A leading-order viscoelastic model for crevasse propagation and calving in ice shelves

We use a leading-order viscoelastic model for crevasse evolution, in which a purely viscous model for the deformation of the domain couples with linear elastic fracture mechanics models through a viscous pre-stress. The fracture mechanics model conversely couples with the viscous model by inserting...

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Main Authors: Zarrinderakht, Maryam, Schoof, Christian, Zwinger, Thomas
Format: Text
Language:English
Published: 2023
Subjects:
Online Access:https://doi.org/10.5194/egusphere-2023-807
https://egusphere.copernicus.org/preprints/2023/egusphere-2023-807/
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spelling ftcopernicus:oai:publications.copernicus.org:egusphere111076 2023-07-02T03:32:36+02:00 A leading-order viscoelastic model for crevasse propagation and calving in ice shelves Zarrinderakht, Maryam Schoof, Christian Zwinger, Thomas 2023-06-08 application/pdf https://doi.org/10.5194/egusphere-2023-807 https://egusphere.copernicus.org/preprints/2023/egusphere-2023-807/ eng eng doi:10.5194/egusphere-2023-807 https://egusphere.copernicus.org/preprints/2023/egusphere-2023-807/ eISSN: Text 2023 ftcopernicus https://doi.org/10.5194/egusphere-2023-807 2023-06-12T16:24:16Z We use a leading-order viscoelastic model for crevasse evolution, in which a purely viscous model for the deformation of the domain couples with linear elastic fracture mechanics models through a viscous pre-stress. The fracture mechanics model conversely couples with the viscous model by inserting cracks into the domain, which viscous flow subsequently pulls apart. By contrast with prior work, we solve the fracture mechanics problem on the actual domain geometry using a boundary element method, coupled with a finite element solution of the Stokes equations describing the viscous flow. We study a periodic array of surface and basal crevasses on an ice shelf being stretched at a prescribed rate. We find that calving can either occur instantly for large enough stretching rates or sufficiently high surface water levels or through feedbacks between partial fracture propagation and subsequent viscous deformation and adjustment of the viscous pre-stress acting on crack faces. Our results show that purely stress-based calving laws cannot robustly describe the process of calving, since they cannot account for the gradual evolution of local crevasse and surface geometry, which can be understood at the large scale as being more akin to the evolution of a damage variable. Future work will need to coarse-grain the type of process model we describe here in order to make it applicable to ice sheet simulations. Text Ice Sheet Ice Shelf Ice Shelves Copernicus Publications: E-Journals
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description We use a leading-order viscoelastic model for crevasse evolution, in which a purely viscous model for the deformation of the domain couples with linear elastic fracture mechanics models through a viscous pre-stress. The fracture mechanics model conversely couples with the viscous model by inserting cracks into the domain, which viscous flow subsequently pulls apart. By contrast with prior work, we solve the fracture mechanics problem on the actual domain geometry using a boundary element method, coupled with a finite element solution of the Stokes equations describing the viscous flow. We study a periodic array of surface and basal crevasses on an ice shelf being stretched at a prescribed rate. We find that calving can either occur instantly for large enough stretching rates or sufficiently high surface water levels or through feedbacks between partial fracture propagation and subsequent viscous deformation and adjustment of the viscous pre-stress acting on crack faces. Our results show that purely stress-based calving laws cannot robustly describe the process of calving, since they cannot account for the gradual evolution of local crevasse and surface geometry, which can be understood at the large scale as being more akin to the evolution of a damage variable. Future work will need to coarse-grain the type of process model we describe here in order to make it applicable to ice sheet simulations.
format Text
author Zarrinderakht, Maryam
Schoof, Christian
Zwinger, Thomas
spellingShingle Zarrinderakht, Maryam
Schoof, Christian
Zwinger, Thomas
A leading-order viscoelastic model for crevasse propagation and calving in ice shelves
author_facet Zarrinderakht, Maryam
Schoof, Christian
Zwinger, Thomas
author_sort Zarrinderakht, Maryam
title A leading-order viscoelastic model for crevasse propagation and calving in ice shelves
title_short A leading-order viscoelastic model for crevasse propagation and calving in ice shelves
title_full A leading-order viscoelastic model for crevasse propagation and calving in ice shelves
title_fullStr A leading-order viscoelastic model for crevasse propagation and calving in ice shelves
title_full_unstemmed A leading-order viscoelastic model for crevasse propagation and calving in ice shelves
title_sort leading-order viscoelastic model for crevasse propagation and calving in ice shelves
publishDate 2023
url https://doi.org/10.5194/egusphere-2023-807
https://egusphere.copernicus.org/preprints/2023/egusphere-2023-807/
genre Ice Sheet
Ice Shelf
Ice Shelves
genre_facet Ice Sheet
Ice Shelf
Ice Shelves
op_source eISSN:
op_relation doi:10.5194/egusphere-2023-807
https://egusphere.copernicus.org/preprints/2023/egusphere-2023-807/
op_doi https://doi.org/10.5194/egusphere-2023-807
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