A damage mechanics assessment of the Larsen B ice shelf prior to collapse: Toward a physically‐based calving law
Calving is a primary process of mass ablation for glaciers and ice sheets, though it still eludes a general physical law. Here, we propose a calving framework based on continuum damage mechanics coupled with the equations of viscous deformation of glacier ice. We introduce a scalar damage variable t...
Published in: | Geophysical Research Letters |
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Main Authors: | , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
eScholarship, University of California
2012
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Subjects: | |
Online Access: | https://escholarship.org/uc/item/95v6k9p4 https://escholarship.org/content/qt95v6k9p4/qt95v6k9p4.pdf https://doi.org/10.1029/2012gl053317 |
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author | Borstad, CP Khazendar, A Larour, E Morlighem, M Rignot, E Schodlok, MP Seroussi, H |
author_facet | Borstad, CP Khazendar, A Larour, E Morlighem, M Rignot, E Schodlok, MP Seroussi, H |
author_sort | Borstad, CP |
collection | University of California: eScholarship |
container_issue | 18 |
container_title | Geophysical Research Letters |
container_volume | 39 |
description | Calving is a primary process of mass ablation for glaciers and ice sheets, though it still eludes a general physical law. Here, we propose a calving framework based on continuum damage mechanics coupled with the equations of viscous deformation of glacier ice. We introduce a scalar damage variable that quantifies the loss of load-bearing surface area due to fractures and that feeds back with ice viscosity to represent fracture-induced softening. The calving law is a standard failure criterion for viscous damaging materials and represents a macroscopic brittle instability quantified by a critical or threshold damage. We constrain this threshold using the Ice Sheet System Model (ISSM) by inverting for damage on the Larsen B ice shelf prior to its 2002 collapse. By analyzing the damage distribution in areas that subsequently calved, we conclude that calving occurs after fractures have reduced the load-bearing capacity of the ice by 60 ± 10%. © 2012. American Geophysical Union. All Rights Reserved. |
format | Article in Journal/Newspaper |
genre | Ice Sheet Ice Shelf |
genre_facet | Ice Sheet Ice Shelf |
id | ftcdlib:oai:escholarship.org:ark:/13030/qt95v6k9p4 |
institution | Open Polar |
language | unknown |
op_collection_id | ftcdlib |
op_doi | https://doi.org/10.1029/2012gl053317 |
op_relation | qt95v6k9p4 https://escholarship.org/uc/item/95v6k9p4 https://escholarship.org/content/qt95v6k9p4/qt95v6k9p4.pdf doi:10.1029/2012gl053317 |
op_rights | CC-BY |
op_source | Geophysical Research Letters, vol 39, iss 18 |
publishDate | 2012 |
publisher | eScholarship, University of California |
record_format | openpolar |
spelling | ftcdlib:oai:escholarship.org:ark:/13030/qt95v6k9p4 2025-01-16T22:26:33+00:00 A damage mechanics assessment of the Larsen B ice shelf prior to collapse: Toward a physically‐based calving law Borstad, CP Khazendar, A Larour, E Morlighem, M Rignot, E Schodlok, MP Seroussi, H 2012-09-01 application/pdf https://escholarship.org/uc/item/95v6k9p4 https://escholarship.org/content/qt95v6k9p4/qt95v6k9p4.pdf https://doi.org/10.1029/2012gl053317 unknown eScholarship, University of California qt95v6k9p4 https://escholarship.org/uc/item/95v6k9p4 https://escholarship.org/content/qt95v6k9p4/qt95v6k9p4.pdf doi:10.1029/2012gl053317 CC-BY Geophysical Research Letters, vol 39, iss 18 Meteorology & Atmospheric Sciences article 2012 ftcdlib https://doi.org/10.1029/2012gl053317 2024-06-28T06:28:19Z Calving is a primary process of mass ablation for glaciers and ice sheets, though it still eludes a general physical law. Here, we propose a calving framework based on continuum damage mechanics coupled with the equations of viscous deformation of glacier ice. We introduce a scalar damage variable that quantifies the loss of load-bearing surface area due to fractures and that feeds back with ice viscosity to represent fracture-induced softening. The calving law is a standard failure criterion for viscous damaging materials and represents a macroscopic brittle instability quantified by a critical or threshold damage. We constrain this threshold using the Ice Sheet System Model (ISSM) by inverting for damage on the Larsen B ice shelf prior to its 2002 collapse. By analyzing the damage distribution in areas that subsequently calved, we conclude that calving occurs after fractures have reduced the load-bearing capacity of the ice by 60 ± 10%. © 2012. American Geophysical Union. All Rights Reserved. Article in Journal/Newspaper Ice Sheet Ice Shelf University of California: eScholarship Geophysical Research Letters 39 18 |
spellingShingle | Meteorology & Atmospheric Sciences Borstad, CP Khazendar, A Larour, E Morlighem, M Rignot, E Schodlok, MP Seroussi, H A damage mechanics assessment of the Larsen B ice shelf prior to collapse: Toward a physically‐based calving law |
title | A damage mechanics assessment of the Larsen B ice shelf prior to collapse: Toward a physically‐based calving law |
title_full | A damage mechanics assessment of the Larsen B ice shelf prior to collapse: Toward a physically‐based calving law |
title_fullStr | A damage mechanics assessment of the Larsen B ice shelf prior to collapse: Toward a physically‐based calving law |
title_full_unstemmed | A damage mechanics assessment of the Larsen B ice shelf prior to collapse: Toward a physically‐based calving law |
title_short | A damage mechanics assessment of the Larsen B ice shelf prior to collapse: Toward a physically‐based calving law |
title_sort | damage mechanics assessment of the larsen b ice shelf prior to collapse: toward a physically‐based calving law |
topic | Meteorology & Atmospheric Sciences |
topic_facet | Meteorology & Atmospheric Sciences |
url | https://escholarship.org/uc/item/95v6k9p4 https://escholarship.org/content/qt95v6k9p4/qt95v6k9p4.pdf https://doi.org/10.1029/2012gl053317 |