The neXtSIM-DG dynamical core: A Framework 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...

Full description

Bibliographic Details
Main Authors: Richter, Thomas, Dansereau, Véronique, Lessig, Christian, Minakowski, Piotr
Format: Text
Language:English
Published: 2023
Subjects:
Online Access:https://doi.org/10.5194/egusphere-2023-391
https://egusphere.copernicus.org/preprints/2023/egusphere-2023-391/
id ftcopernicus:oai:publications.copernicus.org:egusphere109989
record_format openpolar
spelling ftcopernicus:oai:publications.copernicus.org:egusphere109989 2023-07-30T03:58:34+02:00 The neXtSIM-DG dynamical core: A Framework 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/egusphere-2023-391 https://egusphere.copernicus.org/preprints/2023/egusphere-2023-391/ eng eng doi:10.5194/egusphere-2023-391 https://egusphere.copernicus.org/preprints/2023/egusphere-2023-391/ eISSN: Text 2023 ftcopernicus https://doi.org/10.5194/egusphere-2023-391 2023-07-17T16:24:18Z 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
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
The neXtSIM-DG dynamical core: A Framework for Higher-order Finite Element Sea Ice Modeling
author_facet Richter, Thomas
Dansereau, Véronique
Lessig, Christian
Minakowski, Piotr
author_sort Richter, Thomas
title The neXtSIM-DG dynamical core: A Framework for Higher-order Finite Element Sea Ice Modeling
title_short The neXtSIM-DG dynamical core: A Framework for Higher-order Finite Element Sea Ice Modeling
title_full The neXtSIM-DG dynamical core: A Framework for Higher-order Finite Element Sea Ice Modeling
title_fullStr The neXtSIM-DG dynamical core: A Framework for Higher-order Finite Element Sea Ice Modeling
title_full_unstemmed The neXtSIM-DG dynamical core: A Framework for Higher-order Finite Element Sea Ice Modeling
title_sort nextsim-dg dynamical core: a framework for higher-order finite element sea ice modeling
publishDate 2023
url https://doi.org/10.5194/egusphere-2023-391
https://egusphere.copernicus.org/preprints/2023/egusphere-2023-391/
geographic Arctic
Antarctic
geographic_facet Arctic
Antarctic
genre Antarc*
Antarctic
Arctic
Sea ice
genre_facet Antarc*
Antarctic
Arctic
Sea ice
op_source eISSN:
op_relation doi:10.5194/egusphere-2023-391
https://egusphere.copernicus.org/preprints/2023/egusphere-2023-391/
op_doi https://doi.org/10.5194/egusphere-2023-391
_version_ 1772821335781670912