Articles | Volume 18, issue 4
https://doi.org/10.5194/cp-18-775-2022
https://doi.org/10.5194/cp-18-775-2022
Research article
 | 
12 Apr 2022
Research article |  | 12 Apr 2022

Dynamic boreal summer atmospheric circulation response as negative feedback to Greenland melt during the MIS-11 interglacial

Brian R. Crow, Matthias Prange, and Michael Schulz

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Latest update: 25 Jun 2024
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Short summary
To better understand the climate conditions which lead to extensive melting of the Greenland ice sheet, we used climate models to reconstruct the climate conditions of the warmest period of the last 800 000 years, which was centered around 410 000 years ago. Surprisingly, we found that atmospheric circulation changes may have acted to reduce the melt of the ice sheet rather than enhance it, despite the extensive warmth of the time.