Interglacial instability of North Atlantic Deep Water ventilation

Disrupting North Atlantic Deep Water (NADW) ventilation is a key concern in climate projections. We use (sub)centennially resolved bottom water d 13 C records that span the interglacials of the last 0.5 million years to assess the frequency of and the climatic backgrounds capable of triggering large...

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Bibliographic Details
Published in:Science
Main Authors: Galaasen, Eirik Vinje, Ninnemann, Ulysses S., Kessler, Augustin, Irvalı, Nil, Rosenthal, Yair, Tjiputra, Jerry, Bouttes, Nathaëlle, Roche, Didier M., Kleiven, Helga F., Hodell, David A.
Format: Article in Journal/Newspaper
Language:English
Published: 2020
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Online Access:https://research.vu.nl/en/publications/ef0a5bbc-9d80-4ee4-b113-3fafa5ba4c4b
https://doi.org/10.1126/science.aay6381
https://hdl.handle.net/1871.1/ef0a5bbc-9d80-4ee4-b113-3fafa5ba4c4b
https://research.vu.nl/ws/files/121792416/Interglacial_instability_of_North_Atlantic_Deep_Water_ventilation.pdf
http://www.scopus.com/inward/record.url?scp=85082470559&partnerID=8YFLogxK
http://www.scopus.com/inward/citedby.url?scp=85082470559&partnerID=8YFLogxK
Description
Summary:Disrupting North Atlantic Deep Water (NADW) ventilation is a key concern in climate projections. We use (sub)centennially resolved bottom water d 13 C records that span the interglacials of the last 0.5 million years to assess the frequency of and the climatic backgrounds capable of triggering large NADW reductions. Episodes of reduced NADW in the deep Atlantic, similar in magnitude to glacial events, have been relatively common and occasionally long-lasting features of interglacials. NADW reductions were triggered across the range of recent interglacial climate backgrounds, which demonstrates that catastrophic freshwater outburst floods were not a prerequisite for large perturbations. Our results argue that large NADW disruptions are more easily achieved than previously appreciated and that they occurred in past climate conditions similar to those we may soon face.