Stratospheric ozone measurements at Arosa (Switzerland):  history and scientific relevance

Staehelin, Johannes; Viatte, Pierre; Stübi, Rene; Tummon, Fiona; Peter, Thomas

doi:https://doi.org/10.5194/acp-18-6567-2018

Articles | Volume 18, issue 9

https://doi.org/10.5194/acp-18-6567-2018

© 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-18-6567-2018

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

Articles | Volume 18, issue 9

Research article

|

08 May 2018

Research article |

| 08 May 2018

Stratospheric ozone measurements at Arosa (Switzerland): history and scientific relevance

Johannes Staehelin, Pierre Viatte, Rene Stübi, Fiona Tummon, and Thomas Peter

Download

Final revised paper (published on 08 May 2018)
Preprint (discussion started on 29 Nov 2017)

Interactive discussion

Status: closed

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

- Printer-friendly version

- Supplement

RC1: 'Review of the manuscript', Anonymous Referee #1, 27 Dec 2017
- RC2: 'Review', Anonymous Referee #2, 22 Jan 2018
  - AC2: 'Comments to Reviewer 2', Johannes Staehelin, 08 Mar 2018
- AC1: 'Comments to Reviewer 1', Johannes Staehelin, 08 Mar 2018

Peer-review completion

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

AR by Svenja Lange on behalf of the Authors (22 Mar 2018) Author's response Manuscript

ED: Publish as is (22 Mar 2018) by Stefan Reis

Short summary

In 1926, total ozone series started in Arosa (Switzerland). Since the mid-1970s ozone is measured to document the effects of anthropogenic ozone-depleting substances (ODSs). ODSs peaked around the mid-1990s, resulting from the Montreal Protocol (1987) and its enforcement. Chemical ozone depletion stopped worsening around the mid-1990s but the large variability complicates demonstrations of the success of the protocol and the effect of ongoing climate change still requires continuous measurement.