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...
Published in: | Frontiers in Earth Science |
---|---|
Main Authors: | , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Frontiers Media S.A.
2016
|
Subjects: | |
Online Access: | https://doi.org/10.3389/feart.2016.00002 https://doaj.org/article/bc0e10bf50584302a5808dcb1e1ce653 |
id |
ftdoajarticles:oai:doaj.org/article:bc0e10bf50584302a5808dcb1e1ce653 |
---|---|
record_format |
openpolar |
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 |
_version_ |
1766031212703383552 |