E. Kjellstrom, A 3-DIMENSIONAL GLOBAL-MODEL STUDY OF CARBONYL SULFIDE IN THE TROPOSPHERE AND THE LOWER STRATOSPHERE, Journal of atmospheric chemistry, 29(2), 1998, pp. 151-177
Global distributions of carbonyl sulfide and carbon disulfide have bee
n calculated with a three-dimensional global model of the atmospheric
general circulation (ECHAM). The model calculates a global sink streng
th for carbonyl sulfide of 0.3 Tg S yr(-1), with vegetation uptake bei
ng the largest sink. With this sink strength, the sources have to be c
lose to the lower limit of the present estimate in the literature. The
calculated mixing ratios are higher in the Southern Hemisphere than i
n the Northern Hemisphere. This interhemispheric gradient is the oppos
ite of what is observed demonstrating that the present knowledge of th
e distribution of sinks and sources is not fully adequate. The model c
alculations support the idea that the open oceans could act as a net s
ink of carbonyl sulfide. The calculated stratospheric photolysis of ca
rbonyl sulfide constitutes about 4% of the total sink of carbonyl sulf
ide. A stratospheric production of sulfate from carbonyl sulfide of 0.
013 Tg S yr(-1) is obtained, which is 3 to 12 times less than what is
needed to maintain the stratospheric sulfate aerosol layer. Although t
hese results are associated with uncertainties, due to the low upper b
oundary and coarse vertical resolution of the model, they support rece
nt findings of a low stratospheric production of sulfate from carbonyl
sulfide. instead, sulfur dioxide transported from the troposphere is
calculated to be the most important precursor for the stratospheric su
lfate aerosol layer.