Inversion of basal friction in Antarctica using exact and incomplete adjoints of a higher‐order model
Basal friction beneath ice sheets remains poorly characterized and yet is a fundamental control on ice mechanics. Here we use a complete map of surface velocity of the Antarctic Ice Sheet to infer the basal friction over the entire continent by combining these observations with a three-dimensional,...
Published in: | Journal of Geophysical Research: Earth Surface |
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2013
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Online Access: | https://escholarship.org/uc/item/4j39c4v4 https://escholarship.org/content/qt4j39c4v4/qt4j39c4v4.pdf https://doi.org/10.1002/jgrf.20125 |
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ftcdlib:oai:escholarship.org:ark:/13030/qt4j39c4v4 2024-09-15T17:44:15+00:00 Inversion of basal friction in Antarctica using exact and incomplete adjoints of a higher‐order model Morlighem, M Seroussi, H Larour, E Rignot, E 1746 - 1753 2013-09-01 application/pdf https://escholarship.org/uc/item/4j39c4v4 https://escholarship.org/content/qt4j39c4v4/qt4j39c4v4.pdf https://doi.org/10.1002/jgrf.20125 unknown eScholarship, University of California qt4j39c4v4 https://escholarship.org/uc/item/4j39c4v4 https://escholarship.org/content/qt4j39c4v4/qt4j39c4v4.pdf doi:10.1002/jgrf.20125 CC-BY Journal of Geophysical Research Earth Surface, vol 118, iss 3 Bioengineering inverse method exact adjoint incomplete adjoint basal friction large-scale modeling Earth Sciences article 2013 ftcdlib https://doi.org/10.1002/jgrf.20125 2024-06-28T06:28:20Z Basal friction beneath ice sheets remains poorly characterized and yet is a fundamental control on ice mechanics. Here we use a complete map of surface velocity of the Antarctic Ice Sheet to infer the basal friction over the entire continent by combining these observations with a three-dimensional, thermomechanical, higher-order ice sheet numerical model from the Ice Sheet System Model open source software. We demonstrate that inverse methods can be readily applied at the continental scale with appropriate selections of cost function and of scheme of regularization, at a spatial resolution as high as 3 km along the coastline. We compare the convergence of two descent algorithms with the exact and incomplete adjoints to show that the incomplete adjoint is an excellent approximation. The results reveal that the driving stress is almost entirely balanced by the basal shear stress over 80% of the ice sheet. The basal friction coefficient, which relates basal friction to basal velocity, is, however, significantly heterogeneous: it is low on fast moving ice and high near topographic divides. Areas with low values extend far out into the interior, along glacier and ice stream tributaries, almost to the flanks of topographic divides, suggesting that basal sliding is widespread beneath the Antarctic Ice Sheet. ©2013. American Geophysical Union. All Rights Reserved. Article in Journal/Newspaper Antarc* Antarctic Antarctica Ice Sheet University of California: eScholarship Journal of Geophysical Research: Earth Surface 118 3 1746 1753 |
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Open Polar |
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University of California: eScholarship |
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ftcdlib |
language |
unknown |
topic |
Bioengineering inverse method exact adjoint incomplete adjoint basal friction large-scale modeling Earth Sciences |
spellingShingle |
Bioengineering inverse method exact adjoint incomplete adjoint basal friction large-scale modeling Earth Sciences Morlighem, M Seroussi, H Larour, E Rignot, E Inversion of basal friction in Antarctica using exact and incomplete adjoints of a higher‐order model |
topic_facet |
Bioengineering inverse method exact adjoint incomplete adjoint basal friction large-scale modeling Earth Sciences |
description |
Basal friction beneath ice sheets remains poorly characterized and yet is a fundamental control on ice mechanics. Here we use a complete map of surface velocity of the Antarctic Ice Sheet to infer the basal friction over the entire continent by combining these observations with a three-dimensional, thermomechanical, higher-order ice sheet numerical model from the Ice Sheet System Model open source software. We demonstrate that inverse methods can be readily applied at the continental scale with appropriate selections of cost function and of scheme of regularization, at a spatial resolution as high as 3 km along the coastline. We compare the convergence of two descent algorithms with the exact and incomplete adjoints to show that the incomplete adjoint is an excellent approximation. The results reveal that the driving stress is almost entirely balanced by the basal shear stress over 80% of the ice sheet. The basal friction coefficient, which relates basal friction to basal velocity, is, however, significantly heterogeneous: it is low on fast moving ice and high near topographic divides. Areas with low values extend far out into the interior, along glacier and ice stream tributaries, almost to the flanks of topographic divides, suggesting that basal sliding is widespread beneath the Antarctic Ice Sheet. ©2013. American Geophysical Union. All Rights Reserved. |
format |
Article in Journal/Newspaper |
author |
Morlighem, M Seroussi, H Larour, E Rignot, E |
author_facet |
Morlighem, M Seroussi, H Larour, E Rignot, E |
author_sort |
Morlighem, M |
title |
Inversion of basal friction in Antarctica using exact and incomplete adjoints of a higher‐order model |
title_short |
Inversion of basal friction in Antarctica using exact and incomplete adjoints of a higher‐order model |
title_full |
Inversion of basal friction in Antarctica using exact and incomplete adjoints of a higher‐order model |
title_fullStr |
Inversion of basal friction in Antarctica using exact and incomplete adjoints of a higher‐order model |
title_full_unstemmed |
Inversion of basal friction in Antarctica using exact and incomplete adjoints of a higher‐order model |
title_sort |
inversion of basal friction in antarctica using exact and incomplete adjoints of a higher‐order model |
publisher |
eScholarship, University of California |
publishDate |
2013 |
url |
https://escholarship.org/uc/item/4j39c4v4 https://escholarship.org/content/qt4j39c4v4/qt4j39c4v4.pdf https://doi.org/10.1002/jgrf.20125 |
op_coverage |
1746 - 1753 |
genre |
Antarc* Antarctic Antarctica Ice Sheet |
genre_facet |
Antarc* Antarctic Antarctica Ice Sheet |
op_source |
Journal of Geophysical Research Earth Surface, vol 118, iss 3 |
op_relation |
qt4j39c4v4 https://escholarship.org/uc/item/4j39c4v4 https://escholarship.org/content/qt4j39c4v4/qt4j39c4v4.pdf doi:10.1002/jgrf.20125 |
op_rights |
CC-BY |
op_doi |
https://doi.org/10.1002/jgrf.20125 |
container_title |
Journal of Geophysical Research: Earth Surface |
container_volume |
118 |
container_issue |
3 |
container_start_page |
1746 |
op_container_end_page |
1753 |
_version_ |
1810491672944967680 |