Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/518
AuthorsScollo, S.* 
Coltelli, M.* 
Prodi, F.* 
Folegani, M.* 
Natali, S.* 
TitleTerminal settling velocity measurements of volcanic ash during the 2002-2003 Etna eruption by an X-band microwave rain gauge disdrometer
Issue Date10-May-2005
Series/Report no.L10302/32(2005)
DOI10.1029/2005GL022100
URIhttp://hdl.handle.net/2122/518
KeywordsVolcanology: Explosive volcanism
Volcanology: Remote sensing of volcanoes
Volcanology: Instruments and techniques
Volcanology: Volcano monitoring
Subject Classification04. Solid Earth::04.08. Volcanology::04.08.02. Experimental volcanism 
04. Solid Earth::04.08. Volcanology::04.08.06. Volcano monitoring 
04. Solid Earth::04.08. Volcanology::04.08.07. Instruments and techniques 
AbstractThis is the first report in the scientific literature of direct measurement of the terminal settling velocity of volcanic particles during an eruption. Field measurements using a continuous wave X-band disdrometer were carried out at Mt. Etna on 18 and 19 December 2002, when the explosive activity produced a 4 km high volcanic plume. These data allow the estimation of the intensity of the fallout and the measurement of the terminal settling velocities of the volcanic particles in real-time. The main results are: (1) the tested instrument detected coherent falling volcanic particles from 0.2 to 1 mm diameter; (2) measured terminal settling velocities were in agreement with both experimental and theoretical methods; (3) however, the measured velocities were clustered around few discrete values, rather than a range of velocities as would be expected if the particles were falling simultaneously and discretely. This new methodology has many new applications for local hazard mitigation and improved understanding of fallout processes.
Appears in Collections:Papers Published / Papers in press

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