Timing and nature of AMOC recovery across Termination 2 and magnitude of deglacial CO2 change

Differences in the sequence and timing of ocean circulation changes across glacial terminations could affect the magnitude of deglacial atmospheric CO2 rise. Here, the authors argue that late ocean circulation recovery during the penultimate deglaciation (T2) led to a larger rise in CO2compared with...

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Bibliographic Details
Main Authors: Emily L. Deaney, Stephen Barker, Tina van de Flierdt
Format: article
Language:EN
Published: Nature Portfolio 2017
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Online Access:https://doaj.org/article/2c33df67abf64c7d98d0bf35ef2ccf24
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