Southern Hemisphere westerlies as a driver of the early deglacial atmospheric CO2 rise
Despite decades of research, the sequence of events leading to the deglacial atmospheric CO2 rise remains unclear. Menviel et al. show that Southern Ocean convection driven by intensified Southern Hemisphere westerlies during Heinrich stadial 1 can explain the abrupt pCO2 rise and changes in atmosph...
| Main Authors: | , , , , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Nature Portfolio
2018-06-01
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| Series: | Nature Communications |
| Online Access: | https://doi.org/10.1038/s41467-018-04876-4 |