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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Bibliographic Details
Published in:The Cryosphere
Main Authors: J. De Rydt, G. H. Gudmundsson, T. Nagler, J. Wuite, E. C. King
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2018
Subjects:
geo
Online Access:https://doi.org/10.5194/tc-12-505-2018
https://www.the-cryosphere.net/12/505/2018/tc-12-505-2018.pdf
https://doaj.org/article/15419e46f51842788fabbeb12105a49f
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spelling fttriple:oai:gotriple.eu:oai:doaj.org/article:15419e46f51842788fabbeb12105a49f 2023-05-15T13:52:50+02:00 Recent rift formation and impact on the structural integrity of the Brunt Ice Shelf, East Antarctica J. De Rydt G. H. Gudmundsson T. Nagler J. Wuite E. C. King 2018-02-01 https://doi.org/10.5194/tc-12-505-2018 https://www.the-cryosphere.net/12/505/2018/tc-12-505-2018.pdf https://doaj.org/article/15419e46f51842788fabbeb12105a49f en eng Copernicus Publications doi:10.5194/tc-12-505-2018 1994-0416 1994-0424 https://www.the-cryosphere.net/12/505/2018/tc-12-505-2018.pdf https://doaj.org/article/15419e46f51842788fabbeb12105a49f undefined The Cryosphere, Vol 12, Pp 505-520 (2018) geo envir Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2018 fttriple https://doi.org/10.5194/tc-12-505-2018 2023-01-22T18:11:47Z 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. Article in Journal/Newspaper Antarc* Antarctica Brunt Ice Shelf East Antarctica Ice Shelf The Cryosphere Unknown 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 Unknown
op_collection_id fttriple
language English
topic geo
envir
spellingShingle geo
envir
J. De Rydt
G. H. Gudmundsson
T. Nagler
J. Wuite
E. C. King
Recent rift formation and impact on the structural integrity of the Brunt Ice Shelf, East Antarctica
topic_facet geo
envir
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 Article in Journal/Newspaper
author J. De Rydt
G. H. Gudmundsson
T. Nagler
J. Wuite
E. C. King
author_facet J. De Rydt
G. H. Gudmundsson
T. Nagler
J. Wuite
E. C. King
author_sort J. De Rydt
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
publisher Copernicus Publications
publishDate 2018
url https://doi.org/10.5194/tc-12-505-2018
https://www.the-cryosphere.net/12/505/2018/tc-12-505-2018.pdf
https://doaj.org/article/15419e46f51842788fabbeb12105a49f
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
The Cryosphere
genre_facet Antarc*
Antarctica
Brunt Ice Shelf
East Antarctica
Ice Shelf
The Cryosphere
op_source The Cryosphere, Vol 12, Pp 505-520 (2018)
op_relation doi:10.5194/tc-12-505-2018
1994-0416
1994-0424
https://www.the-cryosphere.net/12/505/2018/tc-12-505-2018.pdf
https://doaj.org/article/15419e46f51842788fabbeb12105a49f
op_rights undefined
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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