Atmos. Chem. Phys., 20, 8611–8626, 2020 https://doi.org/10.5194/acp-20-8611-2020 © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License. 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 Héron1, Stéphanie Evan1, Jérôme Brioude1, Karen Rosenlof2, Françoise Posny1, Jean-Marc Metzger3, and Jean-Pierre Cammas1,3 1LACy, Laboratoire de l’Atmosphère et des Cyclones, UMR8105, CNRS, Université de La Réunion, Météo-France, Saint-Denis, La Réunion, France 2Chemical Sciences Division, Earth System Research Laboratory, NOAA, Boulder, CO, USA 3Observatoire des Sciences de l’Univers de La Réunion, UMS3365, CNRS, Université de La Réunion, Météo-France, Saint-Denis, La Réunion, France Correspondence: Damien Héron (
[email protected]) Received: 2 January 2020 – Discussion started: 18 February 2020 Revised: 22 May 2020 – Accepted: 25 June 2020 – Published: 22 July 2020 Abstract. Observations of ozonesonde measurements of the but it is observed more than 1000 km away from the island, NDACC/SHADOZ (Network for the Detection of Atmo- in the tropics, either from tropical storms or the Intertropi- spheric Composition Change and the Southern Hemisphere cal Convection Zone (ITCZ). In November and December, ADditional OZonesondes) program and humidity profiles the air masses above Réunion island originate, on average, from the daily Météo-France radiosondes at Réunion island from central Africa and the Mozambique Channel. During (21.1◦ S, 55.5◦ E) from November 2013 to April 2016 were January and February the source region is the northeast of analyzed to identify the origin of wet upper-tropospheric Mozambique and Madagascar.