Simulating Sea‐Ice Deformation in Viscous‐Plastic Sea‐Ice Models With CD‐Grids

Abstract Linear kinematic features (LKFs) are found everywhere in the Arctic sea‐ice cover. They are strongly localized deformations often associated with the formation of leads and pressure ridges. In viscous‐plastic (VP) sea‐ice models, the simulation of LKFs depends on several factors such as the...

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Published in:Journal of Advances in Modeling Earth Systems
Main Authors: C. Mehlmann, G. Capodaglio, S. Danilov
Format: Article in Journal/Newspaper
Language:English
Published: American Geophysical Union (AGU) 2023
Subjects:
Online Access:https://doi.org/10.1029/2023MS003696
https://doaj.org/article/5e3bd884f6d34f12a05416cd2bc89cb0
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author C. Mehlmann
G. Capodaglio
S. Danilov
author_facet C. Mehlmann
G. Capodaglio
S. Danilov
author_sort C. Mehlmann
collection Directory of Open Access Journals: DOAJ Articles
container_issue 8
container_title Journal of Advances in Modeling Earth Systems
container_volume 15
description Abstract Linear kinematic features (LKFs) are found everywhere in the Arctic sea‐ice cover. They are strongly localized deformations often associated with the formation of leads and pressure ridges. In viscous‐plastic (VP) sea‐ice models, the simulation of LKFs depends on several factors such as the grid resolution, the numerical solver convergence, and the placement of the variables on the mesh. In this study, we compare two recently proposed discretization with a CD‐grid placement with respect to their ability to reproduce LKFs. The first (CD1) is based on a nonconforming finite element discretization, whereas the second (CD2) uses a conforming subgrid discretization. To analyze their resolution properties, we evaluate runs from different models (e.g., FESOM, MPAS) on a benchmark problem using quadrilateral, hexagonal and triangular meshes. Our findings show that the CD1 setup simulates more deformation structure than the CD2 setup. This highlights the importance of the type of spatial discretization for the simulation of LKFs. Due to the higher number of degrees of freedom, both CD‐grids resolve more LKFs than traditional A, B, and C‐grids at fixed mesh level. This is an advantage of the CD‐grid approach, as high spatial mesh resolution is needed in VP sea‐ice models to simulate LKFs.
format Article in Journal/Newspaper
genre Arctic
Sea ice
genre_facet Arctic
Sea ice
geographic Arctic
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spelling ftdoajarticles:oai:doaj.org/article:5e3bd884f6d34f12a05416cd2bc89cb0 2025-01-16T20:41:04+00:00 Simulating Sea‐Ice Deformation in Viscous‐Plastic Sea‐Ice Models With CD‐Grids C. Mehlmann G. Capodaglio S. Danilov 2023-08-01T00:00:00Z https://doi.org/10.1029/2023MS003696 https://doaj.org/article/5e3bd884f6d34f12a05416cd2bc89cb0 EN eng American Geophysical Union (AGU) https://doi.org/10.1029/2023MS003696 https://doaj.org/toc/1942-2466 1942-2466 doi:10.1029/2023MS003696 https://doaj.org/article/5e3bd884f6d34f12a05416cd2bc89cb0 Journal of Advances in Modeling Earth Systems, Vol 15, Iss 8, Pp n/a-n/a (2023) sea‐ice dynamics CD‐grids linear kinematic features nonconforming finite elements Physical geography GB3-5030 Oceanography GC1-1581 article 2023 ftdoajarticles https://doi.org/10.1029/2023MS003696 2023-09-03T00:54:21Z Abstract Linear kinematic features (LKFs) are found everywhere in the Arctic sea‐ice cover. They are strongly localized deformations often associated with the formation of leads and pressure ridges. In viscous‐plastic (VP) sea‐ice models, the simulation of LKFs depends on several factors such as the grid resolution, the numerical solver convergence, and the placement of the variables on the mesh. In this study, we compare two recently proposed discretization with a CD‐grid placement with respect to their ability to reproduce LKFs. The first (CD1) is based on a nonconforming finite element discretization, whereas the second (CD2) uses a conforming subgrid discretization. To analyze their resolution properties, we evaluate runs from different models (e.g., FESOM, MPAS) on a benchmark problem using quadrilateral, hexagonal and triangular meshes. Our findings show that the CD1 setup simulates more deformation structure than the CD2 setup. This highlights the importance of the type of spatial discretization for the simulation of LKFs. Due to the higher number of degrees of freedom, both CD‐grids resolve more LKFs than traditional A, B, and C‐grids at fixed mesh level. This is an advantage of the CD‐grid approach, as high spatial mesh resolution is needed in VP sea‐ice models to simulate LKFs. Article in Journal/Newspaper Arctic Sea ice Directory of Open Access Journals: DOAJ Articles Arctic Journal of Advances in Modeling Earth Systems 15 8
spellingShingle sea‐ice dynamics
CD‐grids
linear kinematic features
nonconforming finite elements
Physical geography
GB3-5030
Oceanography
GC1-1581
C. Mehlmann
G. Capodaglio
S. Danilov
Simulating Sea‐Ice Deformation in Viscous‐Plastic Sea‐Ice Models With CD‐Grids
title Simulating Sea‐Ice Deformation in Viscous‐Plastic Sea‐Ice Models With CD‐Grids
title_full Simulating Sea‐Ice Deformation in Viscous‐Plastic Sea‐Ice Models With CD‐Grids
title_fullStr Simulating Sea‐Ice Deformation in Viscous‐Plastic Sea‐Ice Models With CD‐Grids
title_full_unstemmed Simulating Sea‐Ice Deformation in Viscous‐Plastic Sea‐Ice Models With CD‐Grids
title_short Simulating Sea‐Ice Deformation in Viscous‐Plastic Sea‐Ice Models With CD‐Grids
title_sort simulating sea‐ice deformation in viscous‐plastic sea‐ice models with cd‐grids
topic sea‐ice dynamics
CD‐grids
linear kinematic features
nonconforming finite elements
Physical geography
GB3-5030
Oceanography
GC1-1581
topic_facet sea‐ice dynamics
CD‐grids
linear kinematic features
nonconforming finite elements
Physical geography
GB3-5030
Oceanography
GC1-1581
url https://doi.org/10.1029/2023MS003696
https://doaj.org/article/5e3bd884f6d34f12a05416cd2bc89cb0