A frequent ice-free Arctic is likely to occur before the mid-21st century

Abstract Although the trend of sea-ice extent under global warming has been studied extensively in recent years, most climate models have failed to capture the recent rapid change in the Arctic environment, which has brought into question the reliability of climate model projections of sea ice and s...

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Published in:npj Climate and Atmospheric Science
Main Authors: Zili Shen, Wen Zhou, Jinxiao Li, Johnny C. L. Chan
Format: Article in Journal/Newspaper
Language:English
Published: Nature Portfolio 2023
Subjects:
Online Access:https://doi.org/10.1038/s41612-023-00431-1
https://doaj.org/article/a51f0006c3f644de8f2fd66d59dd4fbf
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spelling ftdoajarticles:oai:doaj.org/article:a51f0006c3f644de8f2fd66d59dd4fbf 2023-08-27T04:07:00+02:00 A frequent ice-free Arctic is likely to occur before the mid-21st century Zili Shen Wen Zhou Jinxiao Li Johnny C. L. Chan 2023-07-01T00:00:00Z https://doi.org/10.1038/s41612-023-00431-1 https://doaj.org/article/a51f0006c3f644de8f2fd66d59dd4fbf EN eng Nature Portfolio https://doi.org/10.1038/s41612-023-00431-1 https://doaj.org/toc/2397-3722 doi:10.1038/s41612-023-00431-1 2397-3722 https://doaj.org/article/a51f0006c3f644de8f2fd66d59dd4fbf npj Climate and Atmospheric Science, Vol 6, Iss 1, Pp 1-7 (2023) Environmental sciences GE1-350 Meteorology. Climatology QC851-999 article 2023 ftdoajarticles https://doi.org/10.1038/s41612-023-00431-1 2023-08-06T00:49:20Z Abstract Although the trend of sea-ice extent under global warming has been studied extensively in recent years, most climate models have failed to capture the recent rapid change in the Arctic environment, which has brought into question the reliability of climate model projections of sea ice and suggested a potential shift in Arctic climate dynamics. Here, based on the results of a time-variant emergent constraint method with a weighting scheme, we show that an ice-free Arctic might occur earlier (by at least 5 ~ 10 years) than previously estimated. In other words, Arctic ice will likely disappear before the 2050 s. The observationally constrained date for an ice-free Arctic in September under fossil-fuel-based development (i.e., Shared Socioeconomic Pathway (SSP) 5–8.5) scenarios yields a central estimate of 2050–2054 with a 66% confidence range (equivalent to the IPCC’s ‘likely’ range) of 2037–2066, while an ice-free Arctic will likely occur for another 20 years and 11 years under ambitious mitigation scenarios (i.e., SSP2-4.5) and SSP3-7.0. An ice-free Arctic is unlikely to occur under the sustainable development scenario (i.e., SSP1-2.6). Looking forward, this time-variant emergent constraint may also help detect tipping points in the climate system. Our findings provide useful information to help policy makers cope with climate change. Article in Journal/Newspaper Arctic Climate change Global warming Sea ice Directory of Open Access Journals: DOAJ Articles Arctic npj Climate and Atmospheric Science 6 1
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
spellingShingle Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
Zili Shen
Wen Zhou
Jinxiao Li
Johnny C. L. Chan
A frequent ice-free Arctic is likely to occur before the mid-21st century
topic_facet Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
description Abstract Although the trend of sea-ice extent under global warming has been studied extensively in recent years, most climate models have failed to capture the recent rapid change in the Arctic environment, which has brought into question the reliability of climate model projections of sea ice and suggested a potential shift in Arctic climate dynamics. Here, based on the results of a time-variant emergent constraint method with a weighting scheme, we show that an ice-free Arctic might occur earlier (by at least 5 ~ 10 years) than previously estimated. In other words, Arctic ice will likely disappear before the 2050 s. The observationally constrained date for an ice-free Arctic in September under fossil-fuel-based development (i.e., Shared Socioeconomic Pathway (SSP) 5–8.5) scenarios yields a central estimate of 2050–2054 with a 66% confidence range (equivalent to the IPCC’s ‘likely’ range) of 2037–2066, while an ice-free Arctic will likely occur for another 20 years and 11 years under ambitious mitigation scenarios (i.e., SSP2-4.5) and SSP3-7.0. An ice-free Arctic is unlikely to occur under the sustainable development scenario (i.e., SSP1-2.6). Looking forward, this time-variant emergent constraint may also help detect tipping points in the climate system. Our findings provide useful information to help policy makers cope with climate change.
format Article in Journal/Newspaper
author Zili Shen
Wen Zhou
Jinxiao Li
Johnny C. L. Chan
author_facet Zili Shen
Wen Zhou
Jinxiao Li
Johnny C. L. Chan
author_sort Zili Shen
title A frequent ice-free Arctic is likely to occur before the mid-21st century
title_short A frequent ice-free Arctic is likely to occur before the mid-21st century
title_full A frequent ice-free Arctic is likely to occur before the mid-21st century
title_fullStr A frequent ice-free Arctic is likely to occur before the mid-21st century
title_full_unstemmed A frequent ice-free Arctic is likely to occur before the mid-21st century
title_sort frequent ice-free arctic is likely to occur before the mid-21st century
publisher Nature Portfolio
publishDate 2023
url https://doi.org/10.1038/s41612-023-00431-1
https://doaj.org/article/a51f0006c3f644de8f2fd66d59dd4fbf
geographic Arctic
geographic_facet Arctic
genre Arctic
Climate change
Global warming
Sea ice
genre_facet Arctic
Climate change
Global warming
Sea ice
op_source npj Climate and Atmospheric Science, Vol 6, Iss 1, Pp 1-7 (2023)
op_relation https://doi.org/10.1038/s41612-023-00431-1
https://doaj.org/toc/2397-3722
doi:10.1038/s41612-023-00431-1
2397-3722
https://doaj.org/article/a51f0006c3f644de8f2fd66d59dd4fbf
op_doi https://doi.org/10.1038/s41612-023-00431-1
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