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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

.18 PgC yr −1 ), GFDL-ESM2M (2.04 ± 0.3 PgC yr −1 ), HadGEM2-ES (2.01 ± 0.12 PgC yr −1 ), HadGEM2-CC (2.00 ± 0.19 PgC yr −1 ), and MPI-ESM-LR (1.96 ± 0.17 PgC yr −1 ) simulate values of both the global mean and interannual variability close to the observational values, while CanESM2 (1.64 ± 0.25 PgC yr −1 ) shows the weaker CO 2 sink and NorESM1-ME (2.32 ± 0.15 PgC yr −1 ) well matches the Takahashi estimate. The fact that the CMIP5 models lack processes associated with the river loop of the carbon

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