articleScienceMar 23, 2006Closed access

Simulating Arctic Climate Warmth and Ice Field Retreat in the Last Interglaciation

NSF National Center for Atmospheric Research · University of Arizona · +4 more institutions

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Abstract

In the future, Arctic warming and the melting of polar glaciers will be considerable, but the magnitude of both is uncertain. We used a global climate model, a dynamic ice sheet model, and paleoclimatic data to evaluate Northern Hemisphere high-latitude warming and its impact on Arctic icefields during the Last Interglaciation. Our simulated climate matches paleoclimatic observations of past warming, and the combination of physically based climate and ice-sheet modeling with ice-core constraints indicate that the Greenland Ice Sheet and other circum-Arctic ice fields likely contributed 2.2 to 3.4 meters of sea-level rise during the Last Interglaciation.

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Authors

6

Topics & keywords

Keywords
  • Ice field
  • Greenland ice sheet
  • Arctic
  • Ice sheet
  • Climatology
  • Arctic ice pack
  • Geology
  • Glacier
UN Sustainable Development Goals
  • Climate action
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