Regularized Coulomb Friction Laws for Ice Sheet Sliding: Application to Pine Island Glacier, Antarctica, [Data supporting Geophysical Res. Lett. Paper 2019GL082526R]

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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Main Author: Joughin, Ian
Format: Dataset
Language:English
Published: 2019
Subjects:
Online Access:http://hdl.handle.net/1773/43479
id ftunivwashington:oai:digital.lib.washington.edu:1773/43479
record_format openpolar
spelling ftunivwashington:oai:digital.lib.washington.edu:1773/43479 2023-05-15T13:36:48+02:00 Regularized Coulomb Friction Laws for Ice Sheet Sliding: Application to Pine Island Glacier, Antarctica, [Data supporting Geophysical Res. Lett. Paper 2019GL082526R] Joughin, Ian 2019-04-01 http://hdl.handle.net/1773/43479 en_US eng http://hdl.handle.net/1773/43479 CC0 1.0 Universal http://creativecommons.org/publicdomain/zero/1.0/ Dataset 2019 ftunivwashington 2023-03-12T18:59:08Z 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. Dataset Antarc* Antarctica Ice Sheet Pine Island Pine Island Glacier University of Washington, Seattle: ResearchWorks Pine Island Glacier ENVELOPE(-101.000,-101.000,-75.000,-75.000)
institution Open Polar
collection University of Washington, Seattle: ResearchWorks
op_collection_id ftunivwashington
language English
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.
format Dataset
author Joughin, Ian
spellingShingle Joughin, Ian
Regularized Coulomb Friction Laws for Ice Sheet Sliding: Application to Pine Island Glacier, Antarctica, [Data supporting Geophysical Res. Lett. Paper 2019GL082526R]
author_facet Joughin, Ian
author_sort Joughin, Ian
title Regularized Coulomb Friction Laws for Ice Sheet Sliding: Application to Pine Island Glacier, Antarctica, [Data supporting Geophysical Res. Lett. Paper 2019GL082526R]
title_short Regularized Coulomb Friction Laws for Ice Sheet Sliding: Application to Pine Island Glacier, Antarctica, [Data supporting Geophysical Res. Lett. Paper 2019GL082526R]
title_full Regularized Coulomb Friction Laws for Ice Sheet Sliding: Application to Pine Island Glacier, Antarctica, [Data supporting Geophysical Res. Lett. Paper 2019GL082526R]
title_fullStr Regularized Coulomb Friction Laws for Ice Sheet Sliding: Application to Pine Island Glacier, Antarctica, [Data supporting Geophysical Res. Lett. Paper 2019GL082526R]
title_full_unstemmed Regularized Coulomb Friction Laws for Ice Sheet Sliding: Application to Pine Island Glacier, Antarctica, [Data supporting Geophysical Res. Lett. Paper 2019GL082526R]
title_sort regularized coulomb friction laws for ice sheet sliding: application to pine island glacier, antarctica, [data supporting geophysical res. lett. paper 2019gl082526r]
publishDate 2019
url http://hdl.handle.net/1773/43479
long_lat ENVELOPE(-101.000,-101.000,-75.000,-75.000)
geographic Pine Island Glacier
geographic_facet Pine Island Glacier
genre Antarc*
Antarctica
Ice Sheet
Pine Island
Pine Island Glacier
genre_facet Antarc*
Antarctica
Ice Sheet
Pine Island
Pine Island Glacier
op_relation http://hdl.handle.net/1773/43479
op_rights CC0 1.0 Universal
http://creativecommons.org/publicdomain/zero/1.0/
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