Gp. Ayers et al., DIMETHYLSULFIDE OXIDATION AND THE RATIO OF METHANESULFONATE TO NON SEA-SALT SULFATE IN THE MARINE AEROSOL, Journal of atmospheric chemistry, 25(3), 1996, pp. 307-325
A box model of DMS oxidation in the clean, low-NO, marine atmospheric
boundary layer has been used to predict the latitude dependence of the
aerosol methanesulfonate to non sea-salt sulfate ratio. The observed
latitude dependence of this ratio in the Southern Hemisphere can be re
produced reasonably well if the full suite of reactions proposed by Yi
n ct al. (1990a) is employed, and a strong temperature dependence is s
pecified in the rates of decomposition of CH3SO2 and CH3SO3 radicals.