Performance analysis of high-resolution ice-sheet simulations

Abstract Numerical glacier and ice-sheet models compute evolving ice geometry and velocity fields using various stress-balance approximations and boundary conditions. At high spatial resolution, with horizontal mesh/grid resolutions of a few kilometers or smaller, these models usually require time s...

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Bibliographic Details
Published in:Journal of Glaciology
Main Author: Bueler, Ed
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2022
Subjects:
Online Access:http://dx.doi.org/10.1017/jog.2022.113
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143022001137
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spelling crcambridgeupr:10.1017/jog.2022.113 2024-03-03T08:45:25+00:00 Performance analysis of high-resolution ice-sheet simulations Bueler, Ed 2022 http://dx.doi.org/10.1017/jog.2022.113 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143022001137 en eng Cambridge University Press (CUP) http://creativecommons.org/licenses/by/4.0/ Journal of Glaciology volume 69, issue 276, page 930-935 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 2022 crcambridgeupr https://doi.org/10.1017/jog.2022.113 2024-02-08T08:32:51Z Abstract Numerical glacier and ice-sheet models compute evolving ice geometry and velocity fields using various stress-balance approximations and boundary conditions. At high spatial resolution, with horizontal mesh/grid resolutions of a few kilometers or smaller, these models usually require time steps shorter than climate-coupling time scales because they update ice thickness after each velocity solution. High-resolution performance is degraded by the stability restrictions of such explicit time-stepping. This short note, which considers the shallow ice approximation and Stokes models as stress-balance end members, clarifies the scaling of numerical model performance by quantifying simulation cost per model year in terms of mesh resolution and the number of degrees of freedom. The performance of current-generation explicit time-stepping models is assessed, and then compared to the prospective performance of implicit schemes. The main results highlight the key roles played by the algorithmic scaling of stress-balance solvers and coupled, implicit-step solvers. Article in Journal/Newspaper Ice Sheet Journal of Glaciology Cambridge University Press Journal of Glaciology 1 6
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Bueler, Ed
Performance analysis of high-resolution ice-sheet simulations
topic_facet Earth-Surface Processes
description Abstract Numerical glacier and ice-sheet models compute evolving ice geometry and velocity fields using various stress-balance approximations and boundary conditions. At high spatial resolution, with horizontal mesh/grid resolutions of a few kilometers or smaller, these models usually require time steps shorter than climate-coupling time scales because they update ice thickness after each velocity solution. High-resolution performance is degraded by the stability restrictions of such explicit time-stepping. This short note, which considers the shallow ice approximation and Stokes models as stress-balance end members, clarifies the scaling of numerical model performance by quantifying simulation cost per model year in terms of mesh resolution and the number of degrees of freedom. The performance of current-generation explicit time-stepping models is assessed, and then compared to the prospective performance of implicit schemes. The main results highlight the key roles played by the algorithmic scaling of stress-balance solvers and coupled, implicit-step solvers.
format Article in Journal/Newspaper
author Bueler, Ed
author_facet Bueler, Ed
author_sort Bueler, Ed
title Performance analysis of high-resolution ice-sheet simulations
title_short Performance analysis of high-resolution ice-sheet simulations
title_full Performance analysis of high-resolution ice-sheet simulations
title_fullStr Performance analysis of high-resolution ice-sheet simulations
title_full_unstemmed Performance analysis of high-resolution ice-sheet simulations
title_sort performance analysis of high-resolution ice-sheet simulations
publisher Cambridge University Press (CUP)
publishDate 2022
url http://dx.doi.org/10.1017/jog.2022.113
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143022001137
genre Ice Sheet
Journal of Glaciology
genre_facet Ice Sheet
Journal of Glaciology
op_source Journal of Glaciology
volume 69, issue 276, page 930-935
ISSN 0022-1430 1727-5652
op_rights http://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.1017/jog.2022.113
container_title Journal of Glaciology
container_start_page 1
op_container_end_page 6
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