Oxidation processes in the eastern Mediterranean atmosphere: evidence from the modelling of HO<sub><i>x</i></sub> measurements over Cyprus

<p>The Mediterranean is a climatically sensitive region located at the crossroads of air masses from three continents: Europe, Africa, and Asia. The chemical processing of air masses over this region has implications not only for the air quality but also for the long-range transport of air...

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Main Authors: C. Mallik, L. Tomsche, E. Bourtsoukidis, J. N. Crowley, B. Derstroff, H. Fischer, S. Hafermann, I. Hüser, U. Javed, S. Keßel, J. Lelieveld, M. Martinez, H. Meusel, A. Novelli, G. J. Phillips, A. Pozzer, A. Reiffs, R. Sander, D. Taraborrelli, C. Sauvage, J. Schuladen, H. Su, J. Williams, H. Harder
Format: Article
Language:English
Published: Copernicus Publications 2018-07-01
Series:Atmospheric Chemistry and Physics
Online Access:https://www.atmos-chem-phys.net/18/10825/2018/acp-18-10825-2018.pdf
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Summary:<p>The Mediterranean is a climatically sensitive region located at the crossroads of air masses from three continents: Europe, Africa, and Asia. The chemical processing of air masses over this region has implications not only for the air quality but also for the long-range transport of air pollution. To obtain a comprehensive understanding of oxidation processes over the Mediterranean, atmospheric concentrations of the hydroxyl radical (OH) and the hydroperoxyl radical (HO<sub>2</sub>) were measured during an intensive field campaign (CYprus PHotochemistry EXperiment, CYPHEX-2014) in the northwest of Cyprus in the summer of 2014. Very low local anthropogenic and biogenic emissions around the measurement location provided a vantage point to study the contrasts in atmospheric oxidation pathways under highly processed marine air masses and those influenced by relatively fresh emissions from mainland Europe.</p><p>The CYPHEX measurements were used to evaluate OH and HO<sub>2</sub> simulations using a photochemical box model (CAABA/MECCA) constrained with CYPHEX observations of O<sub>3</sub>, CO, NO<sub><i>x</i></sub>, hydrocarbons, peroxides, and other major HO<sub><i>x</i></sub> (OH&thinsp;+&thinsp;HO<sub>2</sub>) sources and sinks in a low-NO<sub><i>x</i></sub> environment (&lt;&thinsp;100&thinsp;pptv of NO). The model simulations for OH agreed to within 10&thinsp;% with in situ OH observations. Model simulations for HO<sub>2</sub> agreed to within 17&thinsp;% of the in situ observations. However, the model strongly under-predicted HO<sub>2</sub> at high terpene concentrations, this under-prediction reaching up to 38&thinsp;% at the highest terpene levels. Different schemes to improve the agreement between observed and modelled HO<sub>2</sub>, including changing the rate coefficients for the reactions of terpene-generated peroxy radicals (RO<sub>2</sub>) with NO and HO<sub>2</sub> as well as the autoxidation of terpene-generated RO<sub>2</sub> species, are explored in this work. The main source of OH in Cyprus was its primary production from O<sub>3</sub> photolysis during the day and HONO photolysis during early morning. Recycling contributed about one-third of the total OH production, and the maximum recycling efficiency was about 0.7. CO, which was the largest OH sink, was also the largest HO<sub>2</sub> source. The lowest HO<sub><i>x</i></sub> production and losses occurred when the air masses had higher residence time over the oceans.</p>
ISSN:1680-7316
1680-7324