Oscillatory response of Larsen C Ice Shelf flow to the calving of iceberg A-68 ...

Abstract The collapse of several ice shelves in the Antarctic Peninsula since the late 20th century has resulted in the upstream acceleration of multiple formerly buttressed outlet glaciers, raising questions about the stability of Antarctica's remaining ice shelves and the effects their demise...

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Main Authors: Deakin, KA, Christie, FDW, Boxall, K, Willis, IC
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2024
Subjects:
Online Access:https://dx.doi.org/10.17863/cam.104518
https://www.repository.cam.ac.uk/handle/1810/362155
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author Deakin, KA
Christie, FDW
Boxall, K
Willis, IC
author_facet Deakin, KA
Christie, FDW
Boxall, K
Willis, IC
author_sort Deakin, KA
collection DataCite
description Abstract The collapse of several ice shelves in the Antarctic Peninsula since the late 20th century has resulted in the upstream acceleration of multiple formerly buttressed outlet glaciers, raising questions about the stability of Antarctica's remaining ice shelves and the effects their demise may have upon inland ice. Here, we use high temporal resolution Sentinel-1A/B synthetic aperture radar-derived observations to assess the velocity response of Larsen C Ice Shelf (LCIS) to the calving of colossal iceberg A-68 in 2017. We find marked oscillations in ice-shelf flow across LCIS in the months following A-68's calving, beginning with a near-ice-shelf-wide slowdown of 11.3 m yr−1 on average. While falling close to the limits of detectability, these ice-flow variations appear to have been presaged by similar oscillations in the years prior to A-68's breakaway, associated primarily with major rifting events, together reflecting potentially hitherto unobserved ice-shelf mechanical processes with important ...
format Article in Journal/Newspaper
genre Antarc*
Antarctic
Antarctic Peninsula
Ice Shelf
Ice Shelves
Iceberg*
genre_facet Antarc*
Antarctic
Antarctic Peninsula
Ice Shelf
Ice Shelves
Iceberg*
geographic Antarctic
Antarctic Peninsula
The Antarctic
geographic_facet Antarctic
Antarctic Peninsula
The Antarctic
id ftdatacite:10.17863/cam.104518
institution Open Polar
language English
op_collection_id ftdatacite
op_doi https://doi.org/10.17863/cam.10451810.17863/cam.101851
op_relation https://dx.doi.org/10.17863/cam.101851
op_rights open.access
Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
http://purl.org/coar/access_right/c_abf2
publishDate 2024
publisher Cambridge University Press (CUP)
record_format openpolar
spelling ftdatacite:10.17863/cam.104518 2025-04-20T14:26:43+00:00 Oscillatory response of Larsen C Ice Shelf flow to the calving of iceberg A-68 ... Deakin, KA Christie, FDW Boxall, K Willis, IC 2024 https://dx.doi.org/10.17863/cam.104518 https://www.repository.cam.ac.uk/handle/1810/362155 en eng Cambridge University Press (CUP) https://dx.doi.org/10.17863/cam.101851 open.access Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 http://purl.org/coar/access_right/c_abf2 37 Earth Sciences 3709 Physical Geography and Environmental Geoscience ScholarlyArticle article-journal JournalArticle Article 2024 ftdatacite https://doi.org/10.17863/cam.10451810.17863/cam.101851 2025-04-02T15:01:50Z Abstract The collapse of several ice shelves in the Antarctic Peninsula since the late 20th century has resulted in the upstream acceleration of multiple formerly buttressed outlet glaciers, raising questions about the stability of Antarctica's remaining ice shelves and the effects their demise may have upon inland ice. Here, we use high temporal resolution Sentinel-1A/B synthetic aperture radar-derived observations to assess the velocity response of Larsen C Ice Shelf (LCIS) to the calving of colossal iceberg A-68 in 2017. We find marked oscillations in ice-shelf flow across LCIS in the months following A-68's calving, beginning with a near-ice-shelf-wide slowdown of 11.3 m yr−1 on average. While falling close to the limits of detectability, these ice-flow variations appear to have been presaged by similar oscillations in the years prior to A-68's breakaway, associated primarily with major rifting events, together reflecting potentially hitherto unobserved ice-shelf mechanical processes with important ... Article in Journal/Newspaper Antarc* Antarctic Antarctic Peninsula Ice Shelf Ice Shelves Iceberg* DataCite Antarctic Antarctic Peninsula The Antarctic
spellingShingle 37 Earth Sciences
3709 Physical Geography and Environmental Geoscience
Deakin, KA
Christie, FDW
Boxall, K
Willis, IC
Oscillatory response of Larsen C Ice Shelf flow to the calving of iceberg A-68 ...
title Oscillatory response of Larsen C Ice Shelf flow to the calving of iceberg A-68 ...
title_full Oscillatory response of Larsen C Ice Shelf flow to the calving of iceberg A-68 ...
title_fullStr Oscillatory response of Larsen C Ice Shelf flow to the calving of iceberg A-68 ...
title_full_unstemmed Oscillatory response of Larsen C Ice Shelf flow to the calving of iceberg A-68 ...
title_short Oscillatory response of Larsen C Ice Shelf flow to the calving of iceberg A-68 ...
title_sort oscillatory response of larsen c ice shelf flow to the calving of iceberg a-68 ...
topic 37 Earth Sciences
3709 Physical Geography and Environmental Geoscience
topic_facet 37 Earth Sciences
3709 Physical Geography and Environmental Geoscience
url https://dx.doi.org/10.17863/cam.104518
https://www.repository.cam.ac.uk/handle/1810/362155