Articles | Volume 17, issue 2
Atmos. Chem. Phys., 17, 1361–1379, 2017
https://doi.org/10.5194/acp-17-1361-2017

Special issue: Interactions between climate change and the Cryosphere: SVALI,...

Atmos. Chem. Phys., 17, 1361–1379, 2017
https://doi.org/10.5194/acp-17-1361-2017

Research article 30 Jan 2017

Research article | 30 Jan 2017

Simulating ozone dry deposition at a boreal forest with a multi-layer canopy deposition model

Putian Zhou et al.

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Interactive discussion

Status: closed
Status: closed
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 Putian Zhou on behalf of the Authors (03 Nov 2016)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (23 Nov 2016) by Steffen M. Noe
RR by Anonymous Referee #1 (12 Dec 2016)
ED: Reconsider after minor revisions (Editor review) (16 Dec 2016) by Steffen M. Noe
AR by Putian Zhou on behalf of the Authors (28 Dec 2016)  Author's response    Manuscript
ED: Publish as is (03 Jan 2017) by Steffen M. Noe
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Short summary
We implemented a multi-layer O3 dry deposition model in a 1-D model SOSAA to simulate O3 flux and concentration within and above a boreal forest at SMEAR II in Hyytiälä, Finland, in August 2010. The results showed that when RH > 70 % the O3 uptake on leaf wet skin was ~ 51 % to the total deposition at night and ~ 19 % at daytime. The sub-canopy contribution below 4.2 m was ~ 38 % at daytime. The averaged daily chemical contribution to total O3 alteration inside the canopy was less than 10 %.
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