Brief Communication: Rapid acceleration of the Brunt Ice Shelf after calving of iceberg A-81
The Brunt Ice Shelf, Antarctica, accelerated rapidly from 900 m a -1 to 1500 m a -1 during six months following the calving of a 1500 km 2 iceberg on 22 nd January 2023. Initially, the rate of acceleration increased by a factor of ten, with a second, smaller calving at the end of June 2023 leading t...
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ftcopernicus:oai:publications.copernicus.org:egusphere114433 2023-10-09T21:47:11+02:00 Brief Communication: Rapid acceleration of the Brunt Ice Shelf after calving of iceberg A-81 Marsh, Oliver J. Luckman, Adrian J. Hodgson, Dominic A. 2023-09-13 application/pdf https://doi.org/10.5194/egusphere-2023-1949 https://egusphere.copernicus.org/preprints/2023/egusphere-2023-1949/ eng eng doi:10.5194/egusphere-2023-1949 https://egusphere.copernicus.org/preprints/2023/egusphere-2023-1949/ eISSN: Text 2023 ftcopernicus https://doi.org/10.5194/egusphere-2023-1949 2023-09-18T16:24:16Z The Brunt Ice Shelf, Antarctica, accelerated rapidly from 900 m a -1 to 1500 m a -1 during six months following the calving of a 1500 km 2 iceberg on 22 nd January 2023. Initially, the rate of acceleration increased by a factor of ten, with a second, smaller calving at the end of June 2023 leading to further tripling of acceleration. The acceleration is caused by reduction of buttressing at the McDonald Ice Rumples due to loss of contact with the sea floor and has led to high strain rates to the south, with potential consequences for the stability of the remaining ice shelf. Text Antarc* Antarctica Brunt Ice Shelf Ice Shelf Copernicus Publications: E-Journals Brunt Ice Shelf ENVELOPE(-22.500,-22.500,-74.750,-74.750) McDonald Ice Rumples ENVELOPE(-26.352,-26.352,-75.458,-75.458) |
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Open Polar |
collection |
Copernicus Publications: E-Journals |
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ftcopernicus |
language |
English |
description |
The Brunt Ice Shelf, Antarctica, accelerated rapidly from 900 m a -1 to 1500 m a -1 during six months following the calving of a 1500 km 2 iceberg on 22 nd January 2023. Initially, the rate of acceleration increased by a factor of ten, with a second, smaller calving at the end of June 2023 leading to further tripling of acceleration. The acceleration is caused by reduction of buttressing at the McDonald Ice Rumples due to loss of contact with the sea floor and has led to high strain rates to the south, with potential consequences for the stability of the remaining ice shelf. |
format |
Text |
author |
Marsh, Oliver J. Luckman, Adrian J. Hodgson, Dominic A. |
spellingShingle |
Marsh, Oliver J. Luckman, Adrian J. Hodgson, Dominic A. Brief Communication: Rapid acceleration of the Brunt Ice Shelf after calving of iceberg A-81 |
author_facet |
Marsh, Oliver J. Luckman, Adrian J. Hodgson, Dominic A. |
author_sort |
Marsh, Oliver J. |
title |
Brief Communication: Rapid acceleration of the Brunt Ice Shelf after calving of iceberg A-81 |
title_short |
Brief Communication: Rapid acceleration of the Brunt Ice Shelf after calving of iceberg A-81 |
title_full |
Brief Communication: Rapid acceleration of the Brunt Ice Shelf after calving of iceberg A-81 |
title_fullStr |
Brief Communication: Rapid acceleration of the Brunt Ice Shelf after calving of iceberg A-81 |
title_full_unstemmed |
Brief Communication: Rapid acceleration of the Brunt Ice Shelf after calving of iceberg A-81 |
title_sort |
brief communication: rapid acceleration of the brunt ice shelf after calving of iceberg a-81 |
publishDate |
2023 |
url |
https://doi.org/10.5194/egusphere-2023-1949 https://egusphere.copernicus.org/preprints/2023/egusphere-2023-1949/ |
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 Brunt Ice Shelf Ice Shelf |
genre_facet |
Antarc* Antarctica Brunt Ice Shelf Ice Shelf |
op_source |
eISSN: |
op_relation |
doi:10.5194/egusphere-2023-1949 https://egusphere.copernicus.org/preprints/2023/egusphere-2023-1949/ |
op_doi |
https://doi.org/10.5194/egusphere-2023-1949 |
_version_ |
1779310067680542720 |