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A. Anav, P. Friedlingstein, M. Kidston, L. Bopp, P. Ciais, P. Cox, C. Jones, M. Jung, R. Myneni, and Z. Zhu

the land carbon cycle ( Piao et al. 2009 ). In the ocean, physical fields include sea surface temperature (SST), which is important for biological growth and respiration rates as well as air–sea gas exchange, and mixing- layer depth (MLD), which influences nutrient entrainment and the average light field observed by the phytoplankton ( Martinez et al. 2009 ). Considering the land and ocean carbon fluxes, some of the available datasets used for the comparison come from atmospheric inversion

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