On exact solutions and numerics for cold, shallow, and thermocoupled ice sheets ...

This three section report can be regarded as an extended appendix to (Bueler, Brown, and Lingle 2006). First we give the detailed construction of an exact solution to a standard continuum model of a cold, shallow, and thermocoupled ice sheet. The construction is by calculation of compensatory accumu...

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Main Authors: Bueler, Ed, Brown, Jed
Format: Text
Language:unknown
Published: arXiv 2006
Subjects:
Online Access:https://dx.doi.org/10.48550/arxiv.physics/0610106
https://arxiv.org/abs/physics/0610106
id ftdatacite:10.48550/arxiv.physics/0610106
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spelling ftdatacite:10.48550/arxiv.physics/0610106 2023-10-01T03:56:42+02:00 On exact solutions and numerics for cold, shallow, and thermocoupled ice sheets ... Bueler, Ed Brown, Jed 2006 https://dx.doi.org/10.48550/arxiv.physics/0610106 https://arxiv.org/abs/physics/0610106 unknown arXiv https://dx.doi.org/10.3189/002214307783258396 Assumed arXiv.org perpetual, non-exclusive license to distribute this article for submissions made before January 2004 http://arxiv.org/licenses/assumed-1991-2003/ Geophysics physics.geo-ph Computational Physics physics.comp-ph Fluid Dynamics physics.flu-dyn FOS Physical sciences ScholarlyArticle Article article-journal Text 2006 ftdatacite https://doi.org/10.48550/arxiv.physics/061010610.3189/002214307783258396 2023-09-04T14:01:24Z This three section report can be regarded as an extended appendix to (Bueler, Brown, and Lingle 2006). First we give the detailed construction of an exact solution to a standard continuum model of a cold, shallow, and thermocoupled ice sheet. The construction is by calculation of compensatory accumulation and heat source functions which make a chosen pair of functions for thickness and temperature into exact solutions of the coupled system. The solution we construct here is ``TestG'' in (Bueler and others, 2006) and the steady state solution ``Test F'' is a special case. In the second section we give a reference C implementation of these exact solutions. In the last section we give an error analysis of a finite difference scheme for the temperature equation in the thermocoupled model. The error analysis gives three results, first the correct form of the Courant-Friedrichs-Lewy (CFL) condition for stability of the advection scheme, second an equation for error growth which contributes to understanding the ... : 16 pages, two C codes; extended appendix to Bueler, Brown, and Lingle, "Exact solutions to the thermocoupled shallow ice approximation: effective tools for verification," submitted to J. Glaciol ... 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 Geophysics physics.geo-ph
Computational Physics physics.comp-ph
Fluid Dynamics physics.flu-dyn
FOS Physical sciences
spellingShingle Geophysics physics.geo-ph
Computational Physics physics.comp-ph
Fluid Dynamics physics.flu-dyn
FOS Physical sciences
Bueler, Ed
Brown, Jed
On exact solutions and numerics for cold, shallow, and thermocoupled ice sheets ...
topic_facet Geophysics physics.geo-ph
Computational Physics physics.comp-ph
Fluid Dynamics physics.flu-dyn
FOS Physical sciences
description This three section report can be regarded as an extended appendix to (Bueler, Brown, and Lingle 2006). First we give the detailed construction of an exact solution to a standard continuum model of a cold, shallow, and thermocoupled ice sheet. The construction is by calculation of compensatory accumulation and heat source functions which make a chosen pair of functions for thickness and temperature into exact solutions of the coupled system. The solution we construct here is ``TestG'' in (Bueler and others, 2006) and the steady state solution ``Test F'' is a special case. In the second section we give a reference C implementation of these exact solutions. In the last section we give an error analysis of a finite difference scheme for the temperature equation in the thermocoupled model. The error analysis gives three results, first the correct form of the Courant-Friedrichs-Lewy (CFL) condition for stability of the advection scheme, second an equation for error growth which contributes to understanding the ... : 16 pages, two C codes; extended appendix to Bueler, Brown, and Lingle, "Exact solutions to the thermocoupled shallow ice approximation: effective tools for verification," submitted to J. Glaciol ...
format Text
author Bueler, Ed
Brown, Jed
author_facet Bueler, Ed
Brown, Jed
author_sort Bueler, Ed
title On exact solutions and numerics for cold, shallow, and thermocoupled ice sheets ...
title_short On exact solutions and numerics for cold, shallow, and thermocoupled ice sheets ...
title_full On exact solutions and numerics for cold, shallow, and thermocoupled ice sheets ...
title_fullStr On exact solutions and numerics for cold, shallow, and thermocoupled ice sheets ...
title_full_unstemmed On exact solutions and numerics for cold, shallow, and thermocoupled ice sheets ...
title_sort on exact solutions and numerics for cold, shallow, and thermocoupled ice sheets ...
publisher arXiv
publishDate 2006
url https://dx.doi.org/10.48550/arxiv.physics/0610106
https://arxiv.org/abs/physics/0610106
genre Ice Sheet
genre_facet Ice Sheet
op_relation https://dx.doi.org/10.3189/002214307783258396
op_rights Assumed arXiv.org perpetual, non-exclusive license to distribute this article for submissions made before January 2004
http://arxiv.org/licenses/assumed-1991-2003/
op_doi https://doi.org/10.48550/arxiv.physics/061010610.3189/002214307783258396
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