NPJ Climate and Atmospheric Science, 20 May 2026
Human-caused warming has been the primary driver of winter Arctic sea-ice loss since 1980, accounting for most of the observed decline across large parts of the Arctic. Using climate observations from 1950-2024, researchers developed a new approach to distinguish the effects of anthropogenic climate change from those of natural climate variability on winter sea ice. Unlike summer sea ice, which has long exhibited a clear response to rising temperatures, winter sea ice has traditionally been considered more strongly influenced by natural variability. The study found that while natural climate patterns – particularly in the North Atlantic and parts of the central and eastern tropical Pacific – affect winter sea ice conditions, their influence is secondary to that of human-caused warming. The researchers also identified that Arctic sea ice carries far-reaching effects on global climate and weather patterns, with linkages between winter sea ice loss and warmer summer temperatures across much of Europe.
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