Modeling Antarctic tides in response to ice shelf thinning and retreat
This is the final version of the article. Available from American Geophysical Union via the DOI in this record. Tides play an important role in ice sheet dynamics by modulating ice stream velocity, fracturing, and moving ice shelves and mixing water beneath them. Any changes in ice shelf extent or t...
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ftunivexeter:oai:ore.exeter.ac.uk:10871/26364 2024-09-15T17:46:47+00:00 Modeling Antarctic tides in response to ice shelf thinning and retreat Rosier, SHR Green, JAM Scourse, JD Winkelmann, R 2014 http://hdl.handle.net/10871/26364 https://doi.org/10.1002/2013JC009240 en eng American Geophysical Union (AGU) / Wiley Vol. 119 (1), pp. 87 - 97 doi:10.1002/2013JC009240 http://hdl.handle.net/10871/26364 Journal of Geophysical Research: Oceans Open access under a Creative Commons licence: https://creativecommons.org/licenses/by/3.0/ Article 2014 ftunivexeter https://doi.org/10.1002/2013JC009240 2024-07-29T03:24:15Z This is the final version of the article. Available from American Geophysical Union via the DOI in this record. Tides play an important role in ice sheet dynamics by modulating ice stream velocity, fracturing, and moving ice shelves and mixing water beneath them. Any changes in ice shelf extent or thickness will alter the tidal dynamics through modification of water column thickness and coastal topography but these will in turn feed back onto the overall ice shelf stability. Here, we show that removal or reduction in extent and/or thickness of the Ross and Ronne-Filchner ice shelves would have a significant impact on the tides around Antarctica. The Ronne-Filchner appears particularly vulnerable, with an increase in M2 amplitude of over 0.5 m beneath much of the ice shelf potentially leading to tidally induced feedbacks on ice shelf/sheet dynamics. These results highlight the importance of understanding tidal feedbacks on ice shelves/streams due to their influence on ice sheet dynamics. Funding was provided by the Natural Environmental Research Council through grants NE/J/500203/1 (SHRR PhD studentship) and NE/F/014821/1 (JAMG Advanced Fellowship). J.A.M.G. and J.D.S. acknowledge funding from the Climate Change Consortium of Wales (C3W), and R.W. received support from the German Federal Ministry of Education and Research (BMBF grant 01LP1171A). Comments from Paul Holland and three anonymous reviewers greatly improved the manuscript. Article in Journal/Newspaper Antarc* Antarctic Antarctica Ice Sheet Ice Shelf Ice Shelves University of Exeter: Open Research Exeter (ORE) Journal of Geophysical Research: Oceans 119 1 87 97 |
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University of Exeter: Open Research Exeter (ORE) |
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English |
description |
This is the final version of the article. Available from American Geophysical Union via the DOI in this record. Tides play an important role in ice sheet dynamics by modulating ice stream velocity, fracturing, and moving ice shelves and mixing water beneath them. Any changes in ice shelf extent or thickness will alter the tidal dynamics through modification of water column thickness and coastal topography but these will in turn feed back onto the overall ice shelf stability. Here, we show that removal or reduction in extent and/or thickness of the Ross and Ronne-Filchner ice shelves would have a significant impact on the tides around Antarctica. The Ronne-Filchner appears particularly vulnerable, with an increase in M2 amplitude of over 0.5 m beneath much of the ice shelf potentially leading to tidally induced feedbacks on ice shelf/sheet dynamics. These results highlight the importance of understanding tidal feedbacks on ice shelves/streams due to their influence on ice sheet dynamics. Funding was provided by the Natural Environmental Research Council through grants NE/J/500203/1 (SHRR PhD studentship) and NE/F/014821/1 (JAMG Advanced Fellowship). J.A.M.G. and J.D.S. acknowledge funding from the Climate Change Consortium of Wales (C3W), and R.W. received support from the German Federal Ministry of Education and Research (BMBF grant 01LP1171A). Comments from Paul Holland and three anonymous reviewers greatly improved the manuscript. |
format |
Article in Journal/Newspaper |
author |
Rosier, SHR Green, JAM Scourse, JD Winkelmann, R |
spellingShingle |
Rosier, SHR Green, JAM Scourse, JD Winkelmann, R Modeling Antarctic tides in response to ice shelf thinning and retreat |
author_facet |
Rosier, SHR Green, JAM Scourse, JD Winkelmann, R |
author_sort |
Rosier, SHR |
title |
Modeling Antarctic tides in response to ice shelf thinning and retreat |
title_short |
Modeling Antarctic tides in response to ice shelf thinning and retreat |
title_full |
Modeling Antarctic tides in response to ice shelf thinning and retreat |
title_fullStr |
Modeling Antarctic tides in response to ice shelf thinning and retreat |
title_full_unstemmed |
Modeling Antarctic tides in response to ice shelf thinning and retreat |
title_sort |
modeling antarctic tides in response to ice shelf thinning and retreat |
publisher |
American Geophysical Union (AGU) / Wiley |
publishDate |
2014 |
url |
http://hdl.handle.net/10871/26364 https://doi.org/10.1002/2013JC009240 |
genre |
Antarc* Antarctic Antarctica Ice Sheet Ice Shelf Ice Shelves |
genre_facet |
Antarc* Antarctic Antarctica Ice Sheet Ice Shelf Ice Shelves |
op_relation |
Vol. 119 (1), pp. 87 - 97 doi:10.1002/2013JC009240 http://hdl.handle.net/10871/26364 Journal of Geophysical Research: Oceans |
op_rights |
Open access under a Creative Commons licence: https://creativecommons.org/licenses/by/3.0/ |
op_doi |
https://doi.org/10.1002/2013JC009240 |
container_title |
Journal of Geophysical Research: Oceans |
container_volume |
119 |
container_issue |
1 |
container_start_page |
87 |
op_container_end_page |
97 |
_version_ |
1810495146549051392 |