Triggers of the 2022 Larsen B multi-year landfast sea ice breakout and initial glacier response

In late March 2011, landfast sea ice (hereafter, “fast ice”) formed in the northern Larsen B embayment and persisted continuously as multi-year fast ice until January 2022. In the 11 years of fast-ice presence, the northern Larsen B glaciers slowed significantly, thickened in their lower reaches, an...

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Published in:The Cryosphere
Main Authors: N. E. Ochwat, T. A. Scambos, A. F. Banwell, R. S. Anderson, M. L. Maclennan, G. Picard, J. A. Shates, S. Marinsek, L. Margonari, M. Truffer, E. C. Pettit
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2024
Subjects:
Online Access:https://doi.org/10.5194/tc-18-1709-2024
https://doaj.org/article/dbba9d391c7840f1b1fc0cca23ec7d9b
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spelling ftdoajarticles:oai:doaj.org/article:dbba9d391c7840f1b1fc0cca23ec7d9b 2024-09-15T18:12:39+00:00 Triggers of the 2022 Larsen B multi-year landfast sea ice breakout and initial glacier response N. E. Ochwat T. A. Scambos A. F. Banwell R. S. Anderson M. L. Maclennan G. Picard J. A. Shates S. Marinsek L. Margonari M. Truffer E. C. Pettit 2024-04-01T00:00:00Z https://doi.org/10.5194/tc-18-1709-2024 https://doaj.org/article/dbba9d391c7840f1b1fc0cca23ec7d9b EN eng Copernicus Publications https://tc.copernicus.org/articles/18/1709/2024/tc-18-1709-2024.pdf https://doaj.org/toc/1994-0416 https://doaj.org/toc/1994-0424 doi:10.5194/tc-18-1709-2024 1994-0416 1994-0424 https://doaj.org/article/dbba9d391c7840f1b1fc0cca23ec7d9b The Cryosphere, Vol 18, Pp 1709-1731 (2024) Environmental sciences GE1-350 Geology QE1-996.5 article 2024 ftdoajarticles https://doi.org/10.5194/tc-18-1709-2024 2024-08-05T17:49:38Z In late March 2011, landfast sea ice (hereafter, “fast ice”) formed in the northern Larsen B embayment and persisted continuously as multi-year fast ice until January 2022. In the 11 years of fast-ice presence, the northern Larsen B glaciers slowed significantly, thickened in their lower reaches, and developed extensive mélange areas, leading to the formation of ice tongues that extended up to 16 km from the 2011 ice fronts. In situ measurements of ice speed on adjacent ice shelf areas spanning 2011 to 2017 show that the fast ice provided significant resistive stress to ice flow. Fast-ice breakout began in late January 2022 and was closely followed by retreat and breakup of both the fast-ice mélange and the glacier ice tongues. We investigate the probable triggers for the loss of fast ice and document the initial upstream glacier responses. The fast-ice breakup is linked to the arrival of a strong ocean swell event ( >1.5 m amplitude; wave period waves >5 s) originating from the northeast. Wave propagation to the ice front was facilitated by a 12-year low in sea ice concentration in the northwestern Weddell Sea, creating a near-ice-free corridor to the open ocean. Remote sensing data in the months following the fast-ice breakout reveals an initial ice flow speed increase ( >2 -fold), elevation loss (9 to 11 m), and rapid calving of floating and grounded ice for the three main embayment glaciers Crane (11 km), Hektoria (25 km), and Green (18 km). Article in Journal/Newspaper Ice Shelf Sea ice The Cryosphere Weddell Sea Directory of Open Access Journals: DOAJ Articles The Cryosphere 18 4 1709 1731
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Environmental sciences
GE1-350
Geology
QE1-996.5
spellingShingle Environmental sciences
GE1-350
Geology
QE1-996.5
N. E. Ochwat
T. A. Scambos
A. F. Banwell
R. S. Anderson
M. L. Maclennan
G. Picard
J. A. Shates
S. Marinsek
L. Margonari
M. Truffer
E. C. Pettit
Triggers of the 2022 Larsen B multi-year landfast sea ice breakout and initial glacier response
topic_facet Environmental sciences
GE1-350
Geology
QE1-996.5
description In late March 2011, landfast sea ice (hereafter, “fast ice”) formed in the northern Larsen B embayment and persisted continuously as multi-year fast ice until January 2022. In the 11 years of fast-ice presence, the northern Larsen B glaciers slowed significantly, thickened in their lower reaches, and developed extensive mélange areas, leading to the formation of ice tongues that extended up to 16 km from the 2011 ice fronts. In situ measurements of ice speed on adjacent ice shelf areas spanning 2011 to 2017 show that the fast ice provided significant resistive stress to ice flow. Fast-ice breakout began in late January 2022 and was closely followed by retreat and breakup of both the fast-ice mélange and the glacier ice tongues. We investigate the probable triggers for the loss of fast ice and document the initial upstream glacier responses. The fast-ice breakup is linked to the arrival of a strong ocean swell event ( >1.5 m amplitude; wave period waves >5 s) originating from the northeast. Wave propagation to the ice front was facilitated by a 12-year low in sea ice concentration in the northwestern Weddell Sea, creating a near-ice-free corridor to the open ocean. Remote sensing data in the months following the fast-ice breakout reveals an initial ice flow speed increase ( >2 -fold), elevation loss (9 to 11 m), and rapid calving of floating and grounded ice for the three main embayment glaciers Crane (11 km), Hektoria (25 km), and Green (18 km).
format Article in Journal/Newspaper
author N. E. Ochwat
T. A. Scambos
A. F. Banwell
R. S. Anderson
M. L. Maclennan
G. Picard
J. A. Shates
S. Marinsek
L. Margonari
M. Truffer
E. C. Pettit
author_facet N. E. Ochwat
T. A. Scambos
A. F. Banwell
R. S. Anderson
M. L. Maclennan
G. Picard
J. A. Shates
S. Marinsek
L. Margonari
M. Truffer
E. C. Pettit
author_sort N. E. Ochwat
title Triggers of the 2022 Larsen B multi-year landfast sea ice breakout and initial glacier response
title_short Triggers of the 2022 Larsen B multi-year landfast sea ice breakout and initial glacier response
title_full Triggers of the 2022 Larsen B multi-year landfast sea ice breakout and initial glacier response
title_fullStr Triggers of the 2022 Larsen B multi-year landfast sea ice breakout and initial glacier response
title_full_unstemmed Triggers of the 2022 Larsen B multi-year landfast sea ice breakout and initial glacier response
title_sort triggers of the 2022 larsen b multi-year landfast sea ice breakout and initial glacier response
publisher Copernicus Publications
publishDate 2024
url https://doi.org/10.5194/tc-18-1709-2024
https://doaj.org/article/dbba9d391c7840f1b1fc0cca23ec7d9b
genre Ice Shelf
Sea ice
The Cryosphere
Weddell Sea
genre_facet Ice Shelf
Sea ice
The Cryosphere
Weddell Sea
op_source The Cryosphere, Vol 18, Pp 1709-1731 (2024)
op_relation https://tc.copernicus.org/articles/18/1709/2024/tc-18-1709-2024.pdf
https://doaj.org/toc/1994-0416
https://doaj.org/toc/1994-0424
doi:10.5194/tc-18-1709-2024
1994-0416
1994-0424
https://doaj.org/article/dbba9d391c7840f1b1fc0cca23ec7d9b
op_doi https://doi.org/10.5194/tc-18-1709-2024
container_title The Cryosphere
container_volume 18
container_issue 4
container_start_page 1709
op_container_end_page 1731
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