Articles | Volume 17, issue 3
https://doi.org/10.5194/acp-17-2229-2017
https://doi.org/10.5194/acp-17-2229-2017
Research article
 | 
14 Feb 2017
Research article |  | 14 Feb 2017

Impact of a moderate volcanic eruption on chemistry in the lower stratosphere: balloon-borne observations and model calculations

Gwenaël Berthet, Fabrice Jégou, Valéry Catoire, Gisèle Krysztofiak, Jean-Baptiste Renard, Adam E. Bourassa, Doug A. Degenstein, Colette Brogniez, Marcel Dorf, Sebastian Kreycy, Klaus Pfeilsticker, Bodo Werner, Franck Lefèvre, Tjarda J. Roberts, Thibaut Lurton, Damien Vignelles, Nelson Bègue, Quentin Bourgeois, Daniel Daugeron, Michel Chartier, Claude Robert, Bertrand Gaubicher, and Christophe Guimbaud

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AR: Author's response | RR: Referee report | ED: Editor decision
AR by Gwenael Berthet on behalf of the Authors (07 Jan 2017)  Manuscript 
ED: Publish as is (12 Jan 2017) by Andreas Engel
AR by Gwenael Berthet on behalf of the Authors (21 Jan 2017)
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Short summary
Since the last major volcanic event, i.e. the Pinatubo eruption in 1991, only moderate eruptions have regularly injected sulfur into the stratosphere, typically enhancing the aerosol loading for several months. We investigate here for the first time the chemical perturbation associated with the Sarychev eruption in June 2009, using balloon-borne instruments and model calculations. Some chemical compounds are significantly affected by the aerosols, but the impact on stratospheric ozone is weak.
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