Delayed Antarctic sea-ice decline in high-resolution climate change simulations

Delayed Antarctic sea-ice decline is linked to Southern Ocean eddies - and their explicit treatment in models is crucial. New multi-resolution climate change projections give a possible reason for low confidence in IPCC’s current 21st-century Antarctic sea-ice projections.

Bibliographic Details
Published in:Nature Communications
Main Authors: Thomas Rackow, Sergey Danilov, Helge F. Goessling, Hartmut H. Hellmer, Dmitry V. Sein, Tido Semmler, Dmitry Sidorenko, Thomas Jung
Format: Article in Journal/Newspaper
Language:English
Published: Nature Portfolio 2022
Subjects:
Science
Q
Antarctic
Southern Ocean
Antarc*
Sea ice
Online Access:https://doi.org/10.1038/s41467-022-28259-y
https://doaj.org/article/d93ba30d8e5a40cebd842cc3b8eeb9ca
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spelling ftdoajarticles:oai:doaj.org/article:d93ba30d8e5a40cebd842cc3b8eeb9ca 2023-05-15T13:49:11+02:00 Delayed Antarctic sea-ice decline in high-resolution climate change simulations Thomas Rackow Sergey Danilov Helge F. Goessling Hartmut H. Hellmer Dmitry V. Sein Tido Semmler Dmitry Sidorenko Thomas Jung 2022-02-01T00:00:00Z https://doi.org/10.1038/s41467-022-28259-y https://doaj.org/article/d93ba30d8e5a40cebd842cc3b8eeb9ca EN eng Nature Portfolio https://doi.org/10.1038/s41467-022-28259-y https://doaj.org/toc/2041-1723 doi:10.1038/s41467-022-28259-y 2041-1723 https://doaj.org/article/d93ba30d8e5a40cebd842cc3b8eeb9ca Nature Communications, Vol 13, Iss 1, Pp 1-12 (2022) Science Q article 2022 ftdoajarticles https://doi.org/10.1038/s41467-022-28259-y 2022-12-31T00:54:42Z Delayed Antarctic sea-ice decline is linked to Southern Ocean eddies - and their explicit treatment in models is crucial. New multi-resolution climate change projections give a possible reason for low confidence in IPCC’s current 21st-century Antarctic sea-ice projections. Article in Journal/Newspaper Antarc* Antarctic Sea ice Southern Ocean Directory of Open Access Journals: DOAJ Articles Antarctic Southern Ocean Nature Communications 13 1
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Science
Q
spellingShingle Science
Q
Thomas Rackow
Sergey Danilov
Helge F. Goessling
Hartmut H. Hellmer
Dmitry V. Sein
Tido Semmler
Dmitry Sidorenko
Thomas Jung
Delayed Antarctic sea-ice decline in high-resolution climate change simulations
topic_facet Science
Q
description Delayed Antarctic sea-ice decline is linked to Southern Ocean eddies - and their explicit treatment in models is crucial. New multi-resolution climate change projections give a possible reason for low confidence in IPCC’s current 21st-century Antarctic sea-ice projections.
format Article in Journal/Newspaper
author Thomas Rackow
Sergey Danilov
Helge F. Goessling
Hartmut H. Hellmer
Dmitry V. Sein
Tido Semmler
Dmitry Sidorenko
Thomas Jung
author_facet Thomas Rackow
Sergey Danilov
Helge F. Goessling
Hartmut H. Hellmer
Dmitry V. Sein
Tido Semmler
Dmitry Sidorenko
Thomas Jung
author_sort Thomas Rackow
title Delayed Antarctic sea-ice decline in high-resolution climate change simulations
title_short Delayed Antarctic sea-ice decline in high-resolution climate change simulations
title_full Delayed Antarctic sea-ice decline in high-resolution climate change simulations
title_fullStr Delayed Antarctic sea-ice decline in high-resolution climate change simulations
title_full_unstemmed Delayed Antarctic sea-ice decline in high-resolution climate change simulations
title_sort delayed antarctic sea-ice decline in high-resolution climate change simulations
publisher Nature Portfolio
publishDate 2022
url https://doi.org/10.1038/s41467-022-28259-y
https://doaj.org/article/d93ba30d8e5a40cebd842cc3b8eeb9ca
geographic Antarctic
Southern Ocean
geographic_facet Antarctic
Southern Ocean
genre Antarc*
Antarctic
Sea ice
Southern Ocean
genre_facet Antarc*
Antarctic
Sea ice
Southern Ocean
op_source Nature Communications, Vol 13, Iss 1, Pp 1-12 (2022)
op_relation https://doi.org/10.1038/s41467-022-28259-y
https://doaj.org/toc/2041-1723
doi:10.1038/s41467-022-28259-y
2041-1723
https://doaj.org/article/d93ba30d8e5a40cebd842cc3b8eeb9ca
op_doi https://doi.org/10.1038/s41467-022-28259-y
container_title Nature Communications
container_volume 13
container_issue 1
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