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 and Winckler, Gisela (2017) Synchronous volcanic eruptions and abrupt climate change ∼17.7 ka plausibly linked by stratospheric ozone depletion. Proceedings of the National Academy of Sciences of the United States of America, 114 (38). pp. 10035-10040. ISSN 0027-8424
Full text not available from this repository.Abstract
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 unique, ∼192-y series of massive halogen-rich volcanic eruptions geochemically attributed to Mount Takahe in West Antarctica. Rather than a coincidence, we postulate that halogen-catalyzed stratospheric ozone depletion over Antarctica triggered large-scale atmospheric circulation and hydroclimate changes similar to the modern Antarctic ozone hole, explaining the synchronicity and abruptness of accelerated Southern Hemisphere deglaciation.
Item Type: | Article |
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Uncontrolled Keywords: | climate, deglaciation, volcanism, ozone, aerosol |
Subjects: | F800 Physical and Terrestrial Geographical and Environmental Sciences |
Department: | Faculties > Engineering and Environment > Geography and Environmental Sciences |
Depositing User: | Paul Burns |
Date Deposited: | 17 Jan 2019 10:16 |
Last Modified: | 10 Oct 2019 21:16 |
URI: | http://nrl.northumbria.ac.uk/id/eprint/37617 |
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