Five decades of strong temporal variability in the flow of Brunt Ice Shelf, Antarctica
Data showing velocity changes on the Brunt Ice Shelf (BIS), Antarctica, over the last 55 years are presented and analysed. During this period no large-scale calving events took place and the ice shelf gradually grew in size. Ice flow velocities, however, fluctuated greatly, increasing twofold betwee...
Published in: | Journal of Glaciology |
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International Glaciological Society
2017
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Online Access: | https://nrl.northumbria.ac.uk/id/eprint/34601/ https://doi.org/10.1017/jog.2016.132 https://nrl.northumbria.ac.uk/id/eprint/34601/1/five_decades_of_strong_temporal_variability_in_the_flow_of_brunt_ice_shelf_antarctica.pdf |
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ftunivnorthumb:oai:nrl.northumbria.ac.uk:34601 2023-05-15T13:56:54+02:00 Five decades of strong temporal variability in the flow of Brunt Ice Shelf, Antarctica Gudmundsson, Hilmar de Rydt, Jan Nagler, Thomas 2017-02-01 text https://nrl.northumbria.ac.uk/id/eprint/34601/ https://doi.org/10.1017/jog.2016.132 https://nrl.northumbria.ac.uk/id/eprint/34601/1/five_decades_of_strong_temporal_variability_in_the_flow_of_brunt_ice_shelf_antarctica.pdf en eng International Glaciological Society https://nrl.northumbria.ac.uk/id/eprint/34601/1/five_decades_of_strong_temporal_variability_in_the_flow_of_brunt_ice_shelf_antarctica.pdf Gudmundsson, Hilmar, de Rydt, Jan and Nagler, Thomas (2017) Five decades of strong temporal variability in the flow of Brunt Ice Shelf, Antarctica. Journal of Glaciology, 63 (237). pp. 164-175. ISSN 0022-1430 cc_by_nc_nd_4_0 CC-BY-NC-ND F800 Physical and Terrestrial Geographical and Environmental Sciences Article PeerReviewed 2017 ftunivnorthumb https://doi.org/10.1017/jog.2016.132 2022-09-25T06:07:25Z Data showing velocity changes on the Brunt Ice Shelf (BIS), Antarctica, over the last 55 years are presented and analysed. During this period no large-scale calving events took place and the ice shelf gradually grew in size. Ice flow velocities, however, fluctuated greatly, increasing twofold between 1970 and 2000, then decreasing again to previous levels by 2012 after which velocities started to increase yet again. In the observational period, velocity changes in the order of 10% a−1 have commonly been observed, and currently velocities are increasing at this rate. By modelling the ice flow numerically, we explore potential causes for the observed changes in velocity. We find that a loss of mechanical contact between the BIS and the McDonald Ice Rumples following a local calving event in 1971 would explain both the increase and the subsequent decrease in ice velocities. Other explanations involving enlargement of observed rift structures are discounted as the effects on ice flow are found to be too small and the spatial pattern of velocity change inconsistent with data. The most recent phase of acceleration remains unexplained but may potentially be related to a recent re-activation of a known rift structure within the BIS. Article in Journal/Newspaper Antarc* Antarctica Antarctica Journal Brunt Ice Shelf Ice Shelf Journal of Glaciology Northumbria University, Newcastle: Northumbria Research Link (NRL) Brunt Ice Shelf ENVELOPE(-22.500,-22.500,-74.750,-74.750) McDonald Ice Rumples ENVELOPE(-26.352,-26.352,-75.458,-75.458) Journal of Glaciology 63 237 164 175 |
institution |
Open Polar |
collection |
Northumbria University, Newcastle: Northumbria Research Link (NRL) |
op_collection_id |
ftunivnorthumb |
language |
English |
topic |
F800 Physical and Terrestrial Geographical and Environmental Sciences |
spellingShingle |
F800 Physical and Terrestrial Geographical and Environmental Sciences Gudmundsson, Hilmar de Rydt, Jan Nagler, Thomas Five decades of strong temporal variability in the flow of Brunt Ice Shelf, Antarctica |
topic_facet |
F800 Physical and Terrestrial Geographical and Environmental Sciences |
description |
Data showing velocity changes on the Brunt Ice Shelf (BIS), Antarctica, over the last 55 years are presented and analysed. During this period no large-scale calving events took place and the ice shelf gradually grew in size. Ice flow velocities, however, fluctuated greatly, increasing twofold between 1970 and 2000, then decreasing again to previous levels by 2012 after which velocities started to increase yet again. In the observational period, velocity changes in the order of 10% a−1 have commonly been observed, and currently velocities are increasing at this rate. By modelling the ice flow numerically, we explore potential causes for the observed changes in velocity. We find that a loss of mechanical contact between the BIS and the McDonald Ice Rumples following a local calving event in 1971 would explain both the increase and the subsequent decrease in ice velocities. Other explanations involving enlargement of observed rift structures are discounted as the effects on ice flow are found to be too small and the spatial pattern of velocity change inconsistent with data. The most recent phase of acceleration remains unexplained but may potentially be related to a recent re-activation of a known rift structure within the BIS. |
format |
Article in Journal/Newspaper |
author |
Gudmundsson, Hilmar de Rydt, Jan Nagler, Thomas |
author_facet |
Gudmundsson, Hilmar de Rydt, Jan Nagler, Thomas |
author_sort |
Gudmundsson, Hilmar |
title |
Five decades of strong temporal variability in the flow of Brunt Ice Shelf, Antarctica |
title_short |
Five decades of strong temporal variability in the flow of Brunt Ice Shelf, Antarctica |
title_full |
Five decades of strong temporal variability in the flow of Brunt Ice Shelf, Antarctica |
title_fullStr |
Five decades of strong temporal variability in the flow of Brunt Ice Shelf, Antarctica |
title_full_unstemmed |
Five decades of strong temporal variability in the flow of Brunt Ice Shelf, Antarctica |
title_sort |
five decades of strong temporal variability in the flow of brunt ice shelf, antarctica |
publisher |
International Glaciological Society |
publishDate |
2017 |
url |
https://nrl.northumbria.ac.uk/id/eprint/34601/ https://doi.org/10.1017/jog.2016.132 https://nrl.northumbria.ac.uk/id/eprint/34601/1/five_decades_of_strong_temporal_variability_in_the_flow_of_brunt_ice_shelf_antarctica.pdf |
long_lat |
ENVELOPE(-22.500,-22.500,-74.750,-74.750) ENVELOPE(-26.352,-26.352,-75.458,-75.458) |
geographic |
Brunt Ice Shelf McDonald Ice Rumples |
geographic_facet |
Brunt Ice Shelf McDonald Ice Rumples |
genre |
Antarc* Antarctica Antarctica Journal Brunt Ice Shelf Ice Shelf Journal of Glaciology |
genre_facet |
Antarc* Antarctica Antarctica Journal Brunt Ice Shelf Ice Shelf Journal of Glaciology |
op_relation |
https://nrl.northumbria.ac.uk/id/eprint/34601/1/five_decades_of_strong_temporal_variability_in_the_flow_of_brunt_ice_shelf_antarctica.pdf Gudmundsson, Hilmar, de Rydt, Jan and Nagler, Thomas (2017) Five decades of strong temporal variability in the flow of Brunt Ice Shelf, Antarctica. Journal of Glaciology, 63 (237). pp. 164-175. ISSN 0022-1430 |
op_rights |
cc_by_nc_nd_4_0 |
op_rightsnorm |
CC-BY-NC-ND |
op_doi |
https://doi.org/10.1017/jog.2016.132 |
container_title |
Journal of Glaciology |
container_volume |
63 |
container_issue |
237 |
container_start_page |
164 |
op_container_end_page |
175 |
_version_ |
1766264494549368832 |