Performance analysis of high-resolution ice-sheet simulations

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 shor...

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Bibliographic Details
Published in:Journal of Glaciology
Main Author: Ed Bueler
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press 2023
Subjects:
Online Access:https://doi.org/10.1017/jog.2022.113
https://doaj.org/article/2fb1f68be37f445da3ab3cf226b62eb3
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spelling ftdoajarticles:oai:doaj.org/article:2fb1f68be37f445da3ab3cf226b62eb3 2023-08-20T04:07:14+02:00 Performance analysis of high-resolution ice-sheet simulations Ed Bueler 2023-08-01T00:00:00Z https://doi.org/10.1017/jog.2022.113 https://doaj.org/article/2fb1f68be37f445da3ab3cf226b62eb3 EN eng Cambridge University Press https://www.cambridge.org/core/product/identifier/S0022143022001137/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2022.113 0022-1430 1727-5652 https://doaj.org/article/2fb1f68be37f445da3ab3cf226b62eb3 Journal of Glaciology, Vol 69, Pp 930-935 (2023) Glacier flow glacier modeling ice-sheet modeling Environmental sciences GE1-350 Meteorology. Climatology QC851-999 article 2023 ftdoajarticles https://doi.org/10.1017/jog.2022.113 2023-07-30T00:36:44Z 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 Directory of Open Access Journals: DOAJ Articles Journal of Glaciology 1 6
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Glacier flow
glacier modeling
ice-sheet modeling
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
spellingShingle Glacier flow
glacier modeling
ice-sheet modeling
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
Ed Bueler
Performance analysis of high-resolution ice-sheet simulations
topic_facet Glacier flow
glacier modeling
ice-sheet modeling
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
description 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 Ed Bueler
author_facet Ed Bueler
author_sort Ed Bueler
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
publishDate 2023
url https://doi.org/10.1017/jog.2022.113
https://doaj.org/article/2fb1f68be37f445da3ab3cf226b62eb3
genre Ice Sheet
Journal of Glaciology
genre_facet Ice Sheet
Journal of Glaciology
op_source Journal of Glaciology, Vol 69, Pp 930-935 (2023)
op_relation https://www.cambridge.org/core/product/identifier/S0022143022001137/type/journal_article
https://doaj.org/toc/0022-1430
https://doaj.org/toc/1727-5652
doi:10.1017/jog.2022.113
0022-1430
1727-5652
https://doaj.org/article/2fb1f68be37f445da3ab3cf226b62eb3
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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