Articles | Volume 18, issue 7
Atmos. Chem. Phys., 18, 5157–5171, 2018
https://doi.org/10.5194/acp-18-5157-2018
Atmos. Chem. Phys., 18, 5157–5171, 2018
https://doi.org/10.5194/acp-18-5157-2018

Research article 17 Apr 2018

Research article | 17 Apr 2018

Observations of ozone-poor air in the tropical tropopause layer

Richard Newton et al.

Download

Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Richard Newton on behalf of the Authors (17 Feb 2018)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (19 Feb 2018) by Jianzhong Ma
RR by Anonymous Referee #1 (27 Feb 2018)
RR by Anonymous Referee #2 (12 Mar 2018)
ED: Publish as is (14 Mar 2018) by Jianzhong Ma
Download
Short summary
We consider the ozone measurements from aircraft during the CAST/CONTRAST/ATTREX campaigns of 2014. Low concentrations of ozone were found in the layer of 10–15 km altitude, which is indicative of uplift of ozone-poor air from near the sea surface to 10–15 km altitude. Chemicals that have origins in the sea were found in greater abundance when ozone concentrations were low compared to when ozone concentrations were high. The lowest ozone concentrations were found in the Southern Hemisphere.
Altmetrics
Final-revised paper
Preprint