Changes in sea ice concentration explain half of the winter warming of the Arctic surface
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2025
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Journal Title:Communications Earth & Environment
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Description:Arctic winter warming is stronger than in summer, but its driving mechanisms remain debated, particularly the roles of local processes, like sea-ice loss, versus remote factors, like atmospheric heat transport. Here we introduce a novel decomposition framework that characterizes Arctic warming as a function of historical atmospheric circulation, sea ice concentration, and carbon dioxide changes using observational and reanalysis data. We show that sea ice changes explain about 55% of the winter Arctic near-surface temperature trend during 1959–2015, after removing the effects directly connected to atmospheric circulation. Dynamically induced warming accounts for about 20% at surface and up to 80% in mid-troposphere. The remaining ~25% is attributed to the increase in carbon dioxide, though it also indirectly affects sea-ice loss and circulation-related warming. These findings highlight the dominant role of sea ice loss and change in atmospheric dynamics in affecting the historical Arctic winter warming.
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Source:Communications Earth & Environment, 6(1)
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Series:PMEL contribution no. 5722
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DOI:
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ISSN:2662-4435
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Rights Information:CC BY
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Compliance:Submitted
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Main Document Checksum:urn:sha-512:3dc86f77516e2e763f9e14d6dfab75424919869759f49401a045b1ed71f4e1fb073138a14a8fb45202b4ded0981ef56d07cf1b91b8547fd2696839cf2d3cdbb3
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