The Long-Range Atmospheric Transport of Natural and Contaminant Substances 1990
DOI: 10.1007/978-94-009-0503-0_5
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The Intercontinental Transport of Sulfur and Nitrogen

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Cited by 6 publications
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“…A high aerosol NRB signal is apparent in Figure 5 around 0.5 km MSL. The estimated residence time for SO 2 is less than 50 h in this region in the boundary layer [Galloway, 1990], and the heterogeneous conversion rate of SO 2 to sulfate is 2.0% h −1 [Takami et al, 2007]. In this case, air pollutants spent a relatively long time aloft and were well oxidized [Takami et al, 2007].…”
Section: Regional Impact Of Case C In Downwind Areasmentioning
confidence: 82%
“…A high aerosol NRB signal is apparent in Figure 5 around 0.5 km MSL. The estimated residence time for SO 2 is less than 50 h in this region in the boundary layer [Galloway, 1990], and the heterogeneous conversion rate of SO 2 to sulfate is 2.0% h −1 [Takami et al, 2007]. In this case, air pollutants spent a relatively long time aloft and were well oxidized [Takami et al, 2007].…”
Section: Regional Impact Of Case C In Downwind Areasmentioning
confidence: 82%