physical sciences 65M99, 86-08, 86A40 article-journal Article ScholarlyArticle Text 2016 ftdatacite https://doi.org/10.48550/arxiv.1605.06970 https://doi.org/10.1016/j.jcp.2016.10.060 2022-04-01T11:40:58Z In this paper we introduce adaptive time step control for simulation of evolution of ice sheets. The discretization error in the approximations is estimated using "Milne's device" by comparing the result from two different methods in a predictor-corrector pair. Using a predictor-corrector pair the expensive part of the procedure, the solution of the velocity and pressure equations, is performed only once per time step and an estimate of the local error is easily obtained. The stability of the numerical solution is maintained and the accuracy is controlled by keeping the local error below a given threshold using PI-control. Depending on the threshold, the time step $Δt$ is bound by stability requirements or accuracy requirements. Our method takes a shorter $Δt$ than an implicit method but with less work in each time step and the solver is simpler. The method is analyzed theoretically with respect to stability and applied to the simulation of a 2D ice slab and a 3D circular ice sheet. %The automatically chosen $Δt$ is either restricted by accuracy or stability depedning on an error tolerance. The stability bounds in the experiments are explained by and agree well with the theoretical results. Text Ice Sheet DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language unknown
topic Computational Physics physics.comp-ph
FOS Physical sciences
65M99, 86-08, 86A40
spellingShingle Computational Physics physics.comp-ph
FOS Physical sciences
65M99, 86-08, 86A40
Cheng, Gong
Lötstedt, Per
von Sydow, Lina
Accurate and stable time stepping in ice sheet modeling
topic_facet Computational Physics physics.comp-ph
FOS Physical sciences
65M99, 86-08, 86A40
description In this paper we introduce adaptive time step control for simulation of evolution of ice sheets. The discretization error in the approximations is estimated using "Milne's device" by comparing the result from two different methods in a predictor-corrector pair. Using a predictor-corrector pair the expensive part of the procedure, the solution of the velocity and pressure equations, is performed only once per time step and an estimate of the local error is easily obtained. The stability of the numerical solution is maintained and the accuracy is controlled by keeping the local error below a given threshold using PI-control. Depending on the threshold, the time step $Δt$ is bound by stability requirements or accuracy requirements. Our method takes a shorter $Δt$ than an implicit method but with less work in each time step and the solver is simpler. The method is analyzed theoretically with respect to stability and applied to the simulation of a 2D ice slab and a 3D circular ice sheet. %The automatically chosen $Δt$ is either restricted by accuracy or stability depedning on an error tolerance. The stability bounds in the experiments are explained by and agree well with the theoretical results.
format Text
author Cheng, Gong
Lötstedt, Per
von Sydow, Lina
author_facet Cheng, Gong
Lötstedt, Per
von Sydow, Lina
author_sort Cheng, Gong
title Accurate and stable time stepping in ice sheet modeling
title_short Accurate and stable time stepping in ice sheet modeling
title_full Accurate and stable time stepping in ice sheet modeling
title_fullStr Accurate and stable time stepping in ice sheet modeling
title_full_unstemmed Accurate and stable time stepping in ice sheet modeling
title_sort accurate and stable time stepping in ice sheet modeling
publisher arXiv
publishDate 2016
url https://dx.doi.org/10.48550/arxiv.1605.06970
https://arxiv.org/abs/1605.06970
genre Ice Sheet
genre_facet Ice Sheet
op_relation https://dx.doi.org/10.1016/j.jcp.2016.10.060
op_rights arXiv.org perpetual, non-exclusive license
http://arxiv.org/licenses/nonexclusive-distrib/1.0/
op_doi https://doi.org/10.48550/arxiv.1605.06970
https://doi.org/10.1016/j.jcp.2016.10.060
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