Abstract.The reaction CH 3 C(O)O 2 + HO 2 → CH 3 C(O)OOH + O 2 (Reaction R5a), CH 3 C(O)OH + O 3 (Reaction R5b), CH 3 + CO 2 + OH + O 2 (Reaction R5c) was studied in a series of experiments conducted at 1000 mbar and (293 ± 2) K in the HIRAC simulation chamber. For the first time, products, (CH 3 C(O)OOH, CH 3 C(O)OH, O 3 and OH) from all three branching pathways of the reaction have been detected directly and simultaneously. Measurements of radical precursors (CH 3 OH, CH 3 CHO), HO 2 and some secondary products HCHO and HCOOH further constrained the system. Fitting a comprehensive model to the experimental data, obtained over a range of conditions, determined the branching ratios α (R5a) = 0.37 ± 0.10, α (R5b) = 0.12 ± 0.04 and α (R5c) = 0.51 ± 0.12 (errors at 2σ level). Improved measurement/model agreement was achieved using k (R5) = (2.4 ± 0.4) × 10 −11 cm 3 molecule −1 s −1 , which is within the large uncertainty of the current IUPAC and JPL recommended rate coefficients for the title reaction. The rate coefficient and branching ratios are in good agreement with a recent study performed by Groß et al. (2014b); taken together, these two studies show that the rate of OH regeneration through Reaction (R5) is more rapid than previously thought. GEOS-Chem has been used to assess the implications of the revised rate coefficients and branching ratios; the modelling shows an enhancement of up to 5 % in OH concentrations in tropical rainforest areas and increases of up to 10 % at altitudes of 6-8 km above the equator, compared to calculations based on the IUPAC recommended rate coefficient and yield. The enhanced rate of acetylperoxy consumption significantly reduces PAN in remote regions (up to 30 %) with commensurate reductions in background NO x .