AI Article Synopsis

  • A sea-ice record from northern Greenland over the last 10,000 years shows that multiyear sea ice was at its lowest around 8,500 to 6,000 years ago, with the ice limit located much farther north than today.
  • The rise in multiyear sea ice over the past 2,500 years is associated with increased ice export from the western Arctic and more variability in ice-drift patterns.
  • There’s a lack of consistency in historical sea-ice changes, likely influenced by large-scale atmospheric factors, which current models fail to accurately capture and should be further investigated to enhance future sea-ice distribution predictions.

Article Abstract

We present a sea-ice record from northern Greenland covering the past 10,000 years. Multiyear sea ice reached a minimum between ~8500 and 6000 years ago, when the limit of year-round sea ice at the coast of Greenland was located ~1000 kilometers to the north of its present position. The subsequent increase in multiyear sea ice culminated during the past 2500 years and is linked to an increase in ice export from the western Arctic and higher variability of ice-drift routes. When the ice was at its minimum in northern Greenland, it greatly increased at Ellesmere Island to the west. The lack of uniformity in past sea-ice changes, which is probably related to large-scale atmospheric anomalies such as the Arctic Oscillation, is not well reproduced in models. This needs to be further explored, as it is likely to have an impact on predictions of future sea-ice distribution.

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http://dx.doi.org/10.1126/science.1202760DOI Listing

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