Fig. 5: Measured DMS (dimethyl sulfide) and SO2 data and the contribution of different pathways to H2SO4 formation. | Nature Communications

Fig. 5: Measured DMS (dimethyl sulfide) and SO2 data and the contribution of different pathways to H2SO4 formation.

From: Direct sulfuric acid formation from the gas-phase oxidation of reduced-sulfur compounds

Fig. 5

Source data are provided as a Source Data file. a Measured average DMS concentrations (colour coded) worldwide with corresponding SO2/DMS ratios (numbers), if available. The map plot was created with R68 using the ggplot2 package (map_data(“world”)). b Calculated H2SO4 formation rates from different pathways combining the modelled CH3S and CH3SO2 formation rates with experimentally determined H2SO4 yields. The “Cloud” scenario represents simulations with cloud passages leading to lower SO2 concentrations due to its uptake and oxidation in clouds. The simulations with “lower HA” represent model runs using lower Henry constants HA of DMS oxidation products (see Supplementary Table 1). c Reproduction of measured SO2 (black line with squares) and DMS (red line with dots) concentrations as well as its SO2/DMS ratio (blues crosses) from observations at Baring Head, New Zealand50. Purple and yellow bars illustrate the calculated relative contributions of DMS (direct route) and SO2 oxidation to total H2SO4 formation at daytime. The contributions are calculated based on results from “no Cloud” simulation.

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