Obliquity-driven expansion of North Atlantic sea ice during the last glacial

North Atlantic late Pleistocene climate (60,000 to 11,650 years ago) was characterized by abrupt and extreme millennial duration oscillations known as Dansgaard-Oeschger (D-O) events. However, during the Last Glacial Maximum (LGM) 23,000 to 19,000 cal years ago (23 to 19 ka), no D-O events are obser...

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Bibliographic Details
Published in:Geophysical Research Letters
Main Authors: Turney, Chris S.M., Thomas, Zoë A., Hutchinson, David K., Bradshaw, Corey J.A., Brook, Barry W., England, Matthew H., Fogwill, Christopher J., Jones, Richard T., Palmer, Jonathan, Hughen, Konrad A., Cooper, Alan
Format: Article in Journal/Newspaper
Language:English
Published: 2015
Subjects:
Greenland
Greenland ice cores
Labrador Sea
North Atlantic
Sea ice
Online Access:https://eprints.soton.ac.uk/476637/
Description
Summary:North Atlantic late Pleistocene climate (60,000 to 11,650 years ago) was characterized by abrupt and extreme millennial duration oscillations known as Dansgaard-Oeschger (D-O) events. However, during the Last Glacial Maximum (LGM) 23,000 to 19,000 cal years ago (23 to 19 ka), no D-O events are observed in the Greenland ice cores. Our new analysis of the Greenland δ18O record reveals a switch in the stability of the climate system around 30 ka, suggesting that a critical threshold was passed. Climate system modeling suggests that low axial obliquity at this time caused vastly expanded sea ice in the Labrador Sea, shifting Northern Hemisphere westerly winds south and reducing the strength of meridional overturning circulation. The results suggest that these feedbacks tipped the climate system into full glacial conditions, leading to maximum continental ice growth during the LGM.

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