We have investigated the dynamics and formation mechanisms of the episodic pollution of photochemical ozone (O
3) during 8-9 May 2007 over Japan using hourly air quality data observed at monitoring stations in the whole Japan and a chemical transport model (CTM) in East Asia.
Observed O
3 concentrations at monitoring stations over Japan began to grow up in north Kyushu area around 900 JST on 8 May, and reached over 120ppbv in north Kyushu area, including isolated islands such as 116 and Gotou, and the west part of Chugoku area at 1500 JST. In night on 8 May, O
3 concentration fall down, but a part of stations in western part of Japan continued to keep the O
3 level over 120ppbv. On next day (9 May), O
3 concentrations are higher than those on previous day at 900 JST and then grew up over the wide area in Japanese Island excluding Hokkaido and the north part of Tohoku area. At 1500 JST, the high O
3 concentrations over 120ppbv were observed at lots of stations over the wide area in Japan: the surrounding areas of megacities (Tokyo, Nagoya, and Osaka) and Hokuriku (Toyarna and Niigata prefectures) and Setouchi areas.
CTM can reproduce the temporal variations of observed O
3 concentrations at monitoring stations during 8-9 May, but underestimates the peak O
3. This underestimation tends to be improved as increasing of emissions in north and central coastal areas of China. Modeled spatial distributions of surface O
3 during 7-9 May showed that a polluted air mass (O
3> 80ppbv) having a spatial scale over 500km was transported from the north coastal area of China to Japanese Island by the westerly strong wind at the northern part of moving high pressure system over the East China Sea. High concentrations of O
3 observed in Japan during 8-9 May were influenced by the transboundary air pollution of the photochemically produced O
3 by precursor gases emitted from China and Korea. Averaged contribution of Chinese emissions to surface O
3 during the high O
3 concentration (O
3> 80ppbv) in the same period is estimated to be over 25% throughout Japan excluding the northern part of Japan and to be 40-45% in Kyushu area. However, it should be noted that the model may fail to estimate the contribution of trasnboundary pollution in surrounding areas of megacities because the model doesn't have the capability to reproduce well the detail of urban air pollution. Finally, the modeled results and the observations of monitoring stations and Lidar shows that SO
2 gas and anthropogenic aerosols as well as O
3 are transported from Asian continent within a mixed layer below 1500m altitude.
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