A dynamical core based on a discontinuous Galerkin method for higher-order finite-element sea ice modeling

The ability of numerical sea ice models to reproduce localized deformation features associated with fracture processes is key for an accurate representation of the ice dynamics and of dynamically coupled physical processes in the Arctic and Antarctic. Equally key is the capacity of these models to m...

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Published in:Geoscientific Model Development
Main Authors: Richter, Thomas, Dansereau, Véronique, Lessig, Christian, Minakowski, Piotr
Format: Text
Language:English
Published: 2023
Subjects:
Online Access:https://doi.org/10.5194/gmd-16-3907-2023
https://gmd.copernicus.org/articles/16/3907/2023/
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spelling ftcopernicus:oai:publications.copernicus.org:gmd109989 2023-07-30T03:58:19+02:00 A dynamical core based on a discontinuous Galerkin method for higher-order finite-element sea ice modeling Richter, Thomas Dansereau, Véronique Lessig, Christian Minakowski, Piotr 2023-07-13 application/pdf https://doi.org/10.5194/gmd-16-3907-2023 https://gmd.copernicus.org/articles/16/3907/2023/ eng eng doi:10.5194/gmd-16-3907-2023 https://gmd.copernicus.org/articles/16/3907/2023/ eISSN: 1991-9603 Text 2023 ftcopernicus https://doi.org/10.5194/gmd-16-3907-2023 2023-07-17T16:24:17Z The ability of numerical sea ice models to reproduce localized deformation features associated with fracture processes is key for an accurate representation of the ice dynamics and of dynamically coupled physical processes in the Arctic and Antarctic. Equally key is the capacity of these models to minimize the numerical diffusion stemming from the advection of these features to ensure that the associated strong gradients persist in time, without the need to unphysically re-inject energy for re-localization. To control diffusion and improve the approximation quality, we present a new numerical core for the dynamics of sea ice that is based on higher-order finite-element discretizations for the momentum equation and higher-order discontinuous Galerkin methods for the advection. The mathematical properties of this core are discussed, and a detailed description of an efficient shared-memory parallel implementation is given. In addition, we present different numerical tests and apply the new framework to a benchmark problem to quantify the advantages of the higher-order discretization. These tests are based on Hibler's viscous–plastic sea ice model, but the implementation of the developed framework in the context of other physical models reproducing a strong localization of the deformation is possible. Text Antarc* Antarctic Arctic Sea ice Copernicus Publications: E-Journals Arctic Antarctic Geoscientific Model Development 16 13 3907 3926
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description The ability of numerical sea ice models to reproduce localized deformation features associated with fracture processes is key for an accurate representation of the ice dynamics and of dynamically coupled physical processes in the Arctic and Antarctic. Equally key is the capacity of these models to minimize the numerical diffusion stemming from the advection of these features to ensure that the associated strong gradients persist in time, without the need to unphysically re-inject energy for re-localization. To control diffusion and improve the approximation quality, we present a new numerical core for the dynamics of sea ice that is based on higher-order finite-element discretizations for the momentum equation and higher-order discontinuous Galerkin methods for the advection. The mathematical properties of this core are discussed, and a detailed description of an efficient shared-memory parallel implementation is given. In addition, we present different numerical tests and apply the new framework to a benchmark problem to quantify the advantages of the higher-order discretization. These tests are based on Hibler's viscous–plastic sea ice model, but the implementation of the developed framework in the context of other physical models reproducing a strong localization of the deformation is possible.
format Text
author Richter, Thomas
Dansereau, Véronique
Lessig, Christian
Minakowski, Piotr
spellingShingle Richter, Thomas
Dansereau, Véronique
Lessig, Christian
Minakowski, Piotr
A dynamical core based on a discontinuous Galerkin method for higher-order finite-element sea ice modeling
author_facet Richter, Thomas
Dansereau, Véronique
Lessig, Christian
Minakowski, Piotr
author_sort Richter, Thomas
title A dynamical core based on a discontinuous Galerkin method for higher-order finite-element sea ice modeling
title_short A dynamical core based on a discontinuous Galerkin method for higher-order finite-element sea ice modeling
title_full A dynamical core based on a discontinuous Galerkin method for higher-order finite-element sea ice modeling
title_fullStr A dynamical core based on a discontinuous Galerkin method for higher-order finite-element sea ice modeling
title_full_unstemmed A dynamical core based on a discontinuous Galerkin method for higher-order finite-element sea ice modeling
title_sort dynamical core based on a discontinuous galerkin method for higher-order finite-element sea ice modeling
publishDate 2023
url https://doi.org/10.5194/gmd-16-3907-2023
https://gmd.copernicus.org/articles/16/3907/2023/
geographic Arctic
Antarctic
geographic_facet Arctic
Antarctic
genre Antarc*
Antarctic
Arctic
Sea ice
genre_facet Antarc*
Antarctic
Arctic
Sea ice
op_source eISSN: 1991-9603
op_relation doi:10.5194/gmd-16-3907-2023
https://gmd.copernicus.org/articles/16/3907/2023/
op_doi https://doi.org/10.5194/gmd-16-3907-2023
container_title Geoscientific Model Development
container_volume 16
container_issue 13
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op_container_end_page 3926
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