First quasi-Lagrangian in situ measurements of Antarctic Polar springtime ozone:  observed ozone loss rates from the Concordiasi long-duration balloon campaign

Schofield, R.; Avallone, L. M.; Kalnajs, L. E.; Hertzog, A.; Wohltmann, I.; Rex, M.

doi:https://doi.org/10.5194/acp-15-2463-2015

Articles | Volume 15, issue 5

https://doi.org/10.5194/acp-15-2463-2015

© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.

https://doi.org/10.5194/acp-15-2463-2015

© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.

Articles | Volume 15, issue 5

Research article

|

05 Mar 2015

Research article |

| 05 Mar 2015

First quasi-Lagrangian in situ measurements of Antarctic Polar springtime ozone: observed ozone loss rates from the Concordiasi long-duration balloon campaign

R. Schofield, L. M. Avallone, L. E. Kalnajs, A. Hertzog, I. Wohltmann, and M. Rex

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Final revised paper (published on 05 Mar 2015)
Preprint (discussion started on 01 Sep 2014)

Interactive discussion

Status: closed

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

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RC C7459: 'Review comment', Anonymous Referee #1, 26 Sep 2014
- AC C11495: 'Reply', Robyn Schofield, 24 Jan 2015
RC C7508: 'Review comments', Marc von Hobe, 29 Sep 2014
- AC C11496: 'Reply', Robyn Schofield, 24 Jan 2015

Peer-review completion

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

AR by Robyn Schofield on behalf of the Authors (24 Jan 2015) Author's response Manuscript

ED: Publish as is (27 Jan 2015) by Martin Dameris

Short summary

Ozone measurements onboard three Concordiasi balloons flown in the stratosphere in the Antarctic spring of 2010 are presented. These measurements are the first long-duration in situ measurements of Antarctic springtime stratospheric ozone. By matching air parcels, ozone loss rates where derived. Downwind of the Antarctic Peninsula, very large ozone losses of up to 230 ppb per day or 16 ppbv per sunlit hour were observed. These high rates are consistent with almost complete chlorine activation.