Brief communication: Rapid acceleration of the Brunt Ice Shelf after calving of iceberg A-81
The Brunt Ice Shelf, Antarctica, accelerated rapidly from a velocity of 900 to 1500 m a−1 during 6 months, following calving of a 1500 km2 iceberg on 22 January 2023. The immediate response to calving was observed as a change to the rate of acceleration and not to velocity directly. Acceleration inc...
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| Veröffentlicht in: | The cryosphere Jg. 18; H. 2; S. 705 - 710 |
|---|---|
| Hauptverfasser: | , , |
| Format: | Journal Article |
| Sprache: | Englisch |
| Veröffentlicht: |
Katlenburg-Lindau
Copernicus GmbH
13.02.2024
Copernicus Publications |
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| ISSN: | 1994-0424, 1994-0416, 1994-0424, 1994-0416 |
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| Abstract | The Brunt Ice Shelf, Antarctica, accelerated rapidly from a velocity of 900 to 1500 m a−1 during 6 months, following calving of a 1500 km2 iceberg on 22 January 2023. The immediate response to calving was observed as a change to the rate of acceleration and not to velocity directly. Acceleration increased by a factor of 10, with a second, smaller calving at the end of June 2023, leading to further tripling of acceleration. The acceleration was caused by the reduction of buttressing at the McDonald Ice Rumples, leading to high localised strain rates, which reduce the strength of the remaining ice shelf. |
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| AbstractList | The Brunt Ice Shelf, Antarctica, accelerated rapidly from a velocity of 900 to 1500 m a −1 during 6 months, following calving of a 1500 km 2 iceberg on 22 January 2023. The immediate response to calving was observed as a change to the rate of acceleration and not to velocity directly. Acceleration increased by a factor of 10, with a second, smaller calving at the end of June 2023, leading to further tripling of acceleration. The acceleration was caused by the reduction of buttressing at the McDonald Ice Rumples, leading to high localised strain rates, which reduce the strength of the remaining ice shelf. The Brunt Ice Shelf, Antarctica, accelerated rapidly from a velocity of 900 to 1500 m a-1 during 6 months, following calving of a 1500 km2 iceberg on 22 January 2023. The immediate response to calving was observed as a change to the rate of acceleration and not to velocity directly. Acceleration increased by a factor of 10, with a second, smaller calving at the end of June 2023, leading to further tripling of acceleration. The acceleration was caused by the reduction of buttressing at the McDonald Ice Rumples, leading to high localised strain rates, which reduce the strength of the remaining ice shelf. The Brunt Ice Shelf, Antarctica, accelerated rapidly from a velocity of 900 to 1500 m a.sup.-1 during 6 months, following calving of a 1500 km.sup.2 iceberg on 22 January 2023. The immediate response to calving was observed as a change to the rate of acceleration and not to velocity directly. Acceleration increased by a factor of 10, with a second, smaller calving at the end of June 2023, leading to further tripling of acceleration. The acceleration was caused by the reduction of buttressing at the McDonald Ice Rumples, leading to high localised strain rates, which reduce the strength of the remaining ice shelf. The Brunt Ice Shelf, Antarctica, accelerated rapidly from a velocity of 900 to 1500 m a−1 during 6 months, following calving of a 1500 km2 iceberg on 22 January 2023. The immediate response to calving was observed as a change to the rate of acceleration and not to velocity directly. Acceleration increased by a factor of 10, with a second, smaller calving at the end of June 2023, leading to further tripling of acceleration. The acceleration was caused by the reduction of buttressing at the McDonald Ice Rumples, leading to high localised strain rates, which reduce the strength of the remaining ice shelf. |
| Audience | Academic |
| Author | Luckman, Adrian J. Hodgson, Dominic A. Marsh, Oliver J. |
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| Cites_doi | 10.5194/tc-14-2115-2020 10.1029/2023GL102880 10.5194/tc-15-663-2021 10.1029/2001GL014606 10.1029/2021JD036424 10.1126/sciadv.abg3080 10.5194/tc-13-2771-2019 10.5194/tc-16-2545-2022 10.5194/tc-12-505-2018 10.5194/tc-12-3361-2018 10.5194/tc-2023-63-supplement 10.1038/nclimate2912 10.1038/nature05430 10.5194/tc-13-545-2019 10.1017/jog.2016.132 10.1038/ncomms9566 10.5194/tc-2023-88-supplement 10.5194/tc-16-397-2022 10.5194/tc-17-157-2023 10.5194/tc-14-17-2020 |
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| Snippet | The Brunt Ice Shelf, Antarctica, accelerated rapidly from a velocity of 900 to 1500 m a−1 during 6 months, following calving of a 1500 km2 iceberg on... The Brunt Ice Shelf, Antarctica, accelerated rapidly from a velocity of 900 to 1500 m a.sup.-1 during 6 months, following calving of a 1500 km.sup.2 iceberg on... The Brunt Ice Shelf, Antarctica, accelerated rapidly from a velocity of 900 to 1500 m a-1 during 6 months, following calving of a 1500 km2 iceberg on 22... The Brunt Ice Shelf, Antarctica, accelerated rapidly from a velocity of 900 to 1500 m a −1 during 6 months, following calving of a 1500 km 2 iceberg on... |
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| SubjectTerms | Acceleration Buttresses Communication Ice calving Ice shelves Icebergs Land ice Research centers Software Velocity |
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| Title | Brief communication: Rapid acceleration of the Brunt Ice Shelf after calving of iceberg A-81 |
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