Brown carbon (BrC) is a crucial light-absorption
component in the
atmosphere, playing a profound role in the radiation budget. Variations
in the light-absorption properties and molecular composition of BrC
due to atmospheric photochemical aging process have not been well
constrained, leading to high uncertainty in evaluating its global
radiative effect. The molecular composition of atmospheric BrC were
investigated to stress the BrC photobleaching in this work. In total,
896 organic compounds were identified, which accounted for 2.5%–26.1%
of organic aerosol in mass concentration. We found that solar radiation
led to the declined mass absorption coefficient at 375 nm (MAC375), indicating BrC photobleaching, coinciding with an elevated
mass fraction of carboxylic acids (CAs). This phenomenon was more
pronounced under higher-energy solar radiation. Specifically, the
mass fraction of nitrocarboxylic acids (NCAs) in CAs increased during
BrC photobleaching, which was potentially caused by the oxidation
of nitrophenols, resulting in an ∼83.3% decrease in MAC375. Our findings provide direct observational evidence of
BrC photobleaching from a molecular-level perspective and elucidate
a potential BrC photobleaching pathway in the urban atmosphere.