The natural oscillations in stratospheric ozone observed by the GROMOS microwave radiometer at the NDACC station Bern

Moreira, Lorena; Hocke, Klemens; Navas-Guzmán, Francisco; Eckert, Ellen; von Clarmann, Thomas; Kämpfer, Niklaus

doi:https://doi.org/10.5194/acp-16-10455-2016

Articles | Volume 16, issue 16

https://doi.org/10.5194/acp-16-10455-2016

© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue:

Twenty-five years of operations of the Network for the Detection...

https://doi.org/10.5194/acp-16-10455-2016

© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Articles | Volume 16, issue 16

Research article

|

19 Aug 2016

Research article |

| 19 Aug 2016

The natural oscillations in stratospheric ozone observed by the GROMOS microwave radiometer at the NDACC station Bern

Lorena Moreira, Klemens Hocke, Francisco Navas-Guzmán, Ellen Eckert, Thomas von Clarmann, and Niklaus Kämpfer

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Final revised paper (published on 19 Aug 2016)
Preprint (discussion started on 15 Mar 2016)

Interactive discussion

Status: closed

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

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RC1: 'Review of manuscript ACP-2016-66 authored by Moreira et al.', Ellis Remsberg, 14 Apr 2016
RC2: 'Review of paper by Moreira et al.', Anonymous Referee #2, 20 Apr 2016
AC1: 'Final author comments', Lorena Moreira, 23 May 2016

Peer-review completion

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

AR by Lorena Moreira on behalf of the Authors (23 May 2016) Author's response Manuscript

ED: Publish as is (30 Jul 2016) by Guy Brasseur

AR by Lorena Moreira on behalf of the Authors (02 Aug 2016)

Short summary

The GROMOS radiometer in Bern has been part of the NDACC since 1994. Our time series of stratospheric ozone profiles allow the assessment of natural oscillations, which are essential for the evaluation of detected stratospheric ozone trends. Among our new findings are the link between the upper stratospheric O₃-SAO and the polar stratopause warmings in winter. We have also detected a strong peak amplitude of 5 % related to the solar activity cycle and the ENSO effect in ozone at midlatitudes.