Measurement report: Photochemical production and loss rates of formaldehyde and ozone across Europe

• Published in: Atmospheric chemistry and physics 2021-12, Vol.21 (24), p.18413-18432
• Main Authors: Nussbaumer, Clara M, Crowley, John N, Schuladen, Jan, Williams, Jonathan, Hafermann, Sascha, Reiffs, Andreas, Axinte, Raoul, Harder, Hartwig, Ernest, Cheryl, Novelli, Anna, Sala, Katrin, Martinez, Monica, Mallik, Chinmay, Tomsche, Laura, Plass-Dülmer, Christian, Bohn, Birger, Lelieveld, Jos, Fischer, Horst
• Format: Article
• Language: English
• Subjects: Acetaldehyde; Air pollution; Atmospheric chemistry; Budgets; Chemistry; Dry deposition; Emissions; Environmental aspects; Experiments; Formaldehyde; Gases; Isoprene; Mathematical analysis; Measurement; Methane; Mountains; Nitrogen compounds; Nitrogen dioxide; Nitrogen oxide; Nitrogen oxides; Organic compounds; Oxidation; Ozone; Ozone chemistry; Ozone production; Photochemicals; Photochemistry; Photolysis; Simulation; Trace gases; VOCs; Volatile organic compounds
• ISSN: 1680-7324; 1680-7316; 1680-7324
• DOI: 10.5194/acp-21-18413-2021

Various atmospheric sources and sinks regulate the abundance of tropospheric formaldehyde (HCHO), which is an important trace gas impacting the HOx (≡ HO2 + OH) budget and the concentration of ozone (O3). In this study, we present the formation and destruction terms of ambient HCHO and O3 calculated from in situ observations of various atmospheric trace gases measured at three different sites across Europe during summertime. These include a coastal site in Cyprus, in the scope of the Cyprus Photochemistry Experiment (CYPHEX) in 2014, a mountain site in southern Germany, as part of the Hohenpeißenberg Photochemistry Experiment (HOPE) in 2012, and a forested site in Finland, where measurements were performed during the Hyytiälä United Measurements of Photochemistry and Particles (HUMPPA) campaign in 2010. We show that, at all three sites, formaldehyde production from the OH oxidation of methane (CH4), acetaldehyde (CH3CHO), isoprene (C5H8) and methanol (CH3OH) can almost completely balance the observed loss via photolysis, OH oxidation and dry deposition. Ozone chemistry is clearly controlled by nitrogen oxides (NOx ≡ NO + NO2) that include O3 production from NO2 photolysis and O3 loss via the reaction with NO. Finally, we use the HCHO budget calculations to determine whether net ozone production is limited by the availability of VOCs (volatile organic compounds; VOC-limited regime) or NOx (NOx-limited regime). At the mountain site in Germany, O3 production is VOC limited, whereas it is NOx limited at the coastal site in Cyprus. The forested site in Finland is in the transition regime.