A viscoelastic model of ice stream flow with application to stick-slip motion

Stick-slip motion such as that observed at Whillans Ice Stream, WestAntarctica, is one example of transient forcing significantly affecting longer-termice-stream dynamics. We develop and present a two-dimensional map-plane viscoelasticmodel of perturbations to ice-stream dynamics suitable for simula...

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Published in:Frontiers in Earth Science
Main Authors: Ryan Thomas Walker, Byron eParizek, Richard eAlley, Sophie eNowicki
Format: Article in Journal/Newspaper
Language:English
Published: Frontiers Media S.A. 2016
Subjects:
Q
Online Access:https://doi.org/10.3389/feart.2016.00002
https://doaj.org/article/bc0e10bf50584302a5808dcb1e1ce653
id ftdoajarticles:oai:doaj.org/article:bc0e10bf50584302a5808dcb1e1ce653
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spelling ftdoajarticles:oai:doaj.org/article:bc0e10bf50584302a5808dcb1e1ce653 2023-05-15T16:40:48+02:00 A viscoelastic model of ice stream flow with application to stick-slip motion Ryan Thomas Walker Byron eParizek Richard eAlley Sophie eNowicki 2016-01-01T00:00:00Z https://doi.org/10.3389/feart.2016.00002 https://doaj.org/article/bc0e10bf50584302a5808dcb1e1ce653 EN eng Frontiers Media S.A. http://journal.frontiersin.org/Journal/10.3389/feart.2016.00002/full https://doaj.org/toc/2296-6463 2296-6463 doi:10.3389/feart.2016.00002 https://doaj.org/article/bc0e10bf50584302a5808dcb1e1ce653 Frontiers in Earth Science, Vol 4 (2016) viscoelasticity STICK-SLIP Ice rheology Whillans Ice Stream ce stream dynamics numerical ice sheet modeling Science Q article 2016 ftdoajarticles https://doi.org/10.3389/feart.2016.00002 2022-12-30T22:14:49Z Stick-slip motion such as that observed at Whillans Ice Stream, WestAntarctica, is one example of transient forcing significantly affecting longer-termice-stream dynamics. We develop and present a two-dimensional map-plane viscoelasticmodel of perturbations to ice-stream dynamics suitable for simulating andanalyzing stick-slip behavior. Model results suggest important roles in stick-slipmotion for both the elastic and viscous components of ice rheology, confirming andextending inferences drawn from simple models and observations. Elastic behaviordepends on the rate of applied stress, at times allowing significant velocity perturbationswith little change in accumulated stress perturbation; in contrast, viscousbehavior depends on total accumulated stress and can lead to changes in ice-streamthickness over many stick-slip cycles. Article in Journal/Newspaper Ice Sheet Whillans Ice Stream Directory of Open Access Journals: DOAJ Articles Whillans ENVELOPE(-64.250,-64.250,-84.450,-84.450) Whillans Ice Stream ENVELOPE(-145.000,-145.000,-83.667,-83.667) Frontiers in Earth Science 4
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic viscoelasticity
STICK-SLIP
Ice rheology
Whillans Ice Stream
ce stream dynamics
numerical ice sheet modeling
Science
Q
spellingShingle viscoelasticity
STICK-SLIP
Ice rheology
Whillans Ice Stream
ce stream dynamics
numerical ice sheet modeling
Science
Q
Ryan Thomas Walker
Byron eParizek
Richard eAlley
Sophie eNowicki
A viscoelastic model of ice stream flow with application to stick-slip motion
topic_facet viscoelasticity
STICK-SLIP
Ice rheology
Whillans Ice Stream
ce stream dynamics
numerical ice sheet modeling
Science
Q
description Stick-slip motion such as that observed at Whillans Ice Stream, WestAntarctica, is one example of transient forcing significantly affecting longer-termice-stream dynamics. We develop and present a two-dimensional map-plane viscoelasticmodel of perturbations to ice-stream dynamics suitable for simulating andanalyzing stick-slip behavior. Model results suggest important roles in stick-slipmotion for both the elastic and viscous components of ice rheology, confirming andextending inferences drawn from simple models and observations. Elastic behaviordepends on the rate of applied stress, at times allowing significant velocity perturbationswith little change in accumulated stress perturbation; in contrast, viscousbehavior depends on total accumulated stress and can lead to changes in ice-streamthickness over many stick-slip cycles.
format Article in Journal/Newspaper
author Ryan Thomas Walker
Byron eParizek
Richard eAlley
Sophie eNowicki
author_facet Ryan Thomas Walker
Byron eParizek
Richard eAlley
Sophie eNowicki
author_sort Ryan Thomas Walker
title A viscoelastic model of ice stream flow with application to stick-slip motion
title_short A viscoelastic model of ice stream flow with application to stick-slip motion
title_full A viscoelastic model of ice stream flow with application to stick-slip motion
title_fullStr A viscoelastic model of ice stream flow with application to stick-slip motion
title_full_unstemmed A viscoelastic model of ice stream flow with application to stick-slip motion
title_sort viscoelastic model of ice stream flow with application to stick-slip motion
publisher Frontiers Media S.A.
publishDate 2016
url https://doi.org/10.3389/feart.2016.00002
https://doaj.org/article/bc0e10bf50584302a5808dcb1e1ce653
long_lat ENVELOPE(-64.250,-64.250,-84.450,-84.450)
ENVELOPE(-145.000,-145.000,-83.667,-83.667)
geographic Whillans
Whillans Ice Stream
geographic_facet Whillans
Whillans Ice Stream
genre Ice Sheet
Whillans Ice Stream
genre_facet Ice Sheet
Whillans Ice Stream
op_source Frontiers in Earth Science, Vol 4 (2016)
op_relation http://journal.frontiersin.org/Journal/10.3389/feart.2016.00002/full
https://doaj.org/toc/2296-6463
2296-6463
doi:10.3389/feart.2016.00002
https://doaj.org/article/bc0e10bf50584302a5808dcb1e1ce653
op_doi https://doi.org/10.3389/feart.2016.00002
container_title Frontiers in Earth Science
container_volume 4
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