Articles | Volume 19, issue 13
https://doi.org/10.5194/acp-19-8547-2019
https://doi.org/10.5194/acp-19-8547-2019
Research article
 | 
05 Jul 2019
Research article |  | 05 Jul 2019

An improved estimate for the δ13C and δ18O signatures of carbon monoxide produced from atmospheric oxidation of volatile organic compounds

Isaac J. Vimont, Jocelyn C. Turnbull, Vasilii V. Petrenko, Philip F. Place, Colm Sweeney, Natasha Miles, Scott Richardson, Bruce H. Vaughn, and James W. C. White

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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 Lorena Grabowski on behalf of the Authors (25 Feb 2019)  Author's response
ED: Referee Nomination & Report Request started (26 Feb 2019) by Jan Kaiser
RR by Anonymous Referee #1 (20 Mar 2019)
RR by Anonymous Referee #2 (24 Mar 2019)
ED: Reconsider after major revisions (24 Mar 2019) by Jan Kaiser
AR by Isaac Vimont on behalf of the Authors (05 May 2019)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (06 May 2019) by Jan Kaiser
RR by Anonymous Referee #1 (16 Jun 2019)
ED: Publish as is (18 Jun 2019) by Jan Kaiser
AR by Isaac Vimont on behalf of the Authors (19 Jun 2019)  Author's response    Manuscript
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Short summary
Stable isotopes of Carbon Monoxide (CO) and radiocarbon carbon dioxide were measured over three summers at Indianapolis, Indiana, US, and for 1 year at a site thought to be strongly influenced by CO from oxidized volatile organic compounds (VOCs) in South Carolina, US. The Indianapolis results were used to provide an estimate of the carbon and oxygen isotopic signatures of CO produced from oxidized VOCs. This updated estimate agrees well with the data from South Carolina during the summer.
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