The 2020 Larsen C Ice Shelf surface melt is a 40-year record high

Along with record-breaking summer air temperatures at an Antarctic Peninsula meteorological station in February 2020, the Larsen C ice shelf experienced an exceptionally long and extensive 2019/2020 melt season. We use a 40-year time series of passive and scatterometer satellite microwave data, whic...

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Published in:The Cryosphere
Main Authors: S. Bevan, A. Luckman, H. Hendon, G. Wang
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2020
Subjects:
Online Access:https://doi.org/10.5194/tc-14-3551-2020
https://doaj.org/article/782a657c588743ba95b6c1051f85a62d
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spelling ftdoajarticles:oai:doaj.org/article:782a657c588743ba95b6c1051f85a62d 2023-05-15T13:47:52+02:00 The 2020 Larsen C Ice Shelf surface melt is a 40-year record high S. Bevan A. Luckman H. Hendon G. Wang 2020-10-01T00:00:00Z https://doi.org/10.5194/tc-14-3551-2020 https://doaj.org/article/782a657c588743ba95b6c1051f85a62d EN eng Copernicus Publications https://tc.copernicus.org/articles/14/3551/2020/tc-14-3551-2020.pdf https://doaj.org/toc/1994-0416 https://doaj.org/toc/1994-0424 doi:10.5194/tc-14-3551-2020 1994-0416 1994-0424 https://doaj.org/article/782a657c588743ba95b6c1051f85a62d The Cryosphere, Vol 14, Pp 3551-3564 (2020) Environmental sciences GE1-350 Geology QE1-996.5 article 2020 ftdoajarticles https://doi.org/10.5194/tc-14-3551-2020 2022-12-31T12:07:03Z Along with record-breaking summer air temperatures at an Antarctic Peninsula meteorological station in February 2020, the Larsen C ice shelf experienced an exceptionally long and extensive 2019/2020 melt season. We use a 40-year time series of passive and scatterometer satellite microwave data, which are sensitive to the presence of liquid water in the snow pack, to reveal that the extent and duration of melt observed on the ice shelf in the austral summer of 2019/2020 was the greatest on record. We find that unusual perturbations to Southern Hemisphere modes of atmospheric flow, including a persistently positive Indian Ocean Dipole in the spring and a very rare Southern Hemisphere sudden stratospheric warming in September 2019, preceded the exceptionally warm Antarctic Peninsula summer. It is likely that teleconnections between the tropics and southern high latitudes were able to bring sufficient heat via the atmosphere and ocean to the Antarctic Peninsula to drive the extreme Larsen C Ice Shelf melt. The record-breaking melt of 2019/2020 brought to an end the trend of decreasing melt that had begun in 1999/2000, will reinitiate earlier thinning of the ice shelf by depletion of the firn air content, and probably affected a much greater region than Larsen C Ice Shelf. Article in Journal/Newspaper Antarc* Antarctic Antarctic Peninsula Ice Shelf The Cryosphere Directory of Open Access Journals: DOAJ Articles Antarctic The Antarctic Antarctic Peninsula Austral Indian The Cryosphere 14 10 3551 3564
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
S. Bevan
A. Luckman
H. Hendon
G. Wang
The 2020 Larsen C Ice Shelf surface melt is a 40-year record high
topic_facet Environmental sciences
GE1-350
Geology
QE1-996.5
description Along with record-breaking summer air temperatures at an Antarctic Peninsula meteorological station in February 2020, the Larsen C ice shelf experienced an exceptionally long and extensive 2019/2020 melt season. We use a 40-year time series of passive and scatterometer satellite microwave data, which are sensitive to the presence of liquid water in the snow pack, to reveal that the extent and duration of melt observed on the ice shelf in the austral summer of 2019/2020 was the greatest on record. We find that unusual perturbations to Southern Hemisphere modes of atmospheric flow, including a persistently positive Indian Ocean Dipole in the spring and a very rare Southern Hemisphere sudden stratospheric warming in September 2019, preceded the exceptionally warm Antarctic Peninsula summer. It is likely that teleconnections between the tropics and southern high latitudes were able to bring sufficient heat via the atmosphere and ocean to the Antarctic Peninsula to drive the extreme Larsen C Ice Shelf melt. The record-breaking melt of 2019/2020 brought to an end the trend of decreasing melt that had begun in 1999/2000, will reinitiate earlier thinning of the ice shelf by depletion of the firn air content, and probably affected a much greater region than Larsen C Ice Shelf.
format Article in Journal/Newspaper
author S. Bevan
A. Luckman
H. Hendon
G. Wang
author_facet S. Bevan
A. Luckman
H. Hendon
G. Wang
author_sort S. Bevan
title The 2020 Larsen C Ice Shelf surface melt is a 40-year record high
title_short The 2020 Larsen C Ice Shelf surface melt is a 40-year record high
title_full The 2020 Larsen C Ice Shelf surface melt is a 40-year record high
title_fullStr The 2020 Larsen C Ice Shelf surface melt is a 40-year record high
title_full_unstemmed The 2020 Larsen C Ice Shelf surface melt is a 40-year record high
title_sort 2020 larsen c ice shelf surface melt is a 40-year record high
publisher Copernicus Publications
publishDate 2020
url https://doi.org/10.5194/tc-14-3551-2020
https://doaj.org/article/782a657c588743ba95b6c1051f85a62d
geographic Antarctic
The Antarctic
Antarctic Peninsula
Austral
Indian
geographic_facet Antarctic
The Antarctic
Antarctic Peninsula
Austral
Indian
genre Antarc*
Antarctic
Antarctic Peninsula
Ice Shelf
The Cryosphere
genre_facet Antarc*
Antarctic
Antarctic Peninsula
Ice Shelf
The Cryosphere
op_source The Cryosphere, Vol 14, Pp 3551-3564 (2020)
op_relation https://tc.copernicus.org/articles/14/3551/2020/tc-14-3551-2020.pdf
https://doaj.org/toc/1994-0416
https://doaj.org/toc/1994-0424
doi:10.5194/tc-14-3551-2020
1994-0416
1994-0424
https://doaj.org/article/782a657c588743ba95b6c1051f85a62d
op_doi https://doi.org/10.5194/tc-14-3551-2020
container_title The Cryosphere
container_volume 14
container_issue 10
container_start_page 3551
op_container_end_page 3564
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