Articles | Volume 37, issue 4
https://doi.org/10.5194/angeo-37-525-2019
https://doi.org/10.5194/angeo-37-525-2019
Regular paper
 | 
04 Jul 2019
Regular paper |  | 04 Jul 2019

Assessing the role of planetary and gravity waves in the vertical structure of ozone over midlatitudinal Europe

Peter Križan

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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
ED: Reconsider after major revisions (further review by editor and referees) (26 Mar 2019) by Andrew J. Kavanagh
AR by Peter Krizan on behalf of the Authors (26 Mar 2019)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (27 Mar 2019) by Andrew J. Kavanagh
RR by Anonymous Referee #1 (25 Apr 2019)
ED: Publish subject to revisions (further review by editor and referees) (26 Apr 2019) by Andrew J. Kavanagh
AR by Peter Krizan on behalf of the Authors (06 Jun 2019)  Author's response   Manuscript 
ED: Publish as is (18 Jun 2019) by Andrew J. Kavanagh
AR by Peter Krizan on behalf of the Authors (19 Jun 2019)  Author's response   Manuscript 
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Short summary
We observe the planetary and gravity wave activity in the vertical profile of ozone at the mid-European ozonosonde stations The performance of the used detection method is satisfactory. There are differences in the following characteristics of the structure caused by the planetary and gravity wave: the annual variation, the size, and the vertical distribution. The results are influenced by the ozonosonde vertical resolution only for small and medium structures.