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BG | Articles | Volume 17, issue 13
Biogeosciences, 17, 3439–3470, 2020
https://doi.org/10.5194/bg-17-3439-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
Biogeosciences, 17, 3439–3470, 2020
https://doi.org/10.5194/bg-17-3439-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 06 Jul 2020

Research article | 06 Jul 2020

Twenty-first century ocean warming, acidification, deoxygenation, and upper-ocean nutrient and primary production decline from CMIP6 model projections

Lester Kwiatkowski et al.

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AR: Author's response | RR: Referee report | ED: Editor decision
ED: Publish subject to minor revisions (review by editor) (27 Mar 2020) by Fortunat Joos
AR by Lester Kwiatkowski on behalf of the Authors (28 Apr 2020)  Author's response
ED: Publish subject to technical corrections (25 May 2020) by Fortunat Joos
AR by Lester Kwiatkowski on behalf of the Authors (28 May 2020)  Author's response    Manuscript
Publications Copernicus
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Short summary
We assess 21st century projections of marine biogeochemistry in the CMIP6 Earth system models. These models represent the most up-to-date understanding of climate change. The models generally project greater surface ocean warming, acidification, subsurface deoxygenation, and euphotic nitrate reductions but lesser primary production declines than the previous generation of models. This has major implications for the impact of anthropogenic climate change on marine ecosystems.
We assess 21st century projections of marine biogeochemistry in the CMIP6 Earth system models....
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