Holocene North Atlantic Overturning in an atmosphere-ocean-sea-ice model compared to proxy-based reconstructions

Climate and ocean circulation in the North Atlantic region changed over the course of the Holocene, partly because of disintegrating ice sheets and partly because of an orbital-induced insolation trend. In the Nordic Seas, this impact was accompanied by a rather small, but significant, amount of Gre...

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Bibliographic Details
Published in:Paleoceanography
Main Authors: Blaschek, M., Renssen, H., Kissel, C., Thornalley, D.
Format: Article in Journal/Newspaper
Language:English
Published: 2015
Subjects:
Greenland
Ice Sheet
Nordic Seas
North Atlantic
Sea ice
Online Access:https://research.vu.nl/en/publications/bab2a8db-95f9-49ee-9861-c5ea4d3003ee
https://doi.org/10.1002/2015PA002828
http://hdl.handle.net/1871.1/bab2a8db-95f9-49ee-9861-c5ea4d3003ee
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Summary:Climate and ocean circulation in the North Atlantic region changed over the course of the Holocene, partly because of disintegrating ice sheets and partly because of an orbital-induced insolation trend. In the Nordic Seas, this impact was accompanied by a rather small, but significant, amount of Greenland ice sheet melting. We have employed the EMIC LOVECLIM and compared our model simulations with proxy-based reconstructions of δ

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