Application of a regularised Coulomb sliding law to Jakobshavn Isbræ, West Greenland

Reliable projections of future sea level rise from the polar ice sheets depend on the ability of ice sheet models to accurately reproduce flow dynamics in an evolving ice sheet system. Ice sheet models are sensitive to the choice of the basal sliding law, which remains a significant source of uncert...

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Main Authors: Trevers, Matt, Payne, Antony J., Cornford, Stephen L.
Format: Text
Language:English
Published: 2024
Subjects:
Online Access:https://doi.org/10.5194/egusphere-2024-1040
https://egusphere.copernicus.org/preprints/2024/egusphere-2024-1040/
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author Trevers, Matt
Payne, Antony J.
Cornford, Stephen L.
author_facet Trevers, Matt
Payne, Antony J.
Cornford, Stephen L.
author_sort Trevers, Matt
collection Copernicus Publications: E-Journals
description Reliable projections of future sea level rise from the polar ice sheets depend on the ability of ice sheet models to accurately reproduce flow dynamics in an evolving ice sheet system. Ice sheet models are sensitive to the choice of the basal sliding law, which remains a significant source of uncertainty. In this study we apply a range of sliding laws to a hindcast model of Jakobshavn Isbræ, western Greenland, from 2009 to 2018. We demonstrate that a linear viscous sliding law requires the assimilation of regular velocity observations into the model in order to reproduce the observed large seasonal and inter-annual variations in flow speed. This requirement introduces a major limitation for producing accurate future projections. A regularised Coulomb friction law, in which basal traction has an upper limit, is able to more accurately reproduce the range of speeds from 2012 to 2015, the period of peak flow and maximal retreat, without the requirement for assimilating regular observations. Additionally, we find evidence that the speed at which sliding transitions between power-law and Coulomb regimes may vary spatially and temporally. These results point towards the possible form of an ideal sliding parameterisation for accurately modelling fast-flowing glaciers and ice streams, although determining this is beyond the scope of this study.
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genre Greenland
Ice Sheet
Jakobshavn
Jakobshavn isbræ
genre_facet Greenland
Ice Sheet
Jakobshavn
Jakobshavn isbræ
geographic Greenland
Jakobshavn Isbræ
geographic_facet Greenland
Jakobshavn Isbræ
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institution Open Polar
language English
long_lat ENVELOPE(-49.917,-49.917,69.167,69.167)
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spelling ftcopernicus:oai:publications.copernicus.org:egusphere119285 2025-01-16T22:10:43+00:00 Application of a regularised Coulomb sliding law to Jakobshavn Isbræ, West Greenland Trevers, Matt Payne, Antony J. Cornford, Stephen L. 2024-11-08 application/pdf https://doi.org/10.5194/egusphere-2024-1040 https://egusphere.copernicus.org/preprints/2024/egusphere-2024-1040/ eng eng eISSN: Text 2024 ftcopernicus https://doi.org/10.5194/egusphere-2024-1040 2024-11-13T01:04:06Z Reliable projections of future sea level rise from the polar ice sheets depend on the ability of ice sheet models to accurately reproduce flow dynamics in an evolving ice sheet system. Ice sheet models are sensitive to the choice of the basal sliding law, which remains a significant source of uncertainty. In this study we apply a range of sliding laws to a hindcast model of Jakobshavn Isbræ, western Greenland, from 2009 to 2018. We demonstrate that a linear viscous sliding law requires the assimilation of regular velocity observations into the model in order to reproduce the observed large seasonal and inter-annual variations in flow speed. This requirement introduces a major limitation for producing accurate future projections. A regularised Coulomb friction law, in which basal traction has an upper limit, is able to more accurately reproduce the range of speeds from 2012 to 2015, the period of peak flow and maximal retreat, without the requirement for assimilating regular observations. Additionally, we find evidence that the speed at which sliding transitions between power-law and Coulomb regimes may vary spatially and temporally. These results point towards the possible form of an ideal sliding parameterisation for accurately modelling fast-flowing glaciers and ice streams, although determining this is beyond the scope of this study. Text Greenland Ice Sheet Jakobshavn Jakobshavn isbræ Copernicus Publications: E-Journals Greenland Jakobshavn Isbræ ENVELOPE(-49.917,-49.917,69.167,69.167)
spellingShingle Trevers, Matt
Payne, Antony J.
Cornford, Stephen L.
Application of a regularised Coulomb sliding law to Jakobshavn Isbræ, West Greenland
title Application of a regularised Coulomb sliding law to Jakobshavn Isbræ, West Greenland
title_full Application of a regularised Coulomb sliding law to Jakobshavn Isbræ, West Greenland
title_fullStr Application of a regularised Coulomb sliding law to Jakobshavn Isbræ, West Greenland
title_full_unstemmed Application of a regularised Coulomb sliding law to Jakobshavn Isbræ, West Greenland
title_short Application of a regularised Coulomb sliding law to Jakobshavn Isbræ, West Greenland
title_sort application of a regularised coulomb sliding law to jakobshavn isbræ, west greenland
url https://doi.org/10.5194/egusphere-2024-1040
https://egusphere.copernicus.org/preprints/2024/egusphere-2024-1040/