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By Andrzej G. Chmielewski (Ed.)

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2009). Fig. 11. Spatial distributions of the differences in the gas phase fraction of nitrate (%) (left panels) and total (dry + wet) deposition of nitrate (μg m-2 mon-1) (right panels). The upper and lower panels show the results for (Sh – CNTRL) and the (S2NHh – CNTRL) runs, respectively. As a result of future SO2 emission decreases, less secondary acidification should occur. However, a decrease in nitrate deposition downwind will also mean that t-NO3 will be transported longer distances, which may result in increased deposition of t-NO3 in regions further downwind.

Borrego, E. Renner, Elsevier, ISBN:978-0-444-52987-9, pp. ; Ueda, H. ; Satsumabayashi, H ; & An, J. (2004). Impacts of the eruption of Miyakejima Volcano on air quality over far east Asia. J. Geophys. , Vol. ; Ueda, H. ; Satsumabayashi, H ; & Han, Z. (2005). Increase in nitrate and chloride deposition in east Asia due to increased sulfate associated with the eruption of Miyakejima Volcano. J. Geophys. , Vol. 1029/2005JD005879 Kajino, M ; Ueda, H. & Nakayama, S. (2008). Secondary acidification : Changes in gasaerosol partitioning of semivolatile nitric acid and enhancement of its deposition due to increased emission and concentration of SOx.

Introduction The air pollution caused by exhaust gases from automobiles has become a critical issue. In some regions, fossil fuel combustion is a problem as well. The principal gases that cause air pollution from automobiles are nitrogen oxides, NOx (NO and NO2), and carbon monoxide (CO). Because NOx gases with sulfur oxides (SOx) emitted from coal fired plants cause acid rain and global warming and produce ozone (O3) that leads to serious metropolitan smog from photochemical reaction, they must be detected and reduced [1-5].

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