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Biogeosciences An interactive open-access journal of the European Geosciences Union
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Millennial-scale changes in oceanic CO2 uptake due to global warming are simulated by a GCM and offline biogeochemical model. Sensitivity studies show that decreases in oceanic CO2 uptake are mainly caused by a weaker biological pump and seawater warming. Enhanced CO2 uptake due to weaker equatorial upwelling cancels out reduced CO2 uptake due to weaker AMOC and AABW formation. Thus, circulation change plays only a small direct role in reduction of CO2 uptake due to global warming.
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Articles | Volume 15, issue 13
Articles | Volume 15, issue 13
Biogeosciences, 15, 4163–4180, 2018
https://doi.org/10.5194/bg-15-4163-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
Biogeosciences, 15, 4163–4180, 2018
https://doi.org/10.5194/bg-15-4163-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 15, issue 13

Research article 10 Jul 2018

Research article | 10 Jul 2018

Long-term response of oceanic carbon uptake to global warming via physical and biological pumps

Akitomo Yamamoto et al.

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Latest update: 20 Jan 2021
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Short summary
Millennial-scale changes in oceanic CO2 uptake due to global warming are simulated by a GCM and offline biogeochemical model. Sensitivity studies show that decreases in oceanic CO2 uptake are mainly caused by a weaker biological pump and seawater warming. Enhanced CO2 uptake due to weaker equatorial upwelling cancels out reduced CO2 uptake due to weaker AMOC and AABW formation. Thus, circulation change plays only a small direct role in reduction of CO2 uptake due to global warming.
Read more
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Final-revised paper
Preprint
Biogeosciences

An interactive open-access journal of the European Geosciences Union

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