The effect of water vapour on the rate coefficient for the atmospherically important, termolecular reaction between OH and NO2 was determined in He-H2O (277, 291 and 332 K) and N2-H2O bath gases (292 K). Combining pulsed laser photolytic generation of OH and its detection by laser induced fluorescence (PLP-LIF) with in-situ, optical measurement of both NO2 and H2O we were able to show that (in contrast to previous investigations) the presence of H2O increases the rate 10 coefficient significantly. We derive a rate coefficient for H2O bath gas at the low-pressure limit ( 0 H2O ) of 15.9 × 10 -30 cm 6 molecue -2 s -1 . This indicates that H2O is a more efficient collisional quencher (by a factor of ≈ 6) of the initially formed HO-NO2 association complex than N2 and a factor ≈ 8 more efficient than O2. Ignoring the effect of water-vapour will lead to an underestimation of the rate coefficient by up to 15% e.g. in the tropical boundary layer. Combining the new experimental results from this study with those from the companion paper in which we report rate coefficients obtained in N2 and O2 bath 15 gases (Amedro et al., 2019) we derive a new parameterisation for atmospheric modelling of the OH + NO2 reaction and use this in a chemical transport model (EMAC) to examine the impact of the new data on the global distribution of NO2, HNO3 and OH. Use of the new parameters (rather than those given in the IUPAC and NASA evaluations) result in significant changes in the HNO3 / NO2 ratio and NOx concentrations, the sign of which depends on which evaluation is used as reference. The model predicts the presence of HOONO (formed along with HNO3 in the title reaction) in concentrations similar to those of 20 HO2NO2 at the tropical tropopause.Reaction (R1) converts NO2 to nitric acid (HNO3) and peroxynitrous acid (HOONO), and its rate strongly influences the relative abundance of atmospheric NOx (NO2 + NO) and longer-lived "reservoirs" of NOx which include e.g. HNO3 and organic nitrates. It also converts OH (the main initiator of atmospheric oxidation) to a long-lived reservoir, HNO3. As the abundance of OH and NOx directly impact on photochemical ozone formation and the lifetimes of greenhouse gases, reaction (R1) may 30 be considered one of the most important gas-phase processes in atmospheric science (Newsome and Evans, 2017). As outlined by Amedro et al. (2019), the rate coefficients and product-branching for this reaction are dependent on pressure and temperature and also on the bath-gas identity, i.e. the identity of the collision partner, M in reaction (R1). The per collision efficiency of energy transfer from the initially "hot" association complex to bath gas can vary considerably, with more complex bath gases molecules possessing more degrees of freedom and bonds with similar vibrational frequencies to those in the 35 association complex being generally more efficient. In this sense, we may expect H2O to be better than N2 or O2 in quenching [HO-NO2] # .In this second part of our study of the reaction between OH and NO2, w...