Measurement report: Photochemical production and loss rates of formaldehyde and ozone across Europe
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Published:2021-12-17
Issue:24
Volume:21
Page:18413-18432
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ISSN:1680-7324
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Container-title:Atmospheric Chemistry and Physics
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language:en
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Short-container-title:Atmos. Chem. Phys.
Author:
Nussbaumer Clara M.ORCID, Crowley John N.ORCID, Schuladen Jan, Williams Jonathan, Hafermann Sascha, Reiffs Andreas, Axinte Raoul, Harder HartwigORCID, Ernest Cheryl, Novelli AnnaORCID, Sala Katrin, Martinez Monica, Mallik Chinmay, Tomsche Laura, Plass-Dülmer Christian, Bohn BirgerORCID, Lelieveld JosORCID, Fischer Horst
Abstract
Abstract. 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.
Publisher
Copernicus GmbH
Subject
Atmospheric Science
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