Global tropospheric hydroxyl distribution, budget and reactivity

The self-cleaning or oxidation capacity of the atmosphere is principally controlled by hydroxyl (OH) radicals in 5 the troposphere. Hydroxyl has primary (P) and secondary (S) sources, the former mainly through the photo-dissociation of ozone, the latter through OH recycling in radical reaction chains. We used the recent Mainz Organics Mechanism (MOM) to advance volatile organic carbon (VOC) chemistry in the general circulation model EMAC, and show that S is larger than previously assumed. By including emissions of a large number of primary VOC, and accounting for their complete breakdown and intermediate products, MOM is mass conserving, and calculates substantially higher OH reactivity from 10 VOC oxidation compared to predecessor models. Whereas previously P and S were found to be of similar magnitude, the present work indicates that S may be twice as large, mostly due to OH recycling in the free troposphere. Further, we find that nighttime OH formation may be significant in the polluted subtropical boundary layer in summer. With a mean OH recycling probability of about 67%, global OH is buffered and not sensitive to perturbations by natural or anthropogenic emission changes. Complementary primary and secondary OH formation mechanisms in pristine and polluted environments in the 15 continental and marine troposphere, connected through long-range transport of O3, maintain stable global OH levels.