Fast and slow components of interstadial warming in the North Atlantic during the last glacial

Abstract The abrupt nature of warming events recorded in Greenland ice-cores during the last glacial has generated much debate over their underlying mechanisms. Here, we present joint marine and terrestrial analyses from the Portuguese Margin, showing a succession of cold stadials and warm interstad...

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Bibliographic Details
Published in:Communications Earth & Environment
Main Authors: Margari, Vasiliki, Skinner, Luke C., Menviel, Laurie, Capron, Emilie, Rhodes, Rachael H., Mleneck-Vautravers, Maryline J., Ezat, Mohamed M., Martrat, Belen, Grimalt, Joan O., Hodell, David A., Tzedakis, Polychronis C.
Format: Article in Journal/Newspaper
Language:English
Published: Springer Science and Business Media LLC 2020
Subjects:
General Earth and Planetary Sciences
General Environmental Science
Greenland
Greenland ice core
Greenland ice cores
ice core
North Atlantic
Sea ice
Online Access:http://dx.doi.org/10.1038/s43247-020-0006-x
https://www.nature.com/articles/s43247-020-0006-x.pdf
https://www.nature.com/articles/s43247-020-0006-x
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Summary:Abstract The abrupt nature of warming events recorded in Greenland ice-cores during the last glacial has generated much debate over their underlying mechanisms. Here, we present joint marine and terrestrial analyses from the Portuguese Margin, showing a succession of cold stadials and warm interstadials over the interval 35–57 ka. Heinrich stadials 4 and 5 contain considerable structure, with a short transitional phase leading to an interval of maximum cooling and aridity, followed by slowly increasing sea-surface temperatures and moisture availability. A climate model experiment reproduces the changes in western Iberia during the final part of Heinrich stadial 4 as a result of the gradual recovery of the Atlantic meridional overturning circulation. What emerges is that Greenland ice-core records do not provide a unique template for warming events, which involved the operation of both fast and slow components of the coupled atmosphere–ocean–sea-ice system, producing adjustments over a range of timescales.

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