“…To this end, given the surface winds range we encountered (U 30 < 16 m s −1 ), as a first approximation, the attribution between the local contribution of N SSA and N LRT can be scaled to the concentration. SSA is produced by the wind stress over the ocean surface, and its concentration has been shown to be (nonlinearly) propositional to the wind speed 4,20,21 , with typical concentrations in the range of 10 s per cubic centimeter 21,22 . Whereas the contribution of N LRT is proportional to the yields of the continental sources (dust, pollution, smoke), the distance the aerosol traveled, and with aerosol lifetime in the atmosphere, in general, inversely proportional to the aerosol size 3,23,24 , the quantity of smaller diameters will be greater.…”