Observations of total RONO₂ over the boreal forest: NOx sinks and HNO₃ sources

In contrast with the textbook view of remote chemistry where HNO₃ formation is the primary sink of nitrogen oxides, recent theoretical analyses show that formation of RONO₂ (ΣANs) from isoprene and other terpene precursors is the primary net chemical loss of nitrogen oxides over the remote continents where the concentration of nitrogen oxides is low. This then increases the prominence of questions concerning the chemical lifetime and ultimate fate of ΣANs.

We present observations of nitrogen oxides and organic molecules collected over the Canadian boreal forest during the summer which show that ΣANs account for ~20% of total oxidized nitrogen and that their instantaneous production rate is larger than that of HNO₃. This confirms the primary role of reactions producing ΣANs as a control over the lifetime of NOx (NOx = NO + NO₂) in remote, continental environments. However, HNO₃ is generally present in larger concentrations than ΣANs indicating that the atmospheric lifetime of ΣANs is shorter than the HNO₃ lifetime.