Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/9898
AuthorsVoigt, C.* 
Jessberg, P.* 
Jurkat, T.* 
Kaufmann, S.* 
Baumann, R.* 
Schlager, H.* 
Bobrowski, N.* 
Giuffrida, G.* 
Salerno, G.* 
TitleReply to comment from Liotta and Rizzo on “Evolution of CO2 , SO2 , HCl and HNO3 in the volcanic plumes from Etna” by Voigt et al. [Geophys. Res. Lett.; 41, doi:10.1002/2013GL058974]
Issue Date26-Aug-2014
Series/Report no./76 (2014)
DOI10.1007/s00445-014-0865-z
URIhttp://hdl.handle.net/2122/9898
KeywordsVolcanic degassing
Volcanic plume
Etna
Chemical evolution of trace gases
Subject Classification04. Solid Earth::04.08. Volcanology::04.08.01. Gases 
AbstractEditor’s Note: The following comment and reply arise from an article published in Geophysical Research Letters by Voigt et al. (2014). The article addresses a volcanology topic, and the commenters take issue with some conclusions and offer an analysis of their own. Voigt and co-authors have responded. Why is this comment-and-reply being published in the Bulletin? It is because Geophysical Research Letters is one of a number of journals that do not offer any published forum for discussion of the papers they publish. This is a matter of editorial policy and a decision for each journal. The Bulletin of Volcanology does provide a forum for discussion of articles published. When contacted by Marcello Liotta with the request that the Bulletin consider hosting a discussion of the Voigt et al. volcanology article in GRL, I agreed to do so if the GRL authors were willing to engage with the comment. Voigt and co-authors were willing to do so and have been allowed a small amount of additional space to summarize for Bulletin readers the key points of the GRL paper under discussion before responding directly to the comment from Liotta and Rizzo. I hope that Bulletin readers find the discussion and reply of interest.
Appears in Collections:Papers Published / Papers in press

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