Simulating the processes controlling ice-shelf rift paths using damage mechanics

Abstract Rifts are full-thickness fractures that propagate laterally across an ice shelf. They cause ice-shelf weakening and calving of tabular icebergs, and control the initial size of calved icebergs. Here, we present a joint inverse and forward computational modeling framework to capture rifting...

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Published in:Journal of Glaciology
Main Authors: Huth, Alex, Duddu, Ravindra, Smith, Benjamin, Sergienko, Olga
Other Authors: National Aeronautics and Space Administration, National Science Foundation
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2023
Subjects:
Online Access:http://dx.doi.org/10.1017/jog.2023.71
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143023000710
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spelling crcambridgeupr:10.1017/jog.2023.71 2024-04-07T07:53:16+00:00 Simulating the processes controlling ice-shelf rift paths using damage mechanics Huth, Alex Duddu, Ravindra Smith, Benjamin Sergienko, Olga National Aeronautics and Space Administration National Science Foundation National Science Foundation 2023 http://dx.doi.org/10.1017/jog.2023.71 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143023000710 en eng Cambridge University Press (CUP) http://creativecommons.org/licenses/by/4.0/ Journal of Glaciology page 1-14 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 2023 crcambridgeupr https://doi.org/10.1017/jog.2023.71 2024-03-08T00:33:38Z Abstract Rifts are full-thickness fractures that propagate laterally across an ice shelf. They cause ice-shelf weakening and calving of tabular icebergs, and control the initial size of calved icebergs. Here, we present a joint inverse and forward computational modeling framework to capture rifting by combining the vertically integrated momentum balance and anisotropic continuum damage mechanics formulations. We incorporate rift–flank boundary processes to investigate how the rift path is influenced by the pressure on rift–flank walls from seawater, contact between flanks, and ice mélange that may also transmit stress between flanks. To illustrate the viability of the framework, we simulate the final 2 years of rift propagation associated with the calving of tabular iceberg A68 in 2017. We find that the rift path can change with varying ice mélange conditions and the extent of contact between rift flanks. Combinations of parameters associated with slower rift widening rates yield simulated rift paths that best match observations. Our modeling framework lays the foundation for robust simulation of rifting and tabular calving processes, which can enable future studies on ice-sheet–climate interactions, and the effects of ice-shelf buttressing on land ice flow. Article in Journal/Newspaper Ice Sheet Ice Shelf Journal of Glaciology Cambridge University Press Journal of Glaciology 1 14
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Huth, Alex
Duddu, Ravindra
Smith, Benjamin
Sergienko, Olga
Simulating the processes controlling ice-shelf rift paths using damage mechanics
topic_facet Earth-Surface Processes
description Abstract Rifts are full-thickness fractures that propagate laterally across an ice shelf. They cause ice-shelf weakening and calving of tabular icebergs, and control the initial size of calved icebergs. Here, we present a joint inverse and forward computational modeling framework to capture rifting by combining the vertically integrated momentum balance and anisotropic continuum damage mechanics formulations. We incorporate rift–flank boundary processes to investigate how the rift path is influenced by the pressure on rift–flank walls from seawater, contact between flanks, and ice mélange that may also transmit stress between flanks. To illustrate the viability of the framework, we simulate the final 2 years of rift propagation associated with the calving of tabular iceberg A68 in 2017. We find that the rift path can change with varying ice mélange conditions and the extent of contact between rift flanks. Combinations of parameters associated with slower rift widening rates yield simulated rift paths that best match observations. Our modeling framework lays the foundation for robust simulation of rifting and tabular calving processes, which can enable future studies on ice-sheet–climate interactions, and the effects of ice-shelf buttressing on land ice flow.
author2 National Aeronautics and Space Administration
National Science Foundation
National Science Foundation
format Article in Journal/Newspaper
author Huth, Alex
Duddu, Ravindra
Smith, Benjamin
Sergienko, Olga
author_facet Huth, Alex
Duddu, Ravindra
Smith, Benjamin
Sergienko, Olga
author_sort Huth, Alex
title Simulating the processes controlling ice-shelf rift paths using damage mechanics
title_short Simulating the processes controlling ice-shelf rift paths using damage mechanics
title_full Simulating the processes controlling ice-shelf rift paths using damage mechanics
title_fullStr Simulating the processes controlling ice-shelf rift paths using damage mechanics
title_full_unstemmed Simulating the processes controlling ice-shelf rift paths using damage mechanics
title_sort simulating the processes controlling ice-shelf rift paths using damage mechanics
publisher Cambridge University Press (CUP)
publishDate 2023
url http://dx.doi.org/10.1017/jog.2023.71
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143023000710
genre Ice Sheet
Ice Shelf
Journal of Glaciology
genre_facet Ice Sheet
Ice Shelf
Journal of Glaciology
op_source Journal of Glaciology
page 1-14
ISSN 0022-1430 1727-5652
op_rights http://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.1017/jog.2023.71
container_title Journal of Glaciology
container_start_page 1
op_container_end_page 14
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