Manufactured analytical solutions for isothermal full-Stokes ice sheet models

We present the detailed construction of a manufactured analytical solution to time-dependent and steady-state isothermal full-Stokes ice sheet problems. The solutions are constructed for two-dimensional flowline and three-dimensional full-Stokes ice sheet models with variable viscosity. The construc...

Full description

Bibliographic Details
Published in:The Cryosphere
Main Authors: A. Sargent, J. L. Fastook
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2010
Subjects:
geo
Online Access:https://doi.org/10.5194/tc-4-285-2010
http://www.the-cryosphere.net/4/285/2010/tc-4-285-2010.pdf
https://doaj.org/article/442622419e56465f978f23e45a92ba04
id fttriple:oai:gotriple.eu:oai:doaj.org/article:442622419e56465f978f23e45a92ba04
record_format openpolar
spelling fttriple:oai:gotriple.eu:oai:doaj.org/article:442622419e56465f978f23e45a92ba04 2023-05-15T16:40:17+02:00 Manufactured analytical solutions for isothermal full-Stokes ice sheet models A. Sargent J. L. Fastook 2010-08-01 https://doi.org/10.5194/tc-4-285-2010 http://www.the-cryosphere.net/4/285/2010/tc-4-285-2010.pdf https://doaj.org/article/442622419e56465f978f23e45a92ba04 en eng Copernicus Publications doi:10.5194/tc-4-285-2010 1994-0416 1994-0424 http://www.the-cryosphere.net/4/285/2010/tc-4-285-2010.pdf https://doaj.org/article/442622419e56465f978f23e45a92ba04 undefined The Cryosphere, Vol 4, Iss 3, Pp 285-311 (2010) geo envir Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2010 fttriple https://doi.org/10.5194/tc-4-285-2010 2023-01-22T19:13:37Z We present the detailed construction of a manufactured analytical solution to time-dependent and steady-state isothermal full-Stokes ice sheet problems. The solutions are constructed for two-dimensional flowline and three-dimensional full-Stokes ice sheet models with variable viscosity. The construction is done by choosing for the specified ice surface and bed a velocity distribution that satisfies both mass conservation and the kinematic boundary conditions. Then a compensatory stress term in the conservation of momentum equations and their boundary conditions is calculated to make the chosen velocity distributions as well as the chosen pressure field into exact solutions. By substituting different ice surface and bed geometry formulas into the derived solution formulas, analytical solutions for different geometries can be constructed. The boundary conditions can be specified as essential Dirichlet conditions or as periodic boundary conditions. By changing a parameter value, the analytical solutions allow investigation of algorithms for a different range of aspect ratios as well as for different, frozen or sliding, basal conditions. The analytical solutions can also be used to estimate the numerical error of the method in the case when the effects of the boundary conditions are eliminated, that is, when the exact solution values are specified as inflow and outflow boundary conditions. Article in Journal/Newspaper Ice Sheet The Cryosphere Unknown The Cryosphere 4 3 285 311
institution Open Polar
collection Unknown
op_collection_id fttriple
language English
topic geo
envir
spellingShingle geo
envir
A. Sargent
J. L. Fastook
Manufactured analytical solutions for isothermal full-Stokes ice sheet models
topic_facet geo
envir
description We present the detailed construction of a manufactured analytical solution to time-dependent and steady-state isothermal full-Stokes ice sheet problems. The solutions are constructed for two-dimensional flowline and three-dimensional full-Stokes ice sheet models with variable viscosity. The construction is done by choosing for the specified ice surface and bed a velocity distribution that satisfies both mass conservation and the kinematic boundary conditions. Then a compensatory stress term in the conservation of momentum equations and their boundary conditions is calculated to make the chosen velocity distributions as well as the chosen pressure field into exact solutions. By substituting different ice surface and bed geometry formulas into the derived solution formulas, analytical solutions for different geometries can be constructed. The boundary conditions can be specified as essential Dirichlet conditions or as periodic boundary conditions. By changing a parameter value, the analytical solutions allow investigation of algorithms for a different range of aspect ratios as well as for different, frozen or sliding, basal conditions. The analytical solutions can also be used to estimate the numerical error of the method in the case when the effects of the boundary conditions are eliminated, that is, when the exact solution values are specified as inflow and outflow boundary conditions.
format Article in Journal/Newspaper
author A. Sargent
J. L. Fastook
author_facet A. Sargent
J. L. Fastook
author_sort A. Sargent
title Manufactured analytical solutions for isothermal full-Stokes ice sheet models
title_short Manufactured analytical solutions for isothermal full-Stokes ice sheet models
title_full Manufactured analytical solutions for isothermal full-Stokes ice sheet models
title_fullStr Manufactured analytical solutions for isothermal full-Stokes ice sheet models
title_full_unstemmed Manufactured analytical solutions for isothermal full-Stokes ice sheet models
title_sort manufactured analytical solutions for isothermal full-stokes ice sheet models
publisher Copernicus Publications
publishDate 2010
url https://doi.org/10.5194/tc-4-285-2010
http://www.the-cryosphere.net/4/285/2010/tc-4-285-2010.pdf
https://doaj.org/article/442622419e56465f978f23e45a92ba04
genre Ice Sheet
The Cryosphere
genre_facet Ice Sheet
The Cryosphere
op_source The Cryosphere, Vol 4, Iss 3, Pp 285-311 (2010)
op_relation doi:10.5194/tc-4-285-2010
1994-0416
1994-0424
http://www.the-cryosphere.net/4/285/2010/tc-4-285-2010.pdf
https://doaj.org/article/442622419e56465f978f23e45a92ba04
op_rights undefined
op_doi https://doi.org/10.5194/tc-4-285-2010
container_title The Cryosphere
container_volume 4
container_issue 3
container_start_page 285
op_container_end_page 311
_version_ 1766030671855222784