The potential role of the reaction between the acetyl peroxy radicals (CH 3 C(O)O 2 ) and the hydroxyl radical in the atmosphere was investigated. Theoretical calculations show that this reaction would form acetic acid (AAc) and 1 O 2 almost exclusively. The reaction proceeds by formation of a trioxide compound as CH 3 C(O)OOOH, in which rapid intramolecular hydrogen atom transfer followed by decomposition to AAc and 1 O 2 was found, while decomposition of the trioxide to CH 3 CO 2 + HO 2 is negligible. With the relatively fast reaction between CH 3 C(O)O 2 and OH with an estimated rate coefficient of 1.8 × 10 −10 cm 3 molecule −1 s −1 , the reaction might be a significant secondary source of AAc in the troposphere. A global atmospheric simulation using GEOS-Chem found that the title reaction results in an average increase of the mixing ratios of AAc by ∼33% (about 6.4 pptv for increase) and a net formation of about 8.0 Tg/yr AAc. Reactions between other RC(O)O 2 and OH may also contribute significantly to the formation of RC(O)OH. The atmospheric chemistry model may need to include the title reaction.