Improved convergence and stability properties in a three-dimensional higher-order ice sheet model

We present a finite difference implementation of a three-dimensional higher-order ice sheet model. In comparison to a conventional centred difference discretisation it enhances both numerical stability and convergence. In order to achieve these benefits the discretisation of the governing force bala...

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Published in:Geoscientific Model Development
Main Authors: J. J. Fürst, O. Rybak, H. Goelzer, B. De Smedt, P. de Groen, P. Huybrechts
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2011
Subjects:
Online Access:https://doi.org/10.5194/gmd-4-1133-2011
https://doaj.org/article/b5353d9d1faf482aa5c39b40bfa94356
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spelling ftdoajarticles:oai:doaj.org/article:b5353d9d1faf482aa5c39b40bfa94356 2023-05-15T16:40:35+02:00 Improved convergence and stability properties in a three-dimensional higher-order ice sheet model J. J. Fürst O. Rybak H. Goelzer B. De Smedt P. de Groen P. Huybrechts 2011-12-01T00:00:00Z https://doi.org/10.5194/gmd-4-1133-2011 https://doaj.org/article/b5353d9d1faf482aa5c39b40bfa94356 EN eng Copernicus Publications http://www.geosci-model-dev.net/4/1133/2011/gmd-4-1133-2011.pdf https://doaj.org/toc/1991-959X https://doaj.org/toc/1991-9603 doi:10.5194/gmd-4-1133-2011 1991-959X 1991-9603 https://doaj.org/article/b5353d9d1faf482aa5c39b40bfa94356 Geoscientific Model Development, Vol 4, Iss 4, Pp 1133-1149 (2011) Geology QE1-996.5 article 2011 ftdoajarticles https://doi.org/10.5194/gmd-4-1133-2011 2022-12-31T12:37:41Z We present a finite difference implementation of a three-dimensional higher-order ice sheet model. In comparison to a conventional centred difference discretisation it enhances both numerical stability and convergence. In order to achieve these benefits the discretisation of the governing force balance equation makes extensive use of information on staggered grid points. Using the same iterative solver, a centred difference discretisation that operates exclusively on the regular grid serves as a reference. The reprise of the ISMIP-HOM experiments indicates that both discretisations are capable of reproducing the higher-order model inter-comparison results. This setup allows a direct comparison of the two numerical implementations also with respect to their convergence behaviour. First and foremost, the new finite difference scheme facilitates convergence by a factor of up to 7 and 2.6 in average. In addition to this decrease in computational costs, the accuracy for the resultant velocity field can be chosen higher in the novel finite difference implementation. Changing the discretisation also prevents build-up of local field irregularites that occasionally cause divergence of the solution for the reference discretisation. The improved behaviour makes the new discretisation more reliable for extensive application to real ice geometries. Higher accuracy and robust numerics are crucial in time dependent applications since numerical oscillations in the velocity field of subsequent time steps are attenuated and divergence of the solution is prevented. Article in Journal/Newspaper Ice Sheet Directory of Open Access Journals: DOAJ Articles Geoscientific Model Development 4 4 1133 1149
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Geology
QE1-996.5
spellingShingle Geology
QE1-996.5
J. J. Fürst
O. Rybak
H. Goelzer
B. De Smedt
P. de Groen
P. Huybrechts
Improved convergence and stability properties in a three-dimensional higher-order ice sheet model
topic_facet Geology
QE1-996.5
description We present a finite difference implementation of a three-dimensional higher-order ice sheet model. In comparison to a conventional centred difference discretisation it enhances both numerical stability and convergence. In order to achieve these benefits the discretisation of the governing force balance equation makes extensive use of information on staggered grid points. Using the same iterative solver, a centred difference discretisation that operates exclusively on the regular grid serves as a reference. The reprise of the ISMIP-HOM experiments indicates that both discretisations are capable of reproducing the higher-order model inter-comparison results. This setup allows a direct comparison of the two numerical implementations also with respect to their convergence behaviour. First and foremost, the new finite difference scheme facilitates convergence by a factor of up to 7 and 2.6 in average. In addition to this decrease in computational costs, the accuracy for the resultant velocity field can be chosen higher in the novel finite difference implementation. Changing the discretisation also prevents build-up of local field irregularites that occasionally cause divergence of the solution for the reference discretisation. The improved behaviour makes the new discretisation more reliable for extensive application to real ice geometries. Higher accuracy and robust numerics are crucial in time dependent applications since numerical oscillations in the velocity field of subsequent time steps are attenuated and divergence of the solution is prevented.
format Article in Journal/Newspaper
author J. J. Fürst
O. Rybak
H. Goelzer
B. De Smedt
P. de Groen
P. Huybrechts
author_facet J. J. Fürst
O. Rybak
H. Goelzer
B. De Smedt
P. de Groen
P. Huybrechts
author_sort J. J. Fürst
title Improved convergence and stability properties in a three-dimensional higher-order ice sheet model
title_short Improved convergence and stability properties in a three-dimensional higher-order ice sheet model
title_full Improved convergence and stability properties in a three-dimensional higher-order ice sheet model
title_fullStr Improved convergence and stability properties in a three-dimensional higher-order ice sheet model
title_full_unstemmed Improved convergence and stability properties in a three-dimensional higher-order ice sheet model
title_sort improved convergence and stability properties in a three-dimensional higher-order ice sheet model
publisher Copernicus Publications
publishDate 2011
url https://doi.org/10.5194/gmd-4-1133-2011
https://doaj.org/article/b5353d9d1faf482aa5c39b40bfa94356
genre Ice Sheet
genre_facet Ice Sheet
op_source Geoscientific Model Development, Vol 4, Iss 4, Pp 1133-1149 (2011)
op_relation http://www.geosci-model-dev.net/4/1133/2011/gmd-4-1133-2011.pdf
https://doaj.org/toc/1991-959X
https://doaj.org/toc/1991-9603
doi:10.5194/gmd-4-1133-2011
1991-959X
1991-9603
https://doaj.org/article/b5353d9d1faf482aa5c39b40bfa94356
op_doi https://doi.org/10.5194/gmd-4-1133-2011
container_title Geoscientific Model Development
container_volume 4
container_issue 4
container_start_page 1133
op_container_end_page 1149
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