Articles | Volume 18, issue 24
https://doi.org/10.5194/acp-18-17945-2018
https://doi.org/10.5194/acp-18-17945-2018
Research article
 | 
18 Dec 2018
Research article |  | 18 Dec 2018

Characterization of ozone deposition to a mixed oak–hornbeam forest – flux measurements at five levels above and inside the canopy and their interactions with nitric oxide

Angelo Finco, Mhairi Coyle, Eiko Nemitz, Riccardo Marzuoli, Maria Chiesa, Benjamin Loubet, Silvano Fares, Eugenio Diaz-Pines, Rainer Gasche, and Giacomo Gerosa

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AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Giacomo Alessandro Gerosa on behalf of the Authors (08 Aug 2018)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (09 Aug 2018) by Alex B. Guenther
RR by Anonymous Referee #1 (16 Aug 2018)
RR by Anonymous Referee #2 (27 Aug 2018)
ED: Reconsider after major revisions (06 Sep 2018) by Alex B. Guenther
AR by Giacomo Alessandro Gerosa on behalf of the Authors (16 Oct 2018)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (22 Oct 2018) by Alex B. Guenther
RR by Anonymous Referee #1 (31 Oct 2018)
ED: Publish subject to minor revisions (review by editor) (13 Nov 2018) by Alex B. Guenther
AR by Giacomo Alessandro Gerosa on behalf of the Authors (21 Nov 2018)  Author's response    Manuscript
ED: Publish subject to technical corrections (02 Dec 2018) by Alex B. Guenther
AR by Giacomo Alessandro Gerosa on behalf of the Authors (05 Dec 2018)  Author's response    Manuscript
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Short summary
A 1-month field campaign of ozone (O3) flux measurements along a five-level vertical profile of a mature broadleaf forest highlighted that the biosphere–atmosphere exchange of this pollutant is modulated by complex diel dynamics occurring within and below the canopy. The canopy removed nearly 80 % of the O3 deposited to the forest; only a minor part was removed by the soil and the understorey (2 %), while the remaining 18.2 % was removed by chemical reactions with NO mostly emitted from soil.
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