“…The increase in O 3 concentration increased the oxidation capacity of the atmosphere and thus enhanced the formation of secondary organic/inorganic aerosols, which has been suggested by previous studies based on numerical modelling and observation data (e.g., Chan et al, 2017 ; Wang et al, 2016 ; Huang et al, 2020 ; Kang et al, 2021 ; Le et al, 2020 ; Li et al, 2021 ). The secondary formed inorganic aerosols and most of the organic aerosols were efficient in scattering and inefficient in absorbing the solar radiation, leading to higher SSA of the total atmospheric aerosols ( Deng et al, 2016 ; Wang et al, 2021 ). In turn, aerosols with higher SSA relatively absorbed less while scattered more solar radiation, which promoted the formation of O 3 ( Liu et al, 2019 ; Ma et al, 2021a ).…”