Mathematics – Logic
Scientific paper
Nov 2003
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2003georl..30vasc1l&link_type=abstract
Geophysical Research Letters, Volume 30, Issue 22, pp. ASC 1-1, CiteID 2136, DOI 10.1029/2003GL018370
Mathematics
Logic
9
Atmospheric Composition And Structure: Aerosols And Particles (0345, 4801), Atmospheric Composition And Structure: Troposphere-Composition And Chemistry, Oceanography: Biological And Chemical: Aerosols (0305)
Scientific paper
Tropospheric distributions of H2SO4-H2O binary nucleation rates are calculated from a 3D model with DMS chemistry. Two mechanisms are used that include and exclude an SO2-independent H2SO4 production path. In the lower troposphere, the SO2-independent path generates extra H2SO4 and, consequently, much higher aerosol nucleation rates. However, these rates are less than 10-5 particles cm-3 s-1 in most of the lower troposphere, which indicates that DMS oxidation does not lead to appreciable aerosol formation there. In the upper troposphere, binary nucleation is fairly insensitive to the mechanism differences, with both yielding rates that exceed 1 particle cm-3 s-1 in the upper tropics. These large upper tropospheric nucleation rates imply that the DMS cycle may have served as an important source of aerosols to the troposphere and stratosphere during preindustrial and volcanically-quiescent periods, or during modern periods in clean marine regions where anthropogenic SO2 and H2SO4 are relatively low.
Lucas Donald D.
Prinn Ronald G.
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