h i g h l i g h t sThe formation of ROOH from RO 2 and HO 2 is significant under NO x -limited conditions. The global burden of ROOH is found to be 3.8 Tg. ROOH peak near the equator having higher photochemistry and large VOC emissions. HO x recycling caused significant increases in ROOH over tropical forested regions.
a b s t r a c tThe global 3-D chemistry-transport model, STOCHEM-CRI (Utembe et al., 2010), has been used to simulate the global distribution of organic hydroperoxides (ROOH) for both present day and pre-industrial scenarios. Globally, the formation of ROOH is solely from the reaction between RO 2 and HO 2 , being more significant under NO x -limited conditions; here the self and cross reactions of RO 2 and HO 2 radicals dominate over their reaction with NO. The predominant global loss processes for ROOH are reaction with OH (95%) and by photolysis (4.4%) with a minor loss (<1%) by deposition, in the present day scenario. The associated global burden of ROOH in our model study is found to be 3.8 Tg. The surface distribution of ROOH shows a peak near the equator corresponding with higher photochemical activity and large (biogenic) VOC emissions. The simulated abundances of ROOH are comparable with those recorded in field campaigns, but generally show a tendency towards underestimation, particularly in the boundary layer. ROOH displayed seasonal cycles with higher concentrations during the summer months and lower concentrations during the winter months. The effects of including proposed HO x recycling schemes, including isomerisation of isoprenederived peroxy radicals on the global budget of ROOH have also been investigated for the present and the pre-industrial environment. The present day simulations showed significant increases in CH 3 OOH and ROOH (up to 80% and 30%, respectively) over tropical forested regions, due to a general increase in HO 2 and RO 2 levels in isoprene-rich regions at low NO x levels. In the pre-industrial scenario, the increases in CH 3 OOH and total ROOH abundances are even larger, reflecting the more efficient operation of HO x recycling mechanisms at lower NO x levels. RCO 3 H species contribute 40e50% of the global burden of ROOH; inclusion of HO x recycling mechanisms leads to an increase in these RCO 3 H species but there is no discernible change in the remaining ROOH (ROOHeRCO 3 H) burden.