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Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/9120

Authors: Liotta, M.*
Rizzo, L.*
Title: Comment 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]
Title of journal: Bulletin of volcanology
Series/Report no.: /76 (2014)
Publisher: Springer Berlin Heidelberg
Issue Date: Nov-2014
DOI: 10.1007/s00445-014-0864-0
URL: http://link.springer.com/article/10.1007/s00445-014-0864-0
Keywords: Evolution . Mt. Etna . Volcanic plumes
Abstract: Editor’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. James D.L. White Executive Editor, Bulletin of Volcanology
Appears in Collections:04.08.01. Gases
Papers Published / Papers in press

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