J. Lelieveld et al., TERRESTRIAL SOURCES AND DISTRIBUTION OF ATMOSPHERIC SULFUR, Philosophical transactions-Royal Society of London. Biological sciences, 352(1350), 1997, pp. 149-157
The general circulation model ECHAM has been coupled to a chemistry an
d sulphur cycle model to study the impact of terrestrial, i.e. mostly
anthropogenic sulphur dioxide (SO2), sources on global distributions o
f sulphur species in the atmosphere. We briefly address currently avai
lable source inventories. It appears that global estimates of natural
emissions are associated with uncertainties up to a factor of 2, while
anthropogenic emissions have uncertainty ranges of about +/- 30 %. Fu
rther, some recent improvements in the model descriptions of multiphas
e chemistry and deposition processes are presented. Dry deposition is
modelled consistently with meteorological processes and surface proper
ties. The results indicate that surface removal of SO2 is less efficie
nt than previously assumed, and that the SO2 lifetime is thus longer.
Coupling of the photochemistry and sulphur chemistry schemes in the mo
del improves the treatment of multiphase processes such as oxidant (hy
drogen peroxide) supply in aqueous phase SO2 oxidation. The results su
ggest that SO2 oxidation by ozone (O-3) in the aqueous phase is more i
mportant than indicated in earlier work. However, it appears that we s
till overestimate atmospheric SO2 concentrations near the surface in t
he relatively polluted Northern Hemisphere. On the other hand, we some
what underestimate sulphate levels in these regions, which suggests th
at additional heterogeneous reaction mechanisms, e.g. on aerosols, enh
ance SO2 oxidation.