Here we compare 11 CMIP6 marine biogeochemical models and find the largest source of inter-model uncertainty in their representation of the marine carbon cycle is phytoplankton-specific loss rates to zooplankton
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seasonally, thus influencing the flux of carbon in the deep ocean. A better understanding of this process and how it might evolve with our changing climate may inform climate models and help us take informed steps to mitigate the impacts of global warming on the marine carbon cycle and food...
The current generation of Earth system models used by the United Nations to project future climate scenarios (CMIP6) relies heavily on marine biogeochemical models to track the fate of carbon absorbed into the oceans. Here we compare 11 CMIP6 marine biog
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Landry Zooplankton and the ocean carbon cycle Annu. Rev. Mar. Sci., 9 (2017), pp. 413-444, 10.1146/annurev-marine-010814-015924 View in ScopusGoogle Scholar Stephenson et al., 2018 F. Stephenson, J.R. Leathwick, S.W. Geange, R.H. Bulmer, J.E. Hewitt, O.F. Anderson, A.A....