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Glacier surge as a trigger for the fastest delta growth in the Arctic

J. Kavan Orcid Logo, M. C. Strzelecki Orcid Logo, D. I. Benn, Adrian Luckman Orcid Logo, M. Roman, P. Zagórski

Communications Earth & Environment, Volume: 5, Issue: 1

Swansea University Author: Adrian Luckman Orcid Logo

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Abstract

The widespread retreat of Svalbard glaciers has been frequently interrupted by short-lived surge advances. In the case of marine-terminating glaciers this is often expressed in the remodelling of coastal zones. Here, we analyzed the coastal zone changes in front of the recently surging Recherchebree...

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Published in: Communications Earth & Environment
ISSN: 2662-4435
Published: Springer Science and Business Media LLC 2024
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URI: https://cronfa.swan.ac.uk/Record/cronfa68277
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spelling 2025-01-15T12:52:41.0857834 v2 68277 2024-11-14 Glacier surge as a trigger for the fastest delta growth in the Arctic 008cb668b2671b653a88677f075799a9 0000-0002-9618-5905 Adrian Luckman Adrian Luckman true false 2024-11-14 BGPS The widespread retreat of Svalbard glaciers has been frequently interrupted by short-lived surge advances. In the case of marine-terminating glaciers this is often expressed in the remodelling of coastal zones. Here, we analyzed the coastal zone changes in front of the recently surging Recherchebreen. The glacier advanced ca 1200 m since 2018 and suddenly stopped in June 2020 followed by the rapid formation of a delta system in front of its subglacial meltwater outlet. The delta advanced by ca 450 m with probably the fastest progradation rate ever detected in the Arctic region (ca 7 m/day). The synchroneity of the final slow-down of the glacier with the delta building indicates that this event records the release of stored water and sediments from beneath the glacier and thus provides direct evidence of drainage reorganisation at the termination of a surge. Such behaviour is likely common among Svalbard surging glaciers, but it only rarely leaves any direct geomorphic evidence. Journal Article Communications Earth &amp; Environment 5 1 Springer Science and Business Media LLC 2662-4435 14 11 2024 2024-11-14 10.1038/s43247-024-01877-8 COLLEGE NANME Biosciences Geography and Physics School COLLEGE CODE BGPS Swansea University Another institution paid the OA fee The research leading to these results has received funding from the Norwegian Financial Mechanism 2014-2021: SVELTA—Svalbard Delta Systems Under Warming Climate (UMO-2020/37/K/ST10/02852) based at the University of Wroclaw. JK wrote the manuscript at Alfred Jahn Cold Regions Research Centre, University of Wroclaw during the SVELTA project. MR was supported by a Czech Science Foundation (GACR) grant 22-206210. M.C.S. work on paraglacial coast is funded by GLAVE project (NCN -UMO-2020/38/E/ST10/00042). 2025-01-15T12:52:41.0857834 2024-11-14T16:33:21.1835764 Faculty of Science and Engineering School of Biosciences, Geography and Physics - Geography J. Kavan 0000-0003-4524-3009 1 M. C. Strzelecki 0000-0003-0479-3565 2 D. I. Benn 3 Adrian Luckman 0000-0002-9618-5905 4 M. Roman 5 P. Zagórski 6 68277__33336__1810ec05a5ad4a8aa22af3f0f4cf81f4.pdf 68277.VoR.pdf 2025-01-15T12:50:37.5053336 Output 9172539 application/pdf Version of Record true © The Author(s) 2024. This article is licensed under a Creative Commons Attribution 4.0 International License. true eng http://creativecommons.org/licenses/by/4.0/
title Glacier surge as a trigger for the fastest delta growth in the Arctic
spellingShingle Glacier surge as a trigger for the fastest delta growth in the Arctic
Adrian Luckman
title_short Glacier surge as a trigger for the fastest delta growth in the Arctic
title_full Glacier surge as a trigger for the fastest delta growth in the Arctic
title_fullStr Glacier surge as a trigger for the fastest delta growth in the Arctic
title_full_unstemmed Glacier surge as a trigger for the fastest delta growth in the Arctic
title_sort Glacier surge as a trigger for the fastest delta growth in the Arctic
author_id_str_mv 008cb668b2671b653a88677f075799a9
author_id_fullname_str_mv 008cb668b2671b653a88677f075799a9_***_Adrian Luckman
author Adrian Luckman
author2 J. Kavan
M. C. Strzelecki
D. I. Benn
Adrian Luckman
M. Roman
P. Zagórski
format Journal article
container_title Communications Earth &amp; Environment
container_volume 5
container_issue 1
publishDate 2024
institution Swansea University
issn 2662-4435
doi_str_mv 10.1038/s43247-024-01877-8
publisher Springer Science and Business Media LLC
college_str Faculty of Science and Engineering
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hierarchy_top_id facultyofscienceandengineering
hierarchy_top_title Faculty of Science and Engineering
hierarchy_parent_id facultyofscienceandengineering
hierarchy_parent_title Faculty of Science and Engineering
department_str School of Biosciences, Geography and Physics - Geography{{{_:::_}}}Faculty of Science and Engineering{{{_:::_}}}School of Biosciences, Geography and Physics - Geography
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description The widespread retreat of Svalbard glaciers has been frequently interrupted by short-lived surge advances. In the case of marine-terminating glaciers this is often expressed in the remodelling of coastal zones. Here, we analyzed the coastal zone changes in front of the recently surging Recherchebreen. The glacier advanced ca 1200 m since 2018 and suddenly stopped in June 2020 followed by the rapid formation of a delta system in front of its subglacial meltwater outlet. The delta advanced by ca 450 m with probably the fastest progradation rate ever detected in the Arctic region (ca 7 m/day). The synchroneity of the final slow-down of the glacier with the delta building indicates that this event records the release of stored water and sediments from beneath the glacier and thus provides direct evidence of drainage reorganisation at the termination of a surge. Such behaviour is likely common among Svalbard surging glaciers, but it only rarely leaves any direct geomorphic evidence.
published_date 2024-11-14T03:07:25Z
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