Fig. 3
From: Anthropogenic combustion iron as a complex climate forcer
Soluble iron deposition flux to the ocean. a, b The deposition flux over a the global ocean and b the southern ocean at mid- and high-latitudes (30–90°S) from anthropogenic (AN, fossil fuel+biofuel), biomass burning (BB), and mineral dust (Dust) sources for the BASE and NEW simulations (5-year mean). Error bars show the uncertainty range by the assumption of the fraction of magnetite to anthropogenic combustion iron (between 20% and 80%). c Global distributions of the ratio of total soluble iron deposition flux (AN+BB+Dust) between the NEW and the BASE simulations (5-year mean)
