Evaluating CMIP5 ocean biogeochemistry and Southern Ocean carbon uptake using atmospheric potential oxygen: Present-day performance and future projection

Observed seasonal cycles in atmospheric potential oxygen (APO~O2+1.1 CO2) were used to evaluate eight ocean biogeochemistry models from the Coupled Model Intercomparison Project (CMIP5). Model APO seasonal cycles were computed from the CMIP5 air-sea O2 and CO2 fluxes and compared to observations at...

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Bibliographic Details
Published in:Geophysical Research Letters
Main Authors: Nevison, C., Manizza, M., Keeling, R., Stephens, B., Bent, J., Dunne, J., Ilyina, T., Long, M., Resplandy, L., Tjiputra, J., Yukimoto, S.
Format: Article in Journal/Newspaper
Language:English
Published: 2016
Subjects:
Southern Ocean
Ocean acidification
Online Access:http://hdl.handle.net/11858/00-001M-0000-002A-0F78-6
http://hdl.handle.net/11858/00-001M-0000-002D-3EAC-1
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Summary:Observed seasonal cycles in atmospheric potential oxygen (APO~O2+1.1 CO2) were used to evaluate eight ocean biogeochemistry models from the Coupled Model Intercomparison Project (CMIP5). Model APO seasonal cycles were computed from the CMIP5 air-sea O2 and CO2 fluxes and compared to observations at three Southern Hemisphere monitoring sites. Four of the models captured either the observed APO seasonal amplitude or phasing relatively well, while the other four did not. Many models had an unrealistic seasonal phasing or amplitude of the CO2 flux, which in turn influenced APO. By 2100 under RCP8.5, the models projected little change in the O2 component of APO but large changes in the seasonality of the CO2 component associated with ocean acidification. The models with poorer performance on present-day APO tended to project larger net carbon uptake in the Southern Ocean, both today and in 2100. ©2016. American Geophysical Union.

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