Hydrogen peroxide (H
2O
2) is believed to be the primary species that oxidizes atmospheric sulfur (IV)to sulfur (VI) in cloud and rain droplets. Until now only a few measurements of atmospheric H
2O
2 have been performed in Japan. We measured atmospheric and rainwater H
2O
2 in the Hiroshima city, urban area, and the Higashi-Hiroshima city, semi-rural area, in western Japan and compared the difference of H
2O
2 concentrations between both areas. Concentration of atmospheric H
2O
2 measured was in a rang e of 0-3 ppbv and there were diurnal and seasonal variations of the H
2O
2 levels. During the day time, maximum concentration of atmospheric H
2O
2 in Hiroshima was about twice as high as that in HigashiHiroshima. H
2O
2 concentrations in rainwater (0.1-77.5 μM) as well as dissolved inorganic anions were at high levels in initial precipitations (first 15 min) and decreased gradually with precipitation. Summer rain contained high levels of H
2O
2. Gas phase H
2O
2 measured in combustion gases of an incinerator and an automobile was 2.90 and 0.31 ppbv (on average), respectively. With using these values, we estimate that the annual flux of gas phase H
2O
2 from all the stationary combustion sources and automobiles is 2.8×10
4 and 2.4×10
5 g H
2O
2, respectively in the Hiroshima area and 5.1×10
3 and 2.9×10
4 g H
2O
2, respectively in the Higashi-Hiroshima area. Our results strongly suggest the importance of stationary combustion facilities and automobile as sources of atmospheric H
2O
2 in urban area.
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