Regularized Coulomb Friction Laws for Ice Sheet Sliding: Application to Pine Island Glacier, Antarctica

The choice of the best basal friction law to use in ice‐sheet models remains a source of uncertainty in projections of sea level. The parameters in commonly used friction laws can produce a broad range of behavior and are poorly constrained. Here we use a time series of elevation and speed data to e...

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Published in:Geophysical Research Letters
Main Authors: Joughin, Ian, Smith, Benjamin E., Schoof, Christian G.
Format: Text
Language:English
Published: John Wiley and Sons Inc. 2019
Subjects:
Online Access:http://www.ncbi.nlm.nih.gov/pmc/articles/PMC6582595/
https://doi.org/10.1029/2019GL082526
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author Joughin, Ian
Smith, Benjamin E.
Schoof, Christian G.
author_facet Joughin, Ian
Smith, Benjamin E.
Schoof, Christian G.
author_sort Joughin, Ian
collection PubMed Central (PMC)
container_issue 9
container_start_page 4764
container_title Geophysical Research Letters
container_volume 46
description The choice of the best basal friction law to use in ice‐sheet models remains a source of uncertainty in projections of sea level. The parameters in commonly used friction laws can produce a broad range of behavior and are poorly constrained. Here we use a time series of elevation and speed data to examine the simulated transient response of Pine Island Glacier, Antarctica, to a loss of basal traction as its grounding line retreats. We evaluate a variety of friction laws, which produces a diversity of responses, to determine which best reproduces the observed speedup when forced with the observed thinning. Forms of the commonly used power law friction provide much larger model‐data disagreement than less commonly used regularized Coulomb friction in which cavitation effects yield an upper bound on basal friction. Thus, adoption of such friction laws could substantially improve the fidelity of large‐scale simulations to determine future sea level.
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genre Antarc*
Antarctica
Ice Sheet
Pine Island
Pine Island Glacier
genre_facet Antarc*
Antarctica
Ice Sheet
Pine Island
Pine Island Glacier
geographic Pine Island Glacier
geographic_facet Pine Island Glacier
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institution Open Polar
language English
long_lat ENVELOPE(-101.000,-101.000,-75.000,-75.000)
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op_doi https://doi.org/10.1029/2019GL082526
op_relation http://www.ncbi.nlm.nih.gov/pmc/articles/PMC6582595/
http://dx.doi.org/10.1029/2019GL082526
op_rights ©2019. The Authors.
This is an open access article under the terms of the http://creativecommons.org/licenses/by-nc-nd/4.0/ License, which permits use and distribution in any medium, provided the original work is properly cited, the use is non‐commercial and no modifications or adaptations are made.
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spelling ftpubmed:oai:pubmedcentral.nih.gov:6582595 2025-01-16T19:01:13+00:00 Regularized Coulomb Friction Laws for Ice Sheet Sliding: Application to Pine Island Glacier, Antarctica Joughin, Ian Smith, Benjamin E. Schoof, Christian G. 2019-05-13 http://www.ncbi.nlm.nih.gov/pmc/articles/PMC6582595/ https://doi.org/10.1029/2019GL082526 en eng John Wiley and Sons Inc. http://www.ncbi.nlm.nih.gov/pmc/articles/PMC6582595/ http://dx.doi.org/10.1029/2019GL082526 ©2019. The Authors. This is an open access article under the terms of the http://creativecommons.org/licenses/by-nc-nd/4.0/ License, which permits use and distribution in any medium, provided the original work is properly cited, the use is non‐commercial and no modifications or adaptations are made. CC-BY-NC-ND Research Letters Text 2019 ftpubmed https://doi.org/10.1029/2019GL082526 2019-06-30T01:03:17Z The choice of the best basal friction law to use in ice‐sheet models remains a source of uncertainty in projections of sea level. The parameters in commonly used friction laws can produce a broad range of behavior and are poorly constrained. Here we use a time series of elevation and speed data to examine the simulated transient response of Pine Island Glacier, Antarctica, to a loss of basal traction as its grounding line retreats. We evaluate a variety of friction laws, which produces a diversity of responses, to determine which best reproduces the observed speedup when forced with the observed thinning. Forms of the commonly used power law friction provide much larger model‐data disagreement than less commonly used regularized Coulomb friction in which cavitation effects yield an upper bound on basal friction. Thus, adoption of such friction laws could substantially improve the fidelity of large‐scale simulations to determine future sea level. Text Antarc* Antarctica Ice Sheet Pine Island Pine Island Glacier PubMed Central (PMC) Pine Island Glacier ENVELOPE(-101.000,-101.000,-75.000,-75.000) Geophysical Research Letters 46 9 4764 4771
spellingShingle Research Letters
Joughin, Ian
Smith, Benjamin E.
Schoof, Christian G.
Regularized Coulomb Friction Laws for Ice Sheet Sliding: Application to Pine Island Glacier, Antarctica
title Regularized Coulomb Friction Laws for Ice Sheet Sliding: Application to Pine Island Glacier, Antarctica
title_full Regularized Coulomb Friction Laws for Ice Sheet Sliding: Application to Pine Island Glacier, Antarctica
title_fullStr Regularized Coulomb Friction Laws for Ice Sheet Sliding: Application to Pine Island Glacier, Antarctica
title_full_unstemmed Regularized Coulomb Friction Laws for Ice Sheet Sliding: Application to Pine Island Glacier, Antarctica
title_short Regularized Coulomb Friction Laws for Ice Sheet Sliding: Application to Pine Island Glacier, Antarctica
title_sort regularized coulomb friction laws for ice sheet sliding: application to pine island glacier, antarctica
topic Research Letters
topic_facet Research Letters
url http://www.ncbi.nlm.nih.gov/pmc/articles/PMC6582595/
https://doi.org/10.1029/2019GL082526