Articles | Volume 11, issue 6
https://doi.org/10.5194/tc-11-2543-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/tc-11-2543-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Ice shelf fracture parameterization in an ice sheet model
Sainan Sun
Laboratoire de Glaciologie, Université libre de Bruxelles, Brussels, Belgium
College of Global Change and Earth System Science, Beijing Normal University, 100082, Beijing, China
Stephen L. Cornford
CORRESPONDING AUTHOR
Department of Geography, College of Science, Swansea University, Singleton Park, Swansea, SA2 8PP, UK
John C. Moore
Arctic Centre, University of Lapland, Rovaniemi, 96101, Finland
College of Global Change and Earth System Science, Beijing Normal University, 100082, Beijing, China
Rupert Gladstone
Arctic Centre, University of Lapland, Rovaniemi, 96101, Finland
Liyun Zhao
College of Global Change and Earth System Science, Beijing Normal University, 100082, Beijing, China
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- The speedup of Pine Island Ice Shelf between 2017 and 2020: revaluating the importance of ice damage S. Sun & G. Gudmundsson 10.1017/jog.2023.76
- Rapid fragmentation of Thwaites Eastern Ice Shelf D. Benn et al. 10.5194/tc-16-2545-2022
- A non-local continuum poro-damage mechanics model for hydrofracturing of surface crevasses in grounded glaciers R. Duddu et al. 10.1017/jog.2020.16
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- The ice dynamic and melting response of Pine Island Ice Shelf to calving A. Bradley et al. 10.1017/aog.2023.24
- The Influence of Pine Island Ice Shelf Calving on Basal Melting A. Bradley et al. 10.1029/2022JC018621
- Episodic dynamic change linked to damage on the Thwaites Glacier Ice Tongue T. Surawy-Stepney et al. 10.1038/s41561-022-01097-9
- A Generalized Interpolation Material Point Method for Shallow Ice Shelves. 1: Shallow Shelf Approximation and Ice Thickness Evolution A. Huth et al. 10.1029/2020MS002277
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- A Generalized Interpolation Material Point Method for Shallow Ice Shelves. 2: Anisotropic Nonlocal Damage Mechanics and Rift Propagation A. Huth et al. 10.1029/2020MS002292
- Marginal Detachment Zones: The Fracture Factories of Ice Shelves? C. Miele et al. 10.1029/2022JF006959
- Drivers of Pine Island Glacier speed-up between 1996 and 2016 J. De Rydt et al. 10.5194/tc-15-113-2021
- Dynamic response of Antarctic Peninsula Ice Sheet to potential collapse of Larsen C and George VI ice shelves C. Schannwell et al. 10.5194/tc-12-2307-2018
- SERMeQ Model Produces a Realistic Upper Bound on Calving Retreat for 155 Greenland Outlet Glaciers L. Ultee & J. Bassis 10.1029/2020GL090213
- The uncertain future of the Antarctic Ice Sheet F. Pattyn & M. Morlighem 10.1126/science.aaz5487
- Simulating ice-shelf extent using damage mechanics S. Kachuck et al. 10.1017/jog.2022.12
- Damage accelerates ice shelf instability and mass loss in Amundsen Sea Embayment S. Lhermitte et al. 10.1073/pnas.1912890117
- Damage detection on antarctic ice shelves using the normalised radon transform M. Izeboud & S. Lhermitte 10.1016/j.rse.2022.113359
- Stability of Ice Shelves and Ice Cliffs in a Changing Climate J. Bassis et al. 10.1146/annurev-earth-040522-122817
- Modelling Antarctic ice shelf basal melt patterns using the one-layer Antarctic model for dynamical downscaling of ice–ocean exchanges (LADDIE v1.0) E. Lambert et al. 10.5194/tc-17-3203-2023
- Analysis of continuous calving front retreat and the associated influencing factors of the Thwaites Glacier using high-resolution remote sensing data from 2015 to 2023 Q. Zhu et al. 10.1080/17538947.2024.2390438
- Progress in Numerical Modeling of Antarctic Ice-Sheet Dynamics F. Pattyn et al. 10.1007/s40641-017-0069-7
- Calving glaciers and ice shelves D. Benn & J. Åström 10.1080/23746149.2018.1513819
28 citations as recorded by crossref.
- Automatic delineation of cracks with Sentinel-1 interferometry for monitoring ice shelf damage and calving L. Libert et al. 10.5194/tc-16-1523-2022
- Simulating the processes controlling ice-shelf rift paths using damage mechanics A. Huth et al. 10.1017/jog.2023.71
- Crevasse advection increases glacier calving B. Berg & J. Bassis 10.1017/jog.2022.10
- The speedup of Pine Island Ice Shelf between 2017 and 2020: revaluating the importance of ice damage S. Sun & G. Gudmundsson 10.1017/jog.2023.76
- Rapid fragmentation of Thwaites Eastern Ice Shelf D. Benn et al. 10.5194/tc-16-2545-2022
- A non-local continuum poro-damage mechanics model for hydrofracturing of surface crevasses in grounded glaciers R. Duddu et al. 10.1017/jog.2020.16
- Simulated retreat of Jakobshavn Isbræ during the 21st century X. Guo et al. 10.5194/tc-13-3139-2019
- Short- and long-term variability of the Antarctic and Greenland ice sheets E. Hanna et al. 10.1038/s43017-023-00509-7
- Failure strength of glacier ice inferred from Greenland crevasses A. Grinsted et al. 10.5194/tc-18-1947-2024
- Investigating the dynamics and interactions of surface features on Pine Island Glacier using remote sensing and deep learning Q. Zhu et al. 10.1016/j.accre.2024.07.011
- Structures and Deformation in Glaciers and Ice Sheets S. Jennings & M. Hambrey 10.1029/2021RG000743
- The ice dynamic and melting response of Pine Island Ice Shelf to calving A. Bradley et al. 10.1017/aog.2023.24
- The Influence of Pine Island Ice Shelf Calving on Basal Melting A. Bradley et al. 10.1029/2022JC018621
- Episodic dynamic change linked to damage on the Thwaites Glacier Ice Tongue T. Surawy-Stepney et al. 10.1038/s41561-022-01097-9
- A Generalized Interpolation Material Point Method for Shallow Ice Shelves. 1: Shallow Shelf Approximation and Ice Thickness Evolution A. Huth et al. 10.1029/2020MS002277
- Weak relationship between remotely detected crevasses and inferred ice rheological parameters on Antarctic ice shelves C. Gerli et al. 10.5194/tc-18-2677-2024
- A Generalized Interpolation Material Point Method for Shallow Ice Shelves. 2: Anisotropic Nonlocal Damage Mechanics and Rift Propagation A. Huth et al. 10.1029/2020MS002292
- Marginal Detachment Zones: The Fracture Factories of Ice Shelves? C. Miele et al. 10.1029/2022JF006959
- Drivers of Pine Island Glacier speed-up between 1996 and 2016 J. De Rydt et al. 10.5194/tc-15-113-2021
- Dynamic response of Antarctic Peninsula Ice Sheet to potential collapse of Larsen C and George VI ice shelves C. Schannwell et al. 10.5194/tc-12-2307-2018
- SERMeQ Model Produces a Realistic Upper Bound on Calving Retreat for 155 Greenland Outlet Glaciers L. Ultee & J. Bassis 10.1029/2020GL090213
- The uncertain future of the Antarctic Ice Sheet F. Pattyn & M. Morlighem 10.1126/science.aaz5487
- Simulating ice-shelf extent using damage mechanics S. Kachuck et al. 10.1017/jog.2022.12
- Damage accelerates ice shelf instability and mass loss in Amundsen Sea Embayment S. Lhermitte et al. 10.1073/pnas.1912890117
- Damage detection on antarctic ice shelves using the normalised radon transform M. Izeboud & S. Lhermitte 10.1016/j.rse.2022.113359
- Stability of Ice Shelves and Ice Cliffs in a Changing Climate J. Bassis et al. 10.1146/annurev-earth-040522-122817
- Modelling Antarctic ice shelf basal melt patterns using the one-layer Antarctic model for dynamical downscaling of ice–ocean exchanges (LADDIE v1.0) E. Lambert et al. 10.5194/tc-17-3203-2023
- Analysis of continuous calving front retreat and the associated influencing factors of the Thwaites Glacier using high-resolution remote sensing data from 2015 to 2023 Q. Zhu et al. 10.1080/17538947.2024.2390438
Latest update: 23 Nov 2024
Short summary
The buttressing effect of the floating ice shelves is diminished by the fracture process. We developed a continuum damage mechanics model component of the ice sheet model to simulate the process. The model is tested on an ideal marine ice sheet geometry. We find that behavior of the simulated marine ice sheet is sensitive to fracture processes on the ice shelf, and the stiffness of ice around the grounding line is essential to ice sheet evolution.
The buttressing effect of the floating ice shelves is diminished by the fracture process. We...