Abstract. The relative contributions of various source regions to the long-term increasing trend in surface ozone (O 3 ) over Japan were estimated by a series of tracer-tagging simulations using a global chemical transport model. The model simulated the observed increasing trend in surface O 3 , including its seasonal variation and geographical features, in Japan well and demonstrated the relative roles of different source regions in forming this trend. Most of the increasing trend in surface O 3 over Japan (∼ 97 %) that was simulated was explained as the sum of trends in contributions of different regions to photochemical O 3 production. The increasing trend in O 3 produced in China accounted for 36 % of the total increasing trend and those in the other northeast Asian regions (the Korean Peninsula, coastal regions in East Asia, and Japan) each accounted for about 12-15 %. Furthermore, the contributions of O 3 created in the entire free troposphere and in western, southern, and southeastern Asian regions also increased, and their increasing trends accounted for 16 and 7 % of the total trend, respectively. The impact of interannual variations in climate, in methane concentration, and in emission of O 3 precursors from different source regions on the relative contributions of O 3 created in each region estimated above was also investigated. The variation of climate and the increase in methane concentration together caused the increase of photochemical O 3 production in several regions, and represented about 19 % of the total increasing trend in surface O 3 over Japan. The increase in emission of O 3 precursors in China caused an increase of photochemical O 3 production not only in China itself but also in the other northeast Asian regions and accounted for about 46 % of the total increase in surface O 3 over Japan. Similarly, the relative impact of O 3 precursor emission changes in the Korean Peninsula and Japan were estimated as about 16 and 4 % of the total increasing trend, respectively. The O 3 precursor emission change in regions other than northeast Asia caused increases in surface O 3 over Japan mainly through increasing photochemical O 3 production in western, southern, and southeast Asia and the free troposphere and accounted for about 16 % of the total.