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Communications Earth & Environment (1)

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Southern Ocean convection amplified past Antarctic warming and atmospheric CO₂ rise during Heinrich Stadial 4

Antarctic warming and the rise of atmospheric CO2 levels during Heinrich Stadial 4 were amplified by enhanced convection and air-sea gas and heat exchange in the Southern Ocean, according to an analysis of deep water ventilation and temperature proxies

Luke Skinner
Laurie Menviel
Mervyn Greaves
ResearchOpen Access22 Sept 2020
Communications Earth & Environment

Volume: 1, P: 1-8

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Southern Ocean convection amplified past Antarctic warming and atmospheric CO₂ rise during Heinrich Stadial 4