Northward shift of the southern westerlies during the Antarctic Cold Reversal

• Published in: Quaternary Science Reviews
• Main Authors: Joseph, Alexander, Fletcher, Michael-Shawn, Pedro, Joel, Hall, Tegan, Mariani, Michela, Beck, Kristen, Blaauw, Maarten, Hodgson, Dominic, Heijnis, Henk, Gadd, Patricia, Lise-Pronovost, Agathe
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: Elsevier 2021
• Subjects: Geology; Archeology; Ecology; Evolution; Behavior and Systematics; Global and Planetary Change; Geography: Geosciences; Antarctic; Southern Ocean; The Antarctic; Antarc*; North Atlantic
• Online Access: https://doi.org/10.1016/j.quascirev.2021.107189; https://nottingham-repository.worktribe.com/file/6296098/1/Fletcher%20Et%20Al%20ACR%20QSR%20REVISION%20FINAL; https://nottingham-repository.worktribe.com/output/6296098

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 CO2 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 Bølling–Allerød 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 CO2 from the Southern Ocean drove the deglacial rise in atmospheric CO2.