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  5. Application of differential SAR interferometry for studying eruptive event of 22July 1998 at Mt.Etna
 
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Application of differential SAR interferometry for studying eruptive event of 22July 1998 at Mt.Etna

Author(s)
Coltelli, M.  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia  
Puglisi, G.  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia  
Guglielmino, F.  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia  
Palano, M.  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia  
Language
English
Status
Published
Peer review journal
Yes
Journal
Quaderni di Geofisica  
Issue/vol(year)
/ 43 (2006)
Publisher
INGV
Pages (printed)
15-20
Date Issued
2006
URI
https://www.earth-prints.org/handle/2122/2614
Subjects
04. Solid Earth::04.08. Volcanology::04.08.06. Volcano monitoring  
04. Solid Earth::04.08. Volcanology::04.08.07. Instruments and techniques  
04. Solid Earth::04.08. Volcanology::04.08.08. Volcanic risk  
Subjects

SAR interferometry

Abstract
One of the main objectives of the project
“Development and application of remote sensing
methods for the monitoring of active Italian
volcanoes” is directed to an operational use of
differential interferometry as a tool for volcano
monitoring. A first step to achieve this goal is to
test commercial software in order to evaluate
the most suitable for the project purposes. For
testing software, SAR images collected by
ERS2 from May 98 to August 98, before and
after the strong eruptive event occurred on 22
July 98 at Voragine crater of Etna, have been
selected. The explosive event was classified
sub-plinian producing a 12 km high eruptive
column and lapilli fell on land as far as 70 km
south-eastward along the dispersal axis. Pre,
post and across event image pairs have been
processed. In particular the pair 13 May 98-22
July 98, 22 July 98-26 August 98, 13 May 98-26
August 98 are used for testing respectively pre,
post and across event. In first analysis, the
fringes in the differential products show a positive
elevation trend in the summit area of the
volcano. In particular, an increased of about 1,5
fringes in the period pre-event, and a decrement
of 1 fringe in the period post-event is observed.
This result is agreement whit field of deformation
expected in such kind of event, confirming
that the interferometric processing tool used id
suitable for the purpose of the project.
References
Aloisi, M., D’Agostino, M., Dean, K. G, Mostaccio,
A., Neri, G., (2002). Satellite analysis and
PUFF simulation of the eruptive cloud generated
by the Mount Etna paroxysm of 22 July
1998. J. Geophys. Res., 107(B12) ECV 9/1-
ECV 9/12.
Bonaccorso, A., Davis, M., (1999). Models of
ground deformation from vertical volcanic
conduits with application to eruptions of
Mount. St. Helens and Mount Etna, J.
Geophys. Res., 104, 10531-10542.
Andronico, D. , Coltelli, M., Del Carlo, P. , (in prep).
Tephra fallout from the smaller documented
Subplinian eruption occurred at Mt. Etna on
22 July 1998.
Type
article
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