Chemical processes related to net ozone tendencies in the free troposphere

Bozem, Heiko; Butler, Tim M.; Lawrence, Mark G.; Harder, Hartwig; Martinez, Monica; Kubistin, Dagmar; Lelieveld, Jos; Fischer, Horst

doi:https://doi.org/10.5194/acp-17-10565-2017

Articles | Volume 17, issue 17

https://doi.org/10.5194/acp-17-10565-2017

© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

https://doi.org/10.5194/acp-17-10565-2017

© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Articles | Volume 17, issue 17

Research article

|

08 Sep 2017

Research article |

| 08 Sep 2017

Chemical processes related to net ozone tendencies in the free troposphere

Heiko Bozem, Tim M. Butler, Mark G. Lawrence, Hartwig Harder, Monica Martinez, Dagmar Kubistin, Jos Lelieveld, and Horst Fischer

Download

Final revised paper (published on 08 Sep 2017)
Preprint (discussion started on 24 Feb 2017)

Interactive discussion

Status: closed

AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment

- Printer-friendly version

- Supplement

RC1: 'Reviewer comments', Anonymous Referee #1, 22 Mar 2017
- AC1: 'Answer to Referee #!', Heiko Bozem, 06 Jun 2017
RC2: 'Review of “Chemical processes related to net ozone tendencies in the free troposphere” by Bozem et al.', Anonymous Referee #2, 20 Apr 2017
- AC2: 'Answer to Referee #2', Heiko Bozem, 06 Jun 2017

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision

AR by Heiko Bozem on behalf of the Authors (05 Jul 2017) Author's response Manuscript

ED: Publish as is (17 Jul 2017) by Dwayne Heard

AR by Heiko Bozem on behalf of the Authors (04 Aug 2017)

Short summary

We present airborne measurements and model simulations in the tropics and mid-latitudes during GABRIEL and HOOVER, respectively. Based only on in situ data net ozone formation/destruction tendencies (NOPR) are calculated and compared to a 3-D chemistry transport model. The NOPR is positive in the continental boundary layer and the upper troposphere above 6 km. In the marine boundary layer and the middle troposphere ozone destruction prevails. Fresh convection shows strong net ozone formation.