Synchronous volcanic eruptions and abrupt climate change ∼17.7 ka plausibly linked by stratospheric ozone depletion

Cold and dry glacial-state climate conditions persisted in the Southern Hemisphere until approximately 17.7 ka, when paleoclimate records show a largely unexplained sharp, nearly synchronous acceleration in deglaciation. Detailed measurements in Antarctic ice cores document exactly at that time a un...

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Bibliographic Details
Published in:Proceedings of the National Academy of Sciences
Main Authors: McConnell, Joseph, Burke, Andrea, Dunbar, Nelia, Köhler, Peter, Thomas, Jennie, Arienzo, Monica, Chellman, Nathan, Maselli, Olivia, Sigl, Michael, Adkins, Jess, Baggenstos, Daniel, Burkhart, John, Brook, Edward, Buizert, Christo, Cole-Dai, Jihong, Fudge, T. J., Knorr, Gregor, Graf, Hans-F., Grieman, Mackenzie, Iverson, Nels, McGwire, Kenneth, Mulvaney, Robert, Paris, Guillaume, Rhodes, Rachael, Saltzman, Eric, Severinghaus, Jeffrey, Steffensen, Jørgen, Taylor, Kendrick, Winckler, Gisela
Format: Article in Journal/Newspaper
Language:unknown
Published: National Academy of Sciences 2017
Subjects:
Online Access:https://nrl.northumbria.ac.uk/id/eprint/37617/
https://doi.org/10.1073/pnas.1705595114