Ocean forced variability of Totten Glacier mass loss
A large volume of the East Antarctic Ice Sheet drains through the Totten Glacier (TG) and is thought to be a potential source of substantial global sea level rise over the coming centuries. We show the flow and surface height of floating part of TG, which buttresses the grounded component, have vari...
Published in: | Geological Society, London, Special Publications |
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Online Access: | http://hdl.handle.net/10044/1/44394 https://doi.org/10.1144/SP461.6 |
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ftimperialcol:oai:spiral.imperial.ac.uk:10044/1/44394 2023-05-15T13:50:12+02:00 Ocean forced variability of Totten Glacier mass loss Roberts, J Galton-Fenzi, B Paolo, F Donnelly, C Gwyther, D Padman, L Young, D Warner, R Greenbaum, J Fricker, H Payne, AJ Cornford, S Le Brocq, A Van Ommen, T Blankenship, DD Siegert, MJ 2017-02-07 http://hdl.handle.net/10044/1/44394 https://doi.org/10.1144/SP461.6 unknown The Geological Society Special Publication - Geological Society of London 0305-8719 http://hdl.handle.net/10044/1/44394 doi:10.1144/SP461.6 © 2018 The Author(s). Published by The Geological Society of London https://creativecommons.org/licenses/by/3.0/ 186 175 Journal Article 2017 ftimperialcol https://doi.org/10.1144/SP461.6 2023-03-23T23:43:00Z A large volume of the East Antarctic Ice Sheet drains through the Totten Glacier (TG) and is thought to be a potential source of substantial global sea level rise over the coming centuries. We show the flow and surface height of floating part of TG, which buttresses the grounded component, have varied substantially over two decades (1989–2011), with variations in surface height and basal melt rates highly anti-correlated (r=0.70, p <0.05). Coupled glacier/ice-shelf simulations confirm ice flow and thickness respond to both basal melting of the ice shelf and grounding on bed obstacles. We conclude the observed variability of TG is primarily ocean-driven and enhanced ice-sheet dynamism, leading to upstream grounded ice loss, will occur from the region with ocean warming. Article in Journal/Newspaper Antarc* Antarctic Ice Sheet Ice Shelf Totten Glacier Imperial College London: Spiral Antarctic East Antarctic Ice Sheet Totten Glacier ENVELOPE(116.333,116.333,-66.833,-66.833) Geological Society, London, Special Publications 461 1 175 186 |
institution |
Open Polar |
collection |
Imperial College London: Spiral |
op_collection_id |
ftimperialcol |
language |
unknown |
description |
A large volume of the East Antarctic Ice Sheet drains through the Totten Glacier (TG) and is thought to be a potential source of substantial global sea level rise over the coming centuries. We show the flow and surface height of floating part of TG, which buttresses the grounded component, have varied substantially over two decades (1989–2011), with variations in surface height and basal melt rates highly anti-correlated (r=0.70, p <0.05). Coupled glacier/ice-shelf simulations confirm ice flow and thickness respond to both basal melting of the ice shelf and grounding on bed obstacles. We conclude the observed variability of TG is primarily ocean-driven and enhanced ice-sheet dynamism, leading to upstream grounded ice loss, will occur from the region with ocean warming. |
format |
Article in Journal/Newspaper |
author |
Roberts, J Galton-Fenzi, B Paolo, F Donnelly, C Gwyther, D Padman, L Young, D Warner, R Greenbaum, J Fricker, H Payne, AJ Cornford, S Le Brocq, A Van Ommen, T Blankenship, DD Siegert, MJ |
spellingShingle |
Roberts, J Galton-Fenzi, B Paolo, F Donnelly, C Gwyther, D Padman, L Young, D Warner, R Greenbaum, J Fricker, H Payne, AJ Cornford, S Le Brocq, A Van Ommen, T Blankenship, DD Siegert, MJ Ocean forced variability of Totten Glacier mass loss |
author_facet |
Roberts, J Galton-Fenzi, B Paolo, F Donnelly, C Gwyther, D Padman, L Young, D Warner, R Greenbaum, J Fricker, H Payne, AJ Cornford, S Le Brocq, A Van Ommen, T Blankenship, DD Siegert, MJ |
author_sort |
Roberts, J |
title |
Ocean forced variability of Totten Glacier mass loss |
title_short |
Ocean forced variability of Totten Glacier mass loss |
title_full |
Ocean forced variability of Totten Glacier mass loss |
title_fullStr |
Ocean forced variability of Totten Glacier mass loss |
title_full_unstemmed |
Ocean forced variability of Totten Glacier mass loss |
title_sort |
ocean forced variability of totten glacier mass loss |
publisher |
The Geological Society |
publishDate |
2017 |
url |
http://hdl.handle.net/10044/1/44394 https://doi.org/10.1144/SP461.6 |
long_lat |
ENVELOPE(116.333,116.333,-66.833,-66.833) |
geographic |
Antarctic East Antarctic Ice Sheet Totten Glacier |
geographic_facet |
Antarctic East Antarctic Ice Sheet Totten Glacier |
genre |
Antarc* Antarctic Ice Sheet Ice Shelf Totten Glacier |
genre_facet |
Antarc* Antarctic Ice Sheet Ice Shelf Totten Glacier |
op_source |
186 175 |
op_relation |
Special Publication - Geological Society of London 0305-8719 http://hdl.handle.net/10044/1/44394 doi:10.1144/SP461.6 |
op_rights |
© 2018 The Author(s). Published by The Geological Society of London https://creativecommons.org/licenses/by/3.0/ |
op_doi |
https://doi.org/10.1144/SP461.6 |
container_title |
Geological Society, London, Special Publications |
container_volume |
461 |
container_issue |
1 |
container_start_page |
175 |
op_container_end_page |
186 |
_version_ |
1766253217325252608 |