Nitrites (NO 2 - /HONO), as the primary source of hydroxyl radicals ( • OH) in the atmosphere, play a key role in atmospheric chemistry. However, the current understanding of the source of NO 2 - /HONO is insufficient and therefore hinders the accurate quantification of atmospheric oxidation capacity. Herein, we highlighted an overlooked HONO source by the reaction between nitrophenols (NPs) and • OH in the aqueous phase and provided kinetic data to better evaluate the contribution of this process to atmospheric HONO. Three typical NPs, including 4-nitrophenol (4NP), 2-nitrophenol (2NP), and 4-nitrocatechol (4NC), underwent a denitration process to form aqueous NO 2 - and gaseous HONO through the • OH oxidation, with the yield of NO 2 - /HONO varied from 15.0 to 33.5%. According to chemical composition and structure analysis, the reaction pathway, where the ipso addition of • OH to the NO 2 group on 4NP generated hydroquinone, can contribute to more than 61.9% of the NO 2 - /HONO formation. The aqueous photooxidation of NPs may account for HONO in the atmosphere, depending on the specific conditions. The results clearly suggest that the photooxidation of NPs should be considered in the field observation and calculation to better evaluate the HONO budget in the atmosphere.