Southern Ocean carbon sink enhanced by sea-ice feedbacks at the Antarctic Cold Reversal

Increased Southern Ocean productivity driven by sea-ice feedbacks contributed to a slowdown in rising CO(2)levels during the last deglaciation, according to analyses of marine-derived aerosols from an Antarctic ice core. The Southern Ocean occupies 14% of the Earth's surface and plays a fundame...

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Bibliographic Details
Published in:Nature Geoscience
Main Authors: Fogwill, C. J., Turney, C. S. M., Menviel, L., Baker, A., Weber, M. E., Ellis, B., Thomas, Z. A., Golledge, N. R., Etheridge, D., Rubino, M., Thornton, D. P., van Ommen, T. D., Moy, A. D., Curran, M. A. J., Davies, S., Bird, M., I, Munksgaard, N. C., Rootes, C. M., Millman, H., Vohra, J., Rivera, A., Mackintosh, A., Pike, J., Hall, I. R., Bagshaw, E. A., Rainsley, E., Bronk-Ramsey, C., Montenari, M., Cage, A. G., Harris, M. R. P., Jones, R., Power, A., Love, J., Young, J., Weyrich, L. S., Cooper, A.
Format: Article in Journal/Newspaper
Language:English
Published: Nature 2020
Subjects:
Online Access:https://doi.org/10.1038/s41561-020-0587-0
https://repositorio.uchile.cl/handle/2250/176350