A twenty-first century structural change in Antarctica’s sea ice system

Abstract From 1979 to 2016, total Antarctic sea ice extent experienced a positive trend with record winter maxima in 2012 and 2014. Record summer minima followed within the period 2017-2024, raising the possibility that the Antarctic sea ice system might be changing state. Here we use a Bayesian reconstruction of Antarctic sea ice extent which extends the record back to 1899, to show that the sequence of extreme minima in summer Antarctic sea ice extent is unlikely to have happened in the 20th century. We show that they represent a structural change in the sea ice system, manifest by increased persistence in the sea ice extent anomalies and a strongly reduced tendency to return to the mean state. Further, our analysis suggests that we may no longer rely on the past, long-term, behavior of the sea ice system to predict its future state. Extreme conditions may characterize the future state of Antarctic sea ice.

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Publication Details

Journal
Communications Earth & Environment
Published
2025-02-21
DOI
https://doi.org/10.1038/s43247-025-02107-5
Citations
19
Primary Topic
Cryospheric studies and observations
Type
article
Field-Weighted Citation Impact
24.71

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article

A twenty-first century structural change in Antarctica’s sea ice system

Thomas Maierhofer, Mark S. Handcock, Marilyn Raphael, Ryan L. Fogt et al.
19 citations
Communications Earth & Environment
Cryospheric studies and observations
24.71
article

A twenty-first century structural change in Antarctica’s sea ice system

Thomas Maierhofer, Mark S. Handcock, Marilyn Raphael, Ryan L. Fogt, Will Hobbs
article en
19 citations

Abstract

Abstract From 1979 to 2016, total Antarctic sea ice extent experienced a positive trend with record winter maxima in 2012 and 2014. Record summer minima followed within the period 2017-2024, raising the possibility that the Antarctic sea ice system might be changing state. Here we use a Bayesian reconstruction of Antarctic sea ice extent which extends the record back to 1899, to show that the sequence of extreme minima in summer Antarctic sea ice extent is unlikely to have happened in the 20th century. We show that they represent a structural change in the sea ice system, manifest by increased persistence in the sea ice extent anomalies and a strongly reduced tendency to return to the mean state. Further, our analysis suggests that we may no longer rely on the past, long-term, behavior of the sea ice system to predict its future state. Extreme conditions may characterize the future state of Antarctic sea ice.

Communications Earth & EnvironmentVol. 6(1)
University of Tasmania (AU), Australian Antarctic Division (AU), University of California, Los Angeles (US), Ohio University (US)
National Science Foundation
Openalex Percentile: Top 0%
Cryospheric studies and observations
24.71
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