Middle atmospheric ozone, nitrogen dioxide and nitrogen  trioxide in 2002–2011: SD-WACCM simulations  compared to GOMOS observations

Kyrölä, Erkki; Andersson, Monika E.; Verronen, Pekka T.; Laine, Marko; Tukiainen, Simo; Marsh, Daniel R.

doi:https://doi.org/10.5194/acp-18-5001-2018

Articles | Volume 18, issue 7

https://doi.org/10.5194/acp-18-5001-2018

© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Special issue:

Quadrennial Ozone Symposium 2016 – Status and trends...

https://doi.org/10.5194/acp-18-5001-2018

© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 18, issue 7

Research article

|

12 Apr 2018

Research article |

| 12 Apr 2018

Middle atmospheric ozone, nitrogen dioxide and nitrogen trioxide in 2002–2011: SD-WACCM simulations compared to GOMOS observations

Erkki Kyrölä, Monika E. Andersson, Pekka T. Verronen, Marko Laine, Simo Tukiainen, and Daniel R. Marsh

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Final revised paper (published on 12 Apr 2018)
Preprint (discussion started on 20 Dec 2017)

Interactive discussion

Status: closed

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

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RC1: 'Review of the manuscript Middle atmospheric ozone, nitrogen dioxide, and nitrogen trioxide in 2002–2011: SD-WACCM simulations compared to GOMOS observations by Kyrölä et al.', Anonymous Referee #1, 26 Jan 2018
- AC1: 'Response to Reviewer 1', Erkki Kyrölä, 14 Mar 2018
RC2: 'review of manuscript', Anonymous Referee #2, 30 Jan 2018
- AC2: 'Response to Reviewer 2', Erkki Kyrölä, 14 Mar 2018

Peer-review completion

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

AR by Erkki Kyrölä on behalf of the Authors (21 Mar 2018) Author's response Manuscript

ED: Publish as is (21 Mar 2018) by Stefan Reis

AR by Erkki Kyrölä on behalf of the Authors (21 Mar 2018)

Short summary

In this work we compare three key constituents of the middle atmosphere (ozone, NO₂, and NO₃) from the GOMOS satellite instrument with the WACCM model. We find that in the stratosphere (below 50 km) ozone differences are very small, but in the mesosphere large deviations are found. GOMOS and WACCM NO₂ agree reasonably well except in the polar areas. These differences can be connected to the solar particle storms. For NO₃, WACCM results agree with GOMOS with a very high correlation.