Tidal modulation of ice shelf buttressing stresses

Ocean tides influence the flow of marine-terminating glaciers. Observations indicate that the large fortnightly variations in ice flow at Rutford Ice Stream in West Antarctica originate in the floating ice shelf. We show that nonlinear variations in ice shelf buttressing driven by tides can produce...

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Bibliographic Details
Published in:Annals of Glaciology
Main Authors: Alexander A. Robel, Victor C. Tsai, Brent Minchew, Mark Simons
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press 2017
Subjects:
Online Access:https://doi.org/10.1017/aog.2017.22
https://doaj.org/article/26ffec4925954ccdb2ce547dfc96da6d
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spelling ftdoajarticles:oai:doaj.org/article:26ffec4925954ccdb2ce547dfc96da6d 2023-05-15T13:29:30+02:00 Tidal modulation of ice shelf buttressing stresses Alexander A. Robel Victor C. Tsai Brent Minchew Mark Simons 2017-04-01T00:00:00Z https://doi.org/10.1017/aog.2017.22 https://doaj.org/article/26ffec4925954ccdb2ce547dfc96da6d EN eng Cambridge University Press https://www.cambridge.org/core/product/identifier/S0260305517000222/type/journal_article https://doaj.org/toc/0260-3055 https://doaj.org/toc/1727-5644 doi:10.1017/aog.2017.22 0260-3055 1727-5644 https://doaj.org/article/26ffec4925954ccdb2ce547dfc96da6d Annals of Glaciology, Vol 58, Pp 12-20 (2017) Antarctic glaciology ice dynamics ice/ocean interactions ice-sheet modelling ice shelves Meteorology. Climatology QC851-999 article 2017 ftdoajarticles https://doi.org/10.1017/aog.2017.22 2023-03-12T01:31:57Z Ocean tides influence the flow of marine-terminating glaciers. Observations indicate that the large fortnightly variations in ice flow at Rutford Ice Stream in West Antarctica originate in the floating ice shelf. We show that nonlinear variations in ice shelf buttressing driven by tides can produce such fortnightly variations in ice flow. These nonlinearities in the tidal modulation of buttressing stresses can be caused by asymmetries in the contact stress from migration of the grounding line and bathymetric pinning points beneath the ice shelf. Using a simple viscoelastic model, we demonstrate that a combination of buttressing and hydrostatic stress variations can explain a diverse range of tidal variations in ice shelf flow, including the period, phase and amplitude of flow variations observed at Rutford and Bindschadler Ice Streams. Article in Journal/Newspaper Annals of Glaciology Antarc* Antarctic Antarctica Ice Sheet Ice Shelf Ice Shelves Rutford Ice Stream West Antarctica Directory of Open Access Journals: DOAJ Articles Antarctic West Antarctica Rutford ENVELOPE(-85.300,-85.300,-78.600,-78.600) Rutford Ice Stream ENVELOPE(-80.000,-80.000,-79.167,-79.167) Annals of Glaciology 58 74 12 20
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Antarctic glaciology
ice dynamics
ice/ocean interactions
ice-sheet modelling
ice shelves
Meteorology. Climatology
QC851-999
spellingShingle Antarctic glaciology
ice dynamics
ice/ocean interactions
ice-sheet modelling
ice shelves
Meteorology. Climatology
QC851-999
Alexander A. Robel
Victor C. Tsai
Brent Minchew
Mark Simons
Tidal modulation of ice shelf buttressing stresses
topic_facet Antarctic glaciology
ice dynamics
ice/ocean interactions
ice-sheet modelling
ice shelves
Meteorology. Climatology
QC851-999
description Ocean tides influence the flow of marine-terminating glaciers. Observations indicate that the large fortnightly variations in ice flow at Rutford Ice Stream in West Antarctica originate in the floating ice shelf. We show that nonlinear variations in ice shelf buttressing driven by tides can produce such fortnightly variations in ice flow. These nonlinearities in the tidal modulation of buttressing stresses can be caused by asymmetries in the contact stress from migration of the grounding line and bathymetric pinning points beneath the ice shelf. Using a simple viscoelastic model, we demonstrate that a combination of buttressing and hydrostatic stress variations can explain a diverse range of tidal variations in ice shelf flow, including the period, phase and amplitude of flow variations observed at Rutford and Bindschadler Ice Streams.
format Article in Journal/Newspaper
author Alexander A. Robel
Victor C. Tsai
Brent Minchew
Mark Simons
author_facet Alexander A. Robel
Victor C. Tsai
Brent Minchew
Mark Simons
author_sort Alexander A. Robel
title Tidal modulation of ice shelf buttressing stresses
title_short Tidal modulation of ice shelf buttressing stresses
title_full Tidal modulation of ice shelf buttressing stresses
title_fullStr Tidal modulation of ice shelf buttressing stresses
title_full_unstemmed Tidal modulation of ice shelf buttressing stresses
title_sort tidal modulation of ice shelf buttressing stresses
publisher Cambridge University Press
publishDate 2017
url https://doi.org/10.1017/aog.2017.22
https://doaj.org/article/26ffec4925954ccdb2ce547dfc96da6d
long_lat ENVELOPE(-85.300,-85.300,-78.600,-78.600)
ENVELOPE(-80.000,-80.000,-79.167,-79.167)
geographic Antarctic
West Antarctica
Rutford
Rutford Ice Stream
geographic_facet Antarctic
West Antarctica
Rutford
Rutford Ice Stream
genre Annals of Glaciology
Antarc*
Antarctic
Antarctica
Ice Sheet
Ice Shelf
Ice Shelves
Rutford Ice Stream
West Antarctica
genre_facet Annals of Glaciology
Antarc*
Antarctic
Antarctica
Ice Sheet
Ice Shelf
Ice Shelves
Rutford Ice Stream
West Antarctica
op_source Annals of Glaciology, Vol 58, Pp 12-20 (2017)
op_relation https://www.cambridge.org/core/product/identifier/S0260305517000222/type/journal_article
https://doaj.org/toc/0260-3055
https://doaj.org/toc/1727-5644
doi:10.1017/aog.2017.22
0260-3055
1727-5644
https://doaj.org/article/26ffec4925954ccdb2ce547dfc96da6d
op_doi https://doi.org/10.1017/aog.2017.22
container_title Annals of Glaciology
container_volume 58
container_issue 74
container_start_page 12
op_container_end_page 20
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