Fig. 5: Change in NPPΣ of the global ocean between time slices.
From: Vertically migrating phytoplankton fuel high oceanic primary production
NPPΣ calculated by the model when the chemocline depths representing the recent past (1971–2000, ‘1985’) are altered on the basis of a scenario simulation by the MPI-ESM for 2071–2100 (‘2085’).
