Long-term change in the source contribution to surface ozone over Japan

Nagashima, Tatsuya; Sudo, Kengo; Akimoto, Hajime; Kurokawa, Junichi; Ohara, Toshimasa

doi:https://doi.org/10.5194/acp-17-8231-2017

Articles | Volume 17, issue 13

https://doi.org/10.5194/acp-17-8231-2017

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

https://doi.org/10.5194/acp-17-8231-2017

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

Articles | Volume 17, issue 13

Research article

|

07 Jul 2017

Research article |

| 07 Jul 2017

Long-term change in the source contribution to surface ozone over Japan

Tatsuya Nagashima, Kengo Sudo, Hajime Akimoto, Junichi Kurokawa, and Toshimasa Ohara

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Final revised paper (published on 07 Jul 2017)
Supplement to the final revised paper
Preprint (discussion started on 19 Jan 2017)
Supplement to the preprint

Interactive discussion

Status: closed

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

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- Supplement

RC1: 'Review of Nagashima et al', Anonymous Referee #1, 20 Feb 2017
- AC1: 'Reply to RC1', Tatsuya Nagashima, 05 May 2017
RC2: 'Interactive comment on “Long-term change in the contributions of various source regions to surface ozone over Japan” by Tatsuya Nagashima et al.', Anonymous Referee #2, 28 Feb 2017
- AC2: 'Reply to RC2', Tatsuya Nagashima, 05 May 2017

Peer-review completion

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

AR by Tatsuya Nagashima on behalf of the Authors (05 May 2017) Author's response Manuscript

ED: Referee Nomination & Report Request started (13 May 2017) by Qiang Zhang

ED: Publish as is (28 May 2017) by Qiang Zhang

AR by Tatsuya Nagashima on behalf of the Authors (01 Jun 2017)

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Short summary

We showed the large contribution of different source regions in Asia to the recent increasing trend in surface ozone over Japan by using a global chemical transport model. China accounted for the largest part of the increasing trend, not only through the domestic ozone production (36 %) but also the ozone production in the adjacent countries due to the ozone precursors emitted in China (10 %). Other factors such as temporal change in climate and methane concentration were also investigated.