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...
Main Authors: | , , , |
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Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Cambridge University Press (CUP)
2024
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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 |