Adaptive mesh refinement versus subgrid friction interpolation in simulations of Antarctic ice dynamics
At least in conventional hydrostatic ice-sheet models, the numerical error associated with grounding line dynamics can be reduced by modifications to the discretization scheme. These involve altering the integration formulae for the basal traction and/or driving stress close to the grounding line an...
Published in: | Annals of Glaciology |
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2016
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Online Access: | https://hdl.handle.net/1983/527ddf2d-66dd-434e-97b4-98da87fbf7b1 https://research-information.bris.ac.uk/en/publications/527ddf2d-66dd-434e-97b4-98da87fbf7b1 https://doi.org/10.1017/aog.2016.13 https://research-information.bris.ac.uk/ws/files/106879872/div_class_title_adaptive_mesh_refinement_versus_subgrid_friction_interpolation_in_simulations_of_antarctic_ice_dynamics_div.pdf |
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ftubristolcris:oai:research-information.bris.ac.uk:publications/527ddf2d-66dd-434e-97b4-98da87fbf7b1 2024-04-28T07:55:30+00:00 Adaptive mesh refinement versus subgrid friction interpolation in simulations of Antarctic ice dynamics Cornford, Stephen Martin, Daniel Lee, Victoria Payne, Tony Ng, Esmond 2016-09 application/pdf https://hdl.handle.net/1983/527ddf2d-66dd-434e-97b4-98da87fbf7b1 https://research-information.bris.ac.uk/en/publications/527ddf2d-66dd-434e-97b4-98da87fbf7b1 https://doi.org/10.1017/aog.2016.13 https://research-information.bris.ac.uk/ws/files/106879872/div_class_title_adaptive_mesh_refinement_versus_subgrid_friction_interpolation_in_simulations_of_antarctic_ice_dynamics_div.pdf eng eng https://research-information.bris.ac.uk/en/publications/527ddf2d-66dd-434e-97b4-98da87fbf7b1 info:eu-repo/semantics/openAccess Cornford , S , Martin , D , Lee , V , Payne , T & Ng , E 2016 , ' Adaptive mesh refinement versus subgrid friction interpolation in simulations of Antarctic ice dynamics ' , Annals of Glaciology , vol. 57 , no. 73 , pp. 1-9 . https://doi.org/10.1017/aog.2016.13 article 2016 ftubristolcris https://doi.org/10.1017/aog.2016.13 2024-04-03T15:33:35Z At least in conventional hydrostatic ice-sheet models, the numerical error associated with grounding line dynamics can be reduced by modifications to the discretization scheme. These involve altering the integration formulae for the basal traction and/or driving stress close to the grounding line and exhibit lower – if still first-order – error in the MISMIP3d experiments. MISMIP3d may not represent the variety of real ice streams, in that it lacks strong lateral stresses, and imposes a large basal traction at the grounding line. We study resolution sensitivity in the context of extreme forcing simulations of the entire Antarctic ice sheet, using the BISICLES adaptive mesh ice-sheet model with two schemes: the original treatment, and a scheme, which modifies the discretization of the basal traction. The second scheme does indeed improve accuracy – by around a factor of two – for a given mesh spacing, but $\lesssim 1$ km resolution is still necessary. For example, in coarser resolution simulations Thwaites Glacier retreats so slowly that other ice streams divert its trunk. In contrast, with $\lesssim 1$ km meshes, the same glacier retreats far more quickly and triggers the final phase of West Antarctic collapse a century before any such diversion can take place. Article in Journal/Newspaper Annals of Glaciology Antarc* Antarctic Ice Sheet Thwaites Glacier University of Bristol: Bristol Research Annals of Glaciology 57 73 1 9 |
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Open Polar |
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University of Bristol: Bristol Research |
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ftubristolcris |
language |
English |
description |
At least in conventional hydrostatic ice-sheet models, the numerical error associated with grounding line dynamics can be reduced by modifications to the discretization scheme. These involve altering the integration formulae for the basal traction and/or driving stress close to the grounding line and exhibit lower – if still first-order – error in the MISMIP3d experiments. MISMIP3d may not represent the variety of real ice streams, in that it lacks strong lateral stresses, and imposes a large basal traction at the grounding line. We study resolution sensitivity in the context of extreme forcing simulations of the entire Antarctic ice sheet, using the BISICLES adaptive mesh ice-sheet model with two schemes: the original treatment, and a scheme, which modifies the discretization of the basal traction. The second scheme does indeed improve accuracy – by around a factor of two – for a given mesh spacing, but $\lesssim 1$ km resolution is still necessary. For example, in coarser resolution simulations Thwaites Glacier retreats so slowly that other ice streams divert its trunk. In contrast, with $\lesssim 1$ km meshes, the same glacier retreats far more quickly and triggers the final phase of West Antarctic collapse a century before any such diversion can take place. |
format |
Article in Journal/Newspaper |
author |
Cornford, Stephen Martin, Daniel Lee, Victoria Payne, Tony Ng, Esmond |
spellingShingle |
Cornford, Stephen Martin, Daniel Lee, Victoria Payne, Tony Ng, Esmond Adaptive mesh refinement versus subgrid friction interpolation in simulations of Antarctic ice dynamics |
author_facet |
Cornford, Stephen Martin, Daniel Lee, Victoria Payne, Tony Ng, Esmond |
author_sort |
Cornford, Stephen |
title |
Adaptive mesh refinement versus subgrid friction interpolation in simulations of Antarctic ice dynamics |
title_short |
Adaptive mesh refinement versus subgrid friction interpolation in simulations of Antarctic ice dynamics |
title_full |
Adaptive mesh refinement versus subgrid friction interpolation in simulations of Antarctic ice dynamics |
title_fullStr |
Adaptive mesh refinement versus subgrid friction interpolation in simulations of Antarctic ice dynamics |
title_full_unstemmed |
Adaptive mesh refinement versus subgrid friction interpolation in simulations of Antarctic ice dynamics |
title_sort |
adaptive mesh refinement versus subgrid friction interpolation in simulations of antarctic ice dynamics |
publishDate |
2016 |
url |
https://hdl.handle.net/1983/527ddf2d-66dd-434e-97b4-98da87fbf7b1 https://research-information.bris.ac.uk/en/publications/527ddf2d-66dd-434e-97b4-98da87fbf7b1 https://doi.org/10.1017/aog.2016.13 https://research-information.bris.ac.uk/ws/files/106879872/div_class_title_adaptive_mesh_refinement_versus_subgrid_friction_interpolation_in_simulations_of_antarctic_ice_dynamics_div.pdf |
genre |
Annals of Glaciology Antarc* Antarctic Ice Sheet Thwaites Glacier |
genre_facet |
Annals of Glaciology Antarc* Antarctic Ice Sheet Thwaites Glacier |
op_source |
Cornford , S , Martin , D , Lee , V , Payne , T & Ng , E 2016 , ' Adaptive mesh refinement versus subgrid friction interpolation in simulations of Antarctic ice dynamics ' , Annals of Glaciology , vol. 57 , no. 73 , pp. 1-9 . https://doi.org/10.1017/aog.2016.13 |
op_relation |
https://research-information.bris.ac.uk/en/publications/527ddf2d-66dd-434e-97b4-98da87fbf7b1 |
op_rights |
info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1017/aog.2016.13 |
container_title |
Annals of Glaciology |
container_volume |
57 |
container_issue |
73 |
container_start_page |
1 |
op_container_end_page |
9 |
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1797580201089040384 |