Articles | Volume 17, issue 24
https://doi.org/10.5194/acp-17-15019-2017
https://doi.org/10.5194/acp-17-15019-2017
Research article
 | 
19 Dec 2017
Research article |  | 19 Dec 2017

Long-range transport of stratospheric aerosols in the Southern Hemisphere following the 2015 Calbuco eruption

Nelson Bègue, Damien Vignelles, Gwenaël Berthet, Thierry Portafaix, Guillaume Payen, Fabrice Jégou, Hassan Benchérif, Julien Jumelet, Jean-Paul Vernier, Thibaut Lurton, Jean-Baptiste Renard, Lieven Clarisse, Vincent Duverger, Françoise Posny, Jean-Marc Metzger, and Sophie Godin-Beekmann

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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 Nelson Bègue on behalf of the Authors (10 Oct 2017)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (12 Oct 2017) by Anja Schmidt
RR by Anonymous Referee #1 (12 Oct 2017)
RR by Anonymous Referee #3 (24 Oct 2017)
RR by Vladislav Gerasimov (24 Oct 2017)
ED: Publish subject to minor revisions (review by editor) (24 Oct 2017) by Anja Schmidt
AR by Nelson Bègue on behalf of the Authors (02 Nov 2017)  Author's response   Manuscript 
ED: Publish as is (06 Nov 2017) by Anja Schmidt
AR by Nelson Bègue on behalf of the Authors (10 Nov 2017)  Manuscript 
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Short summary
The space–time evolutions of the Calbuco plume are investigated by combining satellite, in situ aerosol counting and lidar observations, and a numerical model. All the data at Reunion Island reveal a twofold increase in the amount of aerosol with respect to the values observed before the eruption. The dynamic context has favored the spread of the plume exclusively in the Southern Hemisphere. This study highlights the role played by dynamical barriers in the transport of atmospheric species.
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