The effect of hydrology and crevasse wall contact on calving

Calving is one of the main controls on the dynamics of marine ice sheets. We solve a quasi-static linear elastic fracture dynamics problem, forced by a viscous pre-stress describing the stress state in the ice prior to the introduction of a crack, to determine conditions under which an ice shelf can...

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Main Authors: Zarrinderakht, Maryam, Schoof, Christian, Peirce, Anthony
Format: Text
Language:English
Published: 2022
Subjects:
Online Access:https://doi.org/10.5194/tc-2022-37
https://tc.copernicus.org/preprints/tc-2022-37/
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spelling ftcopernicus:oai:publications.copernicus.org:tcd101362 2023-05-15T16:41:52+02:00 The effect of hydrology and crevasse wall contact on calving Zarrinderakht, Maryam Schoof, Christian Peirce, Anthony 2022-03-04 application/pdf https://doi.org/10.5194/tc-2022-37 https://tc.copernicus.org/preprints/tc-2022-37/ eng eng doi:10.5194/tc-2022-37 https://tc.copernicus.org/preprints/tc-2022-37/ eISSN: 1994-0424 Text 2022 ftcopernicus https://doi.org/10.5194/tc-2022-37 2022-03-07T17:22:16Z Calving is one of the main controls on the dynamics of marine ice sheets. We solve a quasi-static linear elastic fracture dynamics problem, forced by a viscous pre-stress describing the stress state in the ice prior to the introduction of a crack, to determine conditions under which an ice shelf can calve for a variety of different surface hydrologies. Extending previous work, we develop a boundary-element-based method for solving the problem, which enables us to ensure that the faces of crevasses are not spuriously allowed to penetrate into each other in the model. We find that a fixed water table below the ice surface can lead to two distinct styles of calving, one of which involves the abrupt unstable growth of a crack across a finite thickness of unbroken ice that is potentially history-dependent, while the other involves the continuous growth of the crack until the full ice thickness is cracked, which occurs at a critical combination of extensional stress, water level, and ice thickness. We give a relatively simple analytical calving law for the latter case. For a fixed water volume injected into a surface crack, we find that complete crack propagation almost invariably happens at realistic extensional stresses if the initial crack length exceeds a shallow threshold, but we also argue that this process is more likely to correspond to the formation of a localized, moulin-like slot that permits drainage, rather than a calving event. We also revisit the formation of basal cracks and find that, in the model, they invariably propagate across the full ice shelf at stresses that are readily generated near an ice shelf front. This indicates that a more sophisticated coupling of the present model (which has been used in a very similar form by several previous authors) needs modification to incorporate the effect of torques generated by buoyantly-modulated shelf flexure in the far field. Text Ice Shelf Copernicus Publications: E-Journals
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description Calving is one of the main controls on the dynamics of marine ice sheets. We solve a quasi-static linear elastic fracture dynamics problem, forced by a viscous pre-stress describing the stress state in the ice prior to the introduction of a crack, to determine conditions under which an ice shelf can calve for a variety of different surface hydrologies. Extending previous work, we develop a boundary-element-based method for solving the problem, which enables us to ensure that the faces of crevasses are not spuriously allowed to penetrate into each other in the model. We find that a fixed water table below the ice surface can lead to two distinct styles of calving, one of which involves the abrupt unstable growth of a crack across a finite thickness of unbroken ice that is potentially history-dependent, while the other involves the continuous growth of the crack until the full ice thickness is cracked, which occurs at a critical combination of extensional stress, water level, and ice thickness. We give a relatively simple analytical calving law for the latter case. For a fixed water volume injected into a surface crack, we find that complete crack propagation almost invariably happens at realistic extensional stresses if the initial crack length exceeds a shallow threshold, but we also argue that this process is more likely to correspond to the formation of a localized, moulin-like slot that permits drainage, rather than a calving event. We also revisit the formation of basal cracks and find that, in the model, they invariably propagate across the full ice shelf at stresses that are readily generated near an ice shelf front. This indicates that a more sophisticated coupling of the present model (which has been used in a very similar form by several previous authors) needs modification to incorporate the effect of torques generated by buoyantly-modulated shelf flexure in the far field.
format Text
author Zarrinderakht, Maryam
Schoof, Christian
Peirce, Anthony
spellingShingle Zarrinderakht, Maryam
Schoof, Christian
Peirce, Anthony
The effect of hydrology and crevasse wall contact on calving
author_facet Zarrinderakht, Maryam
Schoof, Christian
Peirce, Anthony
author_sort Zarrinderakht, Maryam
title The effect of hydrology and crevasse wall contact on calving
title_short The effect of hydrology and crevasse wall contact on calving
title_full The effect of hydrology and crevasse wall contact on calving
title_fullStr The effect of hydrology and crevasse wall contact on calving
title_full_unstemmed The effect of hydrology and crevasse wall contact on calving
title_sort effect of hydrology and crevasse wall contact on calving
publishDate 2022
url https://doi.org/10.5194/tc-2022-37
https://tc.copernicus.org/preprints/tc-2022-37/
genre Ice Shelf
genre_facet Ice Shelf
op_source eISSN: 1994-0424
op_relation doi:10.5194/tc-2022-37
https://tc.copernicus.org/preprints/tc-2022-37/
op_doi https://doi.org/10.5194/tc-2022-37
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