This is a repository copy of Deep-water circulation changes lead North Atlantic climate during deglaciation. White Rose Research Online URL for this paper: http://eprints.whiterose.ac.uk/144315/ Version: Published Version Article: Muschitiello, F., D'Andrea, W.J., Schmittner, A. et al. (9 more authors) (2019) Deep-water circulation changes lead North Atlantic climate during deglaciation. Nature Communications, 10. 1272. ISSN 2041-1723 https://doi.org/10.1038/s41467-019-09237-3 Reuse This article is distributed under the terms of the Creative Commons Attribution (CC BY) licence. This licence allows you to distribute, remix, tweak, and build upon the work, even commercially, as long as you credit the authors for the original work. More information and the full terms of the licence here: https://creativecommons.org/licenses/ Takedown If you consider content in White Rose Research Online to be in breach of UK law, please notify us by emailing
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[email protected] https://eprints.whiterose.ac.uk/ ARTICLE https://doi.org/10.1038/s41467-019-09237-3 OPEN Deep-water circulation changes lead North Atlantic climate during deglaciation Francesco Muschitiello1,2,3, William J. D’Andrea2, Andreas Schmittner4, Timothy J. Heaton5, Nicholas L. Balascio6, Nicole deRoberts2, Marc W. Caffee 7,8, Thomas E. Woodruff7, Kees C. Welten9, Luke C. Skinner10, Margit H. Simon3 & Trond M. Dokken3 Constraining the response time of the climate system to changes in North Atlantic Deep 1234567890():,; Water (NADW) formation is fundamental to improving climate and Atlantic Meridional Overturning Circulation predictability.