Recent rift formation and impact on the structural integrity of the Brunt Ice Shelf, East Antarctica

We report on the recent reactivation of a large rift in the Brunt Ice Shelf, East Antarctica, in December 2012 and the formation of a 50 km long new rift in October 2016. Observations from a suite of ground-based and remote sensing instruments between January 2000 and July 2017 were used to track pr...

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Published in:The Cryosphere
Main Authors: Rydt, Jan, Gudmundsson, G. Hilmar, Nagler, Thomas, Wuite, Jan, King, Edward C.
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/tc-12-505-2018
https://tc.copernicus.org/articles/12/505/2018/
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spelling ftcopernicus:oai:publications.copernicus.org:tc61440 2023-05-15T13:54:27+02:00 Recent rift formation and impact on the structural integrity of the Brunt Ice Shelf, East Antarctica Rydt, Jan Gudmundsson, G. Hilmar Nagler, Thomas Wuite, Jan King, Edward C. 2018-09-27 application/pdf https://doi.org/10.5194/tc-12-505-2018 https://tc.copernicus.org/articles/12/505/2018/ eng eng doi:10.5194/tc-12-505-2018 https://tc.copernicus.org/articles/12/505/2018/ eISSN: 1994-0424 Text 2018 ftcopernicus https://doi.org/10.5194/tc-12-505-2018 2020-07-20T16:23:25Z We report on the recent reactivation of a large rift in the Brunt Ice Shelf, East Antarctica, in December 2012 and the formation of a 50 km long new rift in October 2016. Observations from a suite of ground-based and remote sensing instruments between January 2000 and July 2017 were used to track progress of both rifts in unprecedented detail. Results reveal a steady accelerating trend in their width, in combination with alternating episodes of fast ( > 600 m day −1 ) and slow propagation of the rift tip, controlled by the heterogeneous structure of the ice shelf. A numerical ice flow model and a simple propagation algorithm based on the stress distribution in the ice shelf were successfully used to hindcast the observed trajectories and to simulate future rift progression under different assumptions. Results show a high likelihood of ice loss at the McDonald Ice Rumples, the only pinning point of the ice shelf. The nascent iceberg calving and associated reduction in pinning of the Brunt Ice Shelf may provide a uniquely monitored natural experiment of ice shelf variability and provoke a deeper understanding of similar processes elsewhere in Antarctica. Text Antarc* Antarctica Brunt Ice Shelf East Antarctica Ice Shelf Copernicus Publications: E-Journals Brunt Ice Shelf ENVELOPE(-22.500,-22.500,-74.750,-74.750) East Antarctica McDonald Ice Rumples ENVELOPE(-26.352,-26.352,-75.458,-75.458) The Cryosphere 12 2 505 520
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description We report on the recent reactivation of a large rift in the Brunt Ice Shelf, East Antarctica, in December 2012 and the formation of a 50 km long new rift in October 2016. Observations from a suite of ground-based and remote sensing instruments between January 2000 and July 2017 were used to track progress of both rifts in unprecedented detail. Results reveal a steady accelerating trend in their width, in combination with alternating episodes of fast ( > 600 m day −1 ) and slow propagation of the rift tip, controlled by the heterogeneous structure of the ice shelf. A numerical ice flow model and a simple propagation algorithm based on the stress distribution in the ice shelf were successfully used to hindcast the observed trajectories and to simulate future rift progression under different assumptions. Results show a high likelihood of ice loss at the McDonald Ice Rumples, the only pinning point of the ice shelf. The nascent iceberg calving and associated reduction in pinning of the Brunt Ice Shelf may provide a uniquely monitored natural experiment of ice shelf variability and provoke a deeper understanding of similar processes elsewhere in Antarctica.
format Text
author Rydt, Jan
Gudmundsson, G. Hilmar
Nagler, Thomas
Wuite, Jan
King, Edward C.
spellingShingle Rydt, Jan
Gudmundsson, G. Hilmar
Nagler, Thomas
Wuite, Jan
King, Edward C.
Recent rift formation and impact on the structural integrity of the Brunt Ice Shelf, East Antarctica
author_facet Rydt, Jan
Gudmundsson, G. Hilmar
Nagler, Thomas
Wuite, Jan
King, Edward C.
author_sort Rydt, Jan
title Recent rift formation and impact on the structural integrity of the Brunt Ice Shelf, East Antarctica
title_short Recent rift formation and impact on the structural integrity of the Brunt Ice Shelf, East Antarctica
title_full Recent rift formation and impact on the structural integrity of the Brunt Ice Shelf, East Antarctica
title_fullStr Recent rift formation and impact on the structural integrity of the Brunt Ice Shelf, East Antarctica
title_full_unstemmed Recent rift formation and impact on the structural integrity of the Brunt Ice Shelf, East Antarctica
title_sort recent rift formation and impact on the structural integrity of the brunt ice shelf, east antarctica
publishDate 2018
url https://doi.org/10.5194/tc-12-505-2018
https://tc.copernicus.org/articles/12/505/2018/
long_lat ENVELOPE(-22.500,-22.500,-74.750,-74.750)
ENVELOPE(-26.352,-26.352,-75.458,-75.458)
geographic Brunt Ice Shelf
East Antarctica
McDonald Ice Rumples
geographic_facet Brunt Ice Shelf
East Antarctica
McDonald Ice Rumples
genre Antarc*
Antarctica
Brunt Ice Shelf
East Antarctica
Ice Shelf
genre_facet Antarc*
Antarctica
Brunt Ice Shelf
East Antarctica
Ice Shelf
op_source eISSN: 1994-0424
op_relation doi:10.5194/tc-12-505-2018
https://tc.copernicus.org/articles/12/505/2018/
op_doi https://doi.org/10.5194/tc-12-505-2018
container_title The Cryosphere
container_volume 12
container_issue 2
container_start_page 505
op_container_end_page 520
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