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,...

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Published in:Journal of Geophysical Research: Earth Surface
Main Authors: Morlighem, M, Seroussi, H, Larour, E, Rignot, E
Format: Article in Journal/Newspaper
Language:unknown
Published: eScholarship, University of California 2013
Subjects:
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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spelling 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
institution Open Polar
collection University of California: eScholarship
op_collection_id 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
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