The atmospheric oxidation mechanism and energetics of propanesulfinic acid (CH 3 CH 2 CH 2 S(O)OH, PSIA) initiated by OH radicals have been investigated at the CCSD(T)/aug-cc-pVTZ// M06-2X/aug-cc-pVTZ level of theory. The PSIA + • OH reaction proceeds through (i) H-atom abstraction and (ii) • OH addition pathways. The calculated energies indicate that the barrier height for the abstraction of H-atom from the −OH moiety of PSIA leading to the formation of CH 3 CH 2 CH 2 S(O) 2 + H 2 O is estimated to be −4.7 kcal mol −1 relative to that of the separated reactants. The rate coefficients were determined for all possible reaction paths by RRKM-ME calculations using Master equation solver for multienergy well reactions (Mesmer) code in the atmospherically relevant temperatures between 200 and 320 K and bath gas pressures between 0.1 and 10 atm. The calculated bimolecular rate coefficients suggest that the formation of CH 3 CH 2 CH 2 S(O) 2 + H 2 O is predominant compared to the other possible reaction paths in the studied temperature range. The total rate coefficient for the PSIA + • OH reaction was found to be ∼8.40 × 10 −11 cm 3 molecule −1 s −1 at T = 298 K and P = 1 atm. In addition, branching ratios, thermochemical parameters, atmospheric lifetime, and global warming potentials were determined. Overall, the results indicate that the atmospheric removal of PSIA with • OH results in the formation of sulfur dioxide (SO 2 ) from C−S single bond fission in the CH 3 −CH 2 −CH 2 − S(O) 2 radical, which is formed by H-atom abstraction from the OH group of PSIA. Thus, the SO 2 product does not originate from the direct elimination of SO 2 from unimolecular dissociation of PSIA. The formed SO 2 , propylene (C 3 H 6 ), sulfurous acid (H 2 SO 3 ), and hydroperoxyl (HO 2 ) radical are major products that may contribute to global warming and aerosol formation.