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
Published in: | Communications Earth & Environment |
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Main Authors: | , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Nature Portfolio
2020
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Subjects: | |
Online Access: | https://doi.org/10.1038/s43247-020-00024-3 https://doaj.org/article/cb8a51b537314a7abe0b32656b054377 |
Summary: | 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 |
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