Antarctic sea ice #3: trends and future projections

Since reliable and continuous satellite records began in 1979, there have been strong regionally- and seasonally-varying patterns of change and variability in sea-ice extent around Antarctica (Fig. 1) in contrast to a largely uniform loss of sea ice across the Arctic. Notably, the region west of the...

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Main Authors: Clem, K, Massom, R, Stammerjohn, S, Reid, P
Format: Text
Language:English
Published: SCAR 2022
Subjects:
Online Access:https://doi.org/10.48361/4d9d-1g64
http://ecite.utas.edu.au/154022
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author Clem, K
Massom, R
Stammerjohn, S
Reid, P
author_facet Clem, K
Massom, R
Stammerjohn, S
Reid, P
author_sort Clem, K
collection Unknown
description Since reliable and continuous satellite records began in 1979, there have been strong regionally- and seasonally-varying patterns of change and variability in sea-ice extent around Antarctica (Fig. 1) in contrast to a largely uniform loss of sea ice across the Arctic. Notably, the region west of the Antarctic Peninsula to the eastern Ross Sea has experienced significant sea ice loss in concert with a strengthening of the Amundsen Sea Low and increased warm northerly winds. On the western Peninsula, the sea ice loss and associated regional warming has led to dramatic and complex ecosystem change (see Antarctic Sea Ice #2 ) and has also been implicated in major ice-shelf disintegration events on the Peninsula (see Antarctic Sea Ice #1 ). Elsewhere, sea-ice coverage has expanded but with substantial interannual variability. The sum of these differing regional and seasonal contributions is a slight increasing trend in overall sea-ice coverage of 1.0 0.5% per decade (or about 11,300km 2 per year) for 19792018 (Fig. 1a).
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genre Amundsen Sea
Antarc*
Antarctic
Antarctic Peninsula
Antarctica
Arctic
Ice Shelf
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Sea ice
genre_facet Amundsen Sea
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Antarctic
Antarctic Peninsula
Antarctica
Arctic
Ice Shelf
Ross Sea
Sea ice
geographic Arctic
Antarctic
The Antarctic
Antarctic Peninsula
Ross Sea
Amundsen Sea
geographic_facet Arctic
Antarctic
The Antarctic
Antarctic Peninsula
Ross Sea
Amundsen Sea
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institution Open Polar
language English
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op_doi https://doi.org/10.48361/4d9d-1g64
op_relation http://ecite.utas.edu.au/154022/1/154022 - Antarctic sea ice 3 - trends and future projections.pdf
http://dx.doi.org/10.48361/4d9d-1g64
Clem, K and Massom, R and Stammerjohn, S and Reid, P, Antarctic sea ice #3: trends and future projections, Antarctic Environments Portal, 02 August pp. 1-12. (2022) [Professional, Refereed Article]
http://ecite.utas.edu.au/154022
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spelling ftunivtasecite:oai:ecite.utas.edu.au:154022 2025-01-16T18:54:22+00:00 Antarctic sea ice #3: trends and future projections Clem, K Massom, R Stammerjohn, S Reid, P 2022 application/pdf https://doi.org/10.48361/4d9d-1g64 http://ecite.utas.edu.au/154022 en eng SCAR http://ecite.utas.edu.au/154022/1/154022 - Antarctic sea ice 3 - trends and future projections.pdf http://dx.doi.org/10.48361/4d9d-1g64 Clem, K and Massom, R and Stammerjohn, S and Reid, P, Antarctic sea ice #3: trends and future projections, Antarctic Environments Portal, 02 August pp. 1-12. (2022) [Professional, Refereed Article] http://ecite.utas.edu.au/154022 Environmental Sciences Other environmental sciences Other environmental sciences not elsewhere classified Professional, Refereed Article PeerReviewed 2022 ftunivtasecite https://doi.org/10.48361/4d9d-1g64 2022-10-24T22:16:50Z Since reliable and continuous satellite records began in 1979, there have been strong regionally- and seasonally-varying patterns of change and variability in sea-ice extent around Antarctica (Fig. 1) in contrast to a largely uniform loss of sea ice across the Arctic. Notably, the region west of the Antarctic Peninsula to the eastern Ross Sea has experienced significant sea ice loss in concert with a strengthening of the Amundsen Sea Low and increased warm northerly winds. On the western Peninsula, the sea ice loss and associated regional warming has led to dramatic and complex ecosystem change (see Antarctic Sea Ice #2 ) and has also been implicated in major ice-shelf disintegration events on the Peninsula (see Antarctic Sea Ice #1 ). Elsewhere, sea-ice coverage has expanded but with substantial interannual variability. The sum of these differing regional and seasonal contributions is a slight increasing trend in overall sea-ice coverage of 1.0 0.5% per decade (or about 11,300km 2 per year) for 19792018 (Fig. 1a). Text Amundsen Sea Antarc* Antarctic Antarctic Peninsula Antarctica Arctic Ice Shelf Ross Sea Sea ice Unknown Arctic Antarctic The Antarctic Antarctic Peninsula Ross Sea Amundsen Sea
spellingShingle Environmental Sciences
Other environmental sciences
Other environmental sciences not elsewhere classified
Clem, K
Massom, R
Stammerjohn, S
Reid, P
Antarctic sea ice #3: trends and future projections
title Antarctic sea ice #3: trends and future projections
title_full Antarctic sea ice #3: trends and future projections
title_fullStr Antarctic sea ice #3: trends and future projections
title_full_unstemmed Antarctic sea ice #3: trends and future projections
title_short Antarctic sea ice #3: trends and future projections
title_sort antarctic sea ice #3: trends and future projections
topic Environmental Sciences
Other environmental sciences
Other environmental sciences not elsewhere classified
topic_facet Environmental Sciences
Other environmental sciences
Other environmental sciences not elsewhere classified
url https://doi.org/10.48361/4d9d-1g64
http://ecite.utas.edu.au/154022