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...
Published in: | Annals of Glaciology |
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Language: | English |
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Cambridge University Press
2017
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Online Access: | https://doi.org/10.1017/aog.2017.22 https://doaj.org/article/26ffec4925954ccdb2ce547dfc96da6d |
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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 |
_version_ |
1766000956810461184 |