Simulating ice-shelf extent using damage mechanics

Abstract Inaccurate representations of iceberg calving from ice shelves are a large source of uncertainty in mass-loss projections from the Antarctic ice sheet. Here, we address this limitation by implementing and testing a continuum damage-mechanics model in a continental scale ice-sheet model. The...

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Bibliographic Details
Published in:Journal of Glaciology
Main Authors: Kachuck, Samuel B., Whitcomb, Morgan, Bassis, Jeremy N., Martin, Daniel F., Price, Stephen F.
Other Authors: National Science Foundation, U.S. Department of Energy
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2022
Subjects:
Online Access:http://dx.doi.org/10.1017/jog.2022.12
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143022000120
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spelling crcambridgeupr:10.1017/jog.2022.12 2024-05-19T07:28:12+00:00 Simulating ice-shelf extent using damage mechanics Kachuck, Samuel B. Whitcomb, Morgan Bassis, Jeremy N. Martin, Daniel F. Price, Stephen F. National Science Foundation U.S. Department of Energy U.S. Department of Energy 2022 http://dx.doi.org/10.1017/jog.2022.12 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143022000120 en eng Cambridge University Press (CUP) https://creativecommons.org/licenses/by/4.0/ Journal of Glaciology page 1-12 ISSN 0022-1430 1727-5652 journal-article 2022 crcambridgeupr https://doi.org/10.1017/jog.2022.12 2024-05-02T06:51:10Z Abstract Inaccurate representations of iceberg calving from ice shelves are a large source of uncertainty in mass-loss projections from the Antarctic ice sheet. Here, we address this limitation by implementing and testing a continuum damage-mechanics model in a continental scale ice-sheet model. The damage-mechanics formulation, based on a linear stability analysis and subsequent long-wavelength approximation of crevasses that evolve in a viscous medium, links damage evolution to climate forcing and the large-scale stresses within an ice shelf. We incorporate this model into the BISICLES ice-sheet model and test it by applying it to idealized (1) ice tongues, for which we present analytical solutions and (2) buttressed ice-shelf geometries. Our simulations show that the model reproduces the large disparity in lengths of ice shelves with geometries and melt rates broadly similar to those of four Antarctic ice shelves: Erebus Glacier Tongue (length ~ 13 km), the unembayed portion of Drygalski Ice Tongue (~ 65 km), the Amery Ice Shelf (~ 350 km) and the Ross Ice Shelf (~ 500 km). These results demonstrate that our simple continuum model holds promise for constraining realistic ice-shelf extents in large-scale ice-sheet models in a computationally tractable manner. Article in Journal/Newspaper Amery Ice Shelf Antarc* Antarctic Erebus Glacier Ice Sheet Ice Shelf Ice Shelves Iceberg* Journal of Glaciology Ross Ice Shelf Cambridge University Press Journal of Glaciology 1 12
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
description Abstract Inaccurate representations of iceberg calving from ice shelves are a large source of uncertainty in mass-loss projections from the Antarctic ice sheet. Here, we address this limitation by implementing and testing a continuum damage-mechanics model in a continental scale ice-sheet model. The damage-mechanics formulation, based on a linear stability analysis and subsequent long-wavelength approximation of crevasses that evolve in a viscous medium, links damage evolution to climate forcing and the large-scale stresses within an ice shelf. We incorporate this model into the BISICLES ice-sheet model and test it by applying it to idealized (1) ice tongues, for which we present analytical solutions and (2) buttressed ice-shelf geometries. Our simulations show that the model reproduces the large disparity in lengths of ice shelves with geometries and melt rates broadly similar to those of four Antarctic ice shelves: Erebus Glacier Tongue (length ~ 13 km), the unembayed portion of Drygalski Ice Tongue (~ 65 km), the Amery Ice Shelf (~ 350 km) and the Ross Ice Shelf (~ 500 km). These results demonstrate that our simple continuum model holds promise for constraining realistic ice-shelf extents in large-scale ice-sheet models in a computationally tractable manner.
author2 National Science Foundation
U.S. Department of Energy
U.S. Department of Energy
format Article in Journal/Newspaper
author Kachuck, Samuel B.
Whitcomb, Morgan
Bassis, Jeremy N.
Martin, Daniel F.
Price, Stephen F.
spellingShingle Kachuck, Samuel B.
Whitcomb, Morgan
Bassis, Jeremy N.
Martin, Daniel F.
Price, Stephen F.
Simulating ice-shelf extent using damage mechanics
author_facet Kachuck, Samuel B.
Whitcomb, Morgan
Bassis, Jeremy N.
Martin, Daniel F.
Price, Stephen F.
author_sort Kachuck, Samuel B.
title Simulating ice-shelf extent using damage mechanics
title_short Simulating ice-shelf extent using damage mechanics
title_full Simulating ice-shelf extent using damage mechanics
title_fullStr Simulating ice-shelf extent using damage mechanics
title_full_unstemmed Simulating ice-shelf extent using damage mechanics
title_sort simulating ice-shelf extent using damage mechanics
publisher Cambridge University Press (CUP)
publishDate 2022
url http://dx.doi.org/10.1017/jog.2022.12
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143022000120
genre Amery Ice Shelf
Antarc*
Antarctic
Erebus Glacier
Ice Sheet
Ice Shelf
Ice Shelves
Iceberg*
Journal of Glaciology
Ross Ice Shelf
genre_facet Amery Ice Shelf
Antarc*
Antarctic
Erebus Glacier
Ice Sheet
Ice Shelf
Ice Shelves
Iceberg*
Journal of Glaciology
Ross Ice Shelf
op_source Journal of Glaciology
page 1-12
ISSN 0022-1430 1727-5652
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.1017/jog.2022.12
container_title Journal of Glaciology
container_start_page 1
op_container_end_page 12
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