Coupled models and parallel simulations for three-dimensional full-Stokes ice sheet modeling

A three-dimensional full-Stokes computational model is considered for determining the dynamics, temperature, and thickness of ice sheets. The governing thermomechanical equations consist of the three-dimensional full-Stokes system with nonlinear rheology for the momentum, an advective-diffusion ener...

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Published in:Numerical Mathematics: Theory, Methods and Applications
Main Authors: Zhang, Huai, Ju, Lili, Gunzburger, Max, Ringler, Todd, Price, Stephen
Other Authors: United States. Department of Energy., United States. Department of Energy. Office of Biological and Environmental Research.
Format: Article in Journal/Newspaper
Language:English
Published: University of South Carolina 2011
Subjects:
Online Access:https://doi.org/10.4208/nmtma.2011.m1031
https://digital.library.unt.edu/ark:/67531/metadc842422/
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author Zhang, Huai
Ju, Lili
Gunzburger, Max
Ringler, Todd
Price, Stephen
author2 United States. Department of Energy.
United States. Department of Energy. Office of Biological and Environmental Research.
author_facet Zhang, Huai
Ju, Lili
Gunzburger, Max
Ringler, Todd
Price, Stephen
author_sort Zhang, Huai
collection University of North Texas: UNT Digital Library
container_issue 3
container_start_page 396
container_title Numerical Mathematics: Theory, Methods and Applications
container_volume 4
description A three-dimensional full-Stokes computational model is considered for determining the dynamics, temperature, and thickness of ice sheets. The governing thermomechanical equations consist of the three-dimensional full-Stokes system with nonlinear rheology for the momentum, an advective-diffusion energy equation for temperature evolution, and a mass conservation equation for icethickness changes. Here, we discuss the variable resolution meshes, the finite element discretizations, and the parallel algorithms employed by the model components. The solvers are integrated through a well-designed coupler for the exchange of parametric data between components. The discretization utilizes high-quality, variable-resolution centroidal Voronoi Delaunay triangulation meshing and existing parallel solvers. We demonstrate the gridding technology, discretization schemes, and the efficiency and scalability of the parallel solvers through computational experiments using both simplified geometries arising from benchmark test problems and a realistic Greenland ice sheet geometry.
format Article in Journal/Newspaper
genre Greenland
Ice Sheet
genre_facet Greenland
Ice Sheet
geographic Greenland
geographic_facet Greenland
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op_doi https://doi.org/10.4208/nmtma.2011.m1031
op_relation rep-no: DOE/FG/ER64431-4
grantno: FG02-07ER64431
doi:10.4208/nmtma.2011.m1031
osti: 1090857
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op_source Journal Name: Numerical Mathematics: Theory, Methods and Applications; Journal Volume: 4
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spelling ftunivnotexas:info:ark/67531/metadc842422 2025-01-16T22:12:01+00:00 Coupled models and parallel simulations for three-dimensional full-Stokes ice sheet modeling Zhang, Huai Ju, Lili Gunzburger, Max Ringler, Todd Price, Stephen United States. Department of Energy. United States. Department of Energy. Office of Biological and Environmental Research. 2011-01-01 359-381 Text https://doi.org/10.4208/nmtma.2011.m1031 https://digital.library.unt.edu/ark:/67531/metadc842422/ English eng University of South Carolina rep-no: DOE/FG/ER64431-4 grantno: FG02-07ER64431 doi:10.4208/nmtma.2011.m1031 osti: 1090857 https://digital.library.unt.edu/ark:/67531/metadc842422/ ark: ark:/67531/metadc842422 Journal Name: Numerical Mathematics: Theory, Methods and Applications; Journal Volume: 4 Ice Sheet Modeling Nonlinear Stokes Equation Finite Element Method Parallel Implementation 97 Mathematics And Computing Ice Sheet Modeling 58 Geosciences Article 2011 ftunivnotexas https://doi.org/10.4208/nmtma.2011.m1031 2018-03-17T23:08:07Z A three-dimensional full-Stokes computational model is considered for determining the dynamics, temperature, and thickness of ice sheets. The governing thermomechanical equations consist of the three-dimensional full-Stokes system with nonlinear rheology for the momentum, an advective-diffusion energy equation for temperature evolution, and a mass conservation equation for icethickness changes. Here, we discuss the variable resolution meshes, the finite element discretizations, and the parallel algorithms employed by the model components. The solvers are integrated through a well-designed coupler for the exchange of parametric data between components. The discretization utilizes high-quality, variable-resolution centroidal Voronoi Delaunay triangulation meshing and existing parallel solvers. We demonstrate the gridding technology, discretization schemes, and the efficiency and scalability of the parallel solvers through computational experiments using both simplified geometries arising from benchmark test problems and a realistic Greenland ice sheet geometry. Article in Journal/Newspaper Greenland Ice Sheet University of North Texas: UNT Digital Library Greenland Numerical Mathematics: Theory, Methods and Applications 4 3 396 418
spellingShingle Ice Sheet Modeling
Nonlinear Stokes Equation
Finite Element Method
Parallel Implementation
97 Mathematics And Computing Ice Sheet Modeling
58 Geosciences
Zhang, Huai
Ju, Lili
Gunzburger, Max
Ringler, Todd
Price, Stephen
Coupled models and parallel simulations for three-dimensional full-Stokes ice sheet modeling
title Coupled models and parallel simulations for three-dimensional full-Stokes ice sheet modeling
title_full Coupled models and parallel simulations for three-dimensional full-Stokes ice sheet modeling
title_fullStr Coupled models and parallel simulations for three-dimensional full-Stokes ice sheet modeling
title_full_unstemmed Coupled models and parallel simulations for three-dimensional full-Stokes ice sheet modeling
title_short Coupled models and parallel simulations for three-dimensional full-Stokes ice sheet modeling
title_sort coupled models and parallel simulations for three-dimensional full-stokes ice sheet modeling
topic Ice Sheet Modeling
Nonlinear Stokes Equation
Finite Element Method
Parallel Implementation
97 Mathematics And Computing Ice Sheet Modeling
58 Geosciences
topic_facet Ice Sheet Modeling
Nonlinear Stokes Equation
Finite Element Method
Parallel Implementation
97 Mathematics And Computing Ice Sheet Modeling
58 Geosciences
url https://doi.org/10.4208/nmtma.2011.m1031
https://digital.library.unt.edu/ark:/67531/metadc842422/