Northward shift of the southern westerlies during the Antarctic Cold Reversal

Inter-hemispheric asynchrony of climate change through the last deglaciation has been theoretically linked to latitudinal shifts in the southern westerlies via their influence over CO 2 out-gassing from the Southern Ocean. Proxy-based reconstructions disagree on the behaviour of the westerlies throu...

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Bibliographic Details
Published in:Quaternary Science Reviews
Main Authors: Fletcher, M-S, Pedro, J, Hall, T, Mariani, M, Alexander, JA, Beck, K, Blaauw, M, Hodgson, DA, Heijnis, H, Gadd, PS, Lise-Pronovos, A
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier Ltd 2021
Subjects:
Earth Sciences
Climate change science
Climate change processes
Antarctic
Southern Ocean
The Antarctic
Antarc*
North Atlantic
Online Access:https://doi.org/10.1016/j.quascirev.2021.107189
http://ecite.utas.edu.au/151337
Description
Summary:Inter-hemispheric asynchrony of climate change through the last deglaciation has been theoretically linked to latitudinal shifts in the southern westerlies via their influence over CO 2 out-gassing from the Southern Ocean. Proxy-based reconstructions disagree on the behaviour of the westerlies through this interval. The last deglaciation was interrupted in the Southern Hemisphere by the Antarctic Cold Reversal (ACR; 14.7 to 13.0 ka BP (thousand years Before Present)), a millennial-scale cooling event that coincided with the Bllinge-Allerd warm phase in the North Atlantic (BA; 14.7 to 12.7 ka BP). We present terrestrial proxy palaeoclimate data that demonstrate a migration of the westerlies during the last deglaciation. We support the hypothesis that wind-driven out-gassing of old CO 2 from the Southern Ocean drove the deglacial rise in atmospheric CO 2 .

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