Tropospheric ozone (O 3) is an important trace gas in the ambient air. The photolysis of O 3 in the troposphere provides an important primary source of the hydroxyl radical (OH), which initiates the chemical oxidation cycle (Lelieveld et al., 2008). Tropospheric O 3 serves as an important greenhouse gas that contributes to global warming (IPCC, 2013; Monks et al., 2015), and long-term exposure to high concentrations of surface O 3 is harmful to human health and vegetation (Fuhrer, 2009). Surface O 3 pollution has become a major environmental concern in China in recent decades (Wang, Xue, et al., 2017; and references therein; Xue, Wang, Gao, et al., 2014), and the increasing trends shown in several long-term studies provide evidence that the situation is worsening (