Articles | Volume 16, issue 7
Research article
07 Apr 2016
Research article |  | 07 Apr 2016

The vertical distribution of volcanic SO2 plumes measured by IASI

Elisa Carboni, Roy G. Grainger, Tamsin A. Mather, David M. Pyle, Gareth E. Thomas, Richard Siddans, Andrew J. A. Smith, Anu Dudhia, Mariliza E. Koukouli, and Dimitrios Balis


Interactive discussion

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 Anna Wenzel on behalf of the Authors (01 Feb 2016)  Author's response
ED: Reconsider after minor revisions (Editor review) (22 Feb 2016) by Marc von Hobe
AR by Svenja Lange on behalf of the Authors (08 Mar 2016)  Author's response
ED: Publish as is (14 Mar 2016) by Marc von Hobe
Short summary
The Infrared Atmospheric Sounding Interferometer (IASI) can be used to study volcanic emission of sulfur dioxide (SO2), returning both SO2 amount and altitude data. The series of analyzed eruptions (2008 to 2012) show that the biggest emitter of volcanic SO2 was Nabro, followed by Kasatochi and Grimsvotn. Our observations also show a tendency for volcanic SO2 to reach the level of the tropopause. This tendency was independent of the maximum amount of SO2 and of the volcanic explosive index.
Final-revised paper