Articles | Volume 18, issue 10
https://doi.org/10.5194/bg-18-3189-2021
https://doi.org/10.5194/bg-18-3189-2021
Research article
 | 
27 May 2021
Research article |  | 27 May 2021

Ocean carbon cycle feedbacks in CMIP6 models: contributions from different basins

Anna Katavouta and Richard G. Williams

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Latest update: 17 Nov 2024
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Short summary
Diagnostics of the latest-generation Earth system models reveal the ocean will continue to absorb a large fraction of the anthropogenic carbon released to the atmosphere in the next century, with the Atlantic Ocean storing a large amount of this carbon relative to its size. The ability of the ocean to absorb carbon will reduce in the future as the ocean warms and acidifies. This reduction is larger in the Atlantic Ocean due to a weakening of the meridional overturning with changes in climate.
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