Articles | Volume 20, issue 14
Atmos. Chem. Phys., 20, 8611–8626, 2020
https://doi.org/10.5194/acp-20-8611-2020
Atmos. Chem. Phys., 20, 8611–8626, 2020
https://doi.org/10.5194/acp-20-8611-2020

Research article 22 Jul 2020

Research article | 22 Jul 2020

Impact of convection on the upper-tropospheric composition (water vapor and ozone) over a subtropical site (Réunion island; 21.1° S, 55.5° E) in the Indian Ocean

Damien Héron et al.

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AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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AR: Author's response | RR: Referee report | ED: Editor decision
AR by Damien Héron on behalf of the Authors (22 May 2020)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (08 Jun 2020) by Farahnaz Khosrawi
RR by Anonymous Referee #1 (09 Jun 2020)
RR by Anonymous Referee #2 (24 Jun 2020)
ED: Publish subject to technical corrections (25 Jun 2020) by Farahnaz Khosrawi
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Short summary
Using a statistical method, summer variations (between 2013 and 2016) of ozone and water vapor are characterized in the upper troposphere above Réunion island (21° S, 55° E). It suggests a convective influence between 9 and 13 km. As deep convection is rarely observed near Réunion island, this study provides new insights on the long-range impact of deep convective outflow from the Intertropical Convergence Zone (ITCZ) on the upper troposphere over a subtropical site.
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