This study examined the variability of near-surface (850 hPa) ozone during summer in East Asia using simulations from 12 models participating in the Chemistry-Climate Model Initiative (CCMI). The empirical orthogonal function (EOF) analysis of non-detrended ozone shows that the first (second) EOF mode is characterized by a monopole (dipole) structure that describe 83.3% (7.1%) of total variance. The corresponding the first principle component (PC1) time series exhibits a gradually increasing trend due to the rising anthropogenic emission, whereas PC2 shows interannual variation. To understand the drivers of this interannual variability, the detrended ozone is also analyzed. The two leading EOF patterns of detrended ozone, EOF1 and EOF2, explain 37.0% and 29.2% of the total variance, respectively. The regression results indicate that the positive ozone anomaly in East Asia associated with EOF1 is caused by the combination of net ozone production and transport from the upper atmosphere. In contrast, EOF2 is associated with the weakened western Pacific subtropical high during the La Niña decaying summer, which tends to decrease monsoon precipitation, thus increasing ozone concentration in China. Our results suggest that the El Niño-Southern Oscillation (ENSO) plays a key role in driving interannual variability in tropospheric ozone in East Asia.Atmosphere 2020, 11, 206 2 of 17 in areas where ozone is not generally produced [8]. Ozone is more prevalent at higher altitudes in the troposphere of the mid-latitudes. Therefore, downward motion leads to more surface ozone by the transport of higher ozone air from the upper troposphere. In addition, when stratospheric ozone flows directly into the troposphere because of tropopause folding or the development of a strong low-pressure system, the concentration of ozone also increases in the upper-middle troposphere [15,16]. The interannual variability such as the East Asian monsoon and El Niño-Southern Oscillation (ENSO) can also result in the redistribution of tropospheric ozone [9][10][11]17,18]. For example, the tropical Pacific ozone concentration varies with the location and intensity of the anomalous vertical motions associated with the Walker circulation that is closely tied to ENSO [19][20][21]. Note that if the various factors affecting ozone concentration act in combination, the characteristics of ozone variation will differ significantly from region to region.East Asia has recently undergone a strong trend of increasing ozone [8], which can be associated with the increase in ozone precursor emissions [22,23]. The East Asia is dominated by southerly winds originating from the western North Pacific Ocean during the boreal summer that affect both climate [24] and air quality [17]. Inland regions that are far from the ocean are subjected to active ozone production under strong solar radiation, and because of the increase in excited oxygen atoms (O 1 D) that catalytically destroy ozone [25], the moistened air coming from the ocean results in a decrease of ozone. This may...