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Volume 17, issue 24
Atmos. Chem. Phys., 17, 15019–15036, 2017
https://doi.org/10.5194/acp-17-15019-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 4.0 License.
Atmos. Chem. Phys., 17, 15019–15036, 2017
https://doi.org/10.5194/acp-17-15019-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 4.0 License.

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 et al.

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Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer review completion

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
Publications Copernicus
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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.
The space–time evolutions of the Calbuco plume are investigated by combining satellite, in situ...
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