Articles | Volume 15, issue 4
Atmos. Chem. Phys., 15, 1901–1912, 2015
https://doi.org/10.5194/acp-15-1901-2015
Atmos. Chem. Phys., 15, 1901–1912, 2015
https://doi.org/10.5194/acp-15-1901-2015

Research article 24 Feb 2015

Research article | 24 Feb 2015

An estimation of the 18O / 16O ratio of UT/LMS ozone based on artefact CO in air sampled during CARIBIC flights

S. Gromov and C. A. M. Brenninkmeijer

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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
AR by Sergey Gromov on behalf of the Authors (19 Oct 2014)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (20 Oct 2014) by Jan Kaiser
RR by Anonymous Referee #1 (30 Oct 2014)
ED: Reconsider after minor revisions (Editor review) (12 Nov 2014) by Jan Kaiser
AR by Sergey Gromov on behalf of the Authors (24 Nov 2014)  Author's response    Manuscript
ED: Reconsider after minor revisions (Editor review) (28 Nov 2014) by Jan Kaiser
AR by Sergey Gromov on behalf of the Authors (08 Dec 2014)  Author's response    Manuscript
ED: Reconsider after minor revisions (Editor review) (09 Dec 2014) by Jan Kaiser
AR by Sergey Gromov on behalf of the Authors (10 Dec 2014)  Author's response    Manuscript
ED: Reconsider after minor revisions (Editor review) (18 Dec 2014) by Jan Kaiser
AR by Sergey Gromov on behalf of the Authors (05 Jan 2015)  Author's response    Manuscript
ED: Publish subject to technical corrections (23 Jan 2015) by Jan Kaiser
AR by Sergey Gromov on behalf of the Authors (04 Feb 2015)  Author's response    Manuscript
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Short summary
We present observational data on δ18O(O3) from the UT/LMS, the region to date not covered by the ozone isotope composition measurements. It is to bridge the gap between the tropospheric (mostly surface) and stratospheric measurement data. We demonstrate an approach suitable for isotope mass-balance calculations (“Keeling plot”) in intricate cases, i.e. admixing of the (unknown) source in question to the reservoirs with (unknown) variable starting compositions.
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