<p><strong>Abstract.</strong> The radical terminating, termolecular reaction between OH and NO<sub>2</sub> exerts great influence on the NO<sub><i>y</i></sub>&#8201;/&#8201;NO<sub><i>x</i></sub> ratio and O<sub>3</sub> formation in the atmosphere. Evaluation panels (IUPAC and NASA) recommend rate coefficients for this reaction that disagree by as much as a factor 1.6 at low temperature and pressure. In this work, the title reaction was studied by pulsed laser photolysis-laser induced fluorescence over the pressure range 16&#8211;1200&#8201;mbar and temperature 217&#8211;333&#8201;K in N<sub>2</sub> bath-gas, with experiments at 295&#8201;K (67&#8211;333&#8201;mbar) for O<sub>2</sub>. In-situ measurement of NO<sub>2</sub> using two optical-absorption set-ups enabled generation of highly precise, accurate rate coefficients in the fall-off pressure range, appropriate for atmospheric conditions. We found, in agreement with previous work, that O<sub>2</sub> bath-gas has a lower collision efficiency than N<sub>2</sub> with a relative collision efficiency to N<sub>2</sub> of 0.74. Using the widely used Troe-type formulation for termolecular reactions we present a new set of parameters with <i>k</i><sub>0</sub>(N<sub>2</sub>)&#8201;=&#8201;2.6&#8201;&#215;&#8201;10<sup>&#8722;30</sup>&#8201;cm<sup>6</sup>&#8201;molecule<sup>&#8722;2</sup>&#8201;s<sup>&#8722;1</sup>, <i>k</i><sub>0</sub>(O<sub>2</sub>)&#8201;=&#8201;2.0&#8201;&#215;&#8201;10<sup>&#8722;30</sup>&#8201;cm<sup>6</sup>&#8201;molecule<sup>&#8722;2</sup>&#8201;s<sup>&#8722;1</sup>, <i>m</i>&#8201;=&#8201;3.6, <i>k</i><sub>&#8734;</sub>&#8201;=&#8201;6.3&#8201;&#215;&#8201;10<sup>&#8722;11</sup>&#8201;cm<sup>3</sup>&#8201;molecule<sup>&#8722;1</sup>&#8201;s<sup>&#8722;1</sup>, <i>F</i><sub>c</sub>&#8201;=&#8201;0.39 and compare our results to previous studies in N<sub>2</sub> and O<sub>2</sub> bath-gases.</p>