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  5. Ground deformation of Long Valley caldera and Mono Basin, eastern California, mapped by satellite radar interferometry
 
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Ground deformation of Long Valley caldera and Mono Basin, eastern California, mapped by satellite radar interferometry

Author(s)
Tizzani, P.  
Istituto per il Rilevamento Elettromagnetico dell'Ambiente, National Research  
Berardino, P.  
Istituto per il Rilevamento Elettromagnetico dell'Ambiente, National Research  
Casu, F.  
Dipartimento di Ingegneria Elettrica ed Elettronica, Università degli studi di Cagliari  
Euillades, P.  
Conicet, Instituto CEDIAC, Facultad de Ingenierìa, Universidad Nac de Cuyo,  
Manzo, M.  
Dipartimento di Ingegneria e Fisica dell'Ambiente, Università degli Studi della Basilicata, I-85100 Potenza, Italy  
Ricciardi, G. P.  
Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia  
Zeni, G.  
Istituto per il Rilevamento Elettromagnetico dell'Ambiente, National Research  
Lanari, R.  
Istituto per il Rilevamento Elettromagnetico dell'Ambiente, National Research  
Language
English
Obiettivo Specifico
1.3. TTC - Sorveglianza geodetica delle aree vulcaniche attive
3.2. Tettonica attiva
4.3. TTC - Scenari di pericolosità vulcanica
Status
Published
JCR Journal
JCR Journal
Peer review journal
Yes
Journal
International Journal of Remote Sensing  
Issue/vol(year)
2 / 29 (2008)
Publisher
Taylor & Francis
Pages (printed)
439–441
Date Issued
2007
DOI
10.1080/01431160701264201
URI
https://www.earth-prints.org/handle/2122/3392
Subjects
04. Solid Earth::04.03. Geodesy::04.03.07. Satellite geodesy  
Subjects

Ground deformation

Long Valley caldera

Mono Basin

satellite radar

Abstract
We have illustrated the key results of the Differential SAR Interferometry
(DInSAR) analysis focused on the ground deformation of Long Valley caldera
and Mono Basin, eastern California. In particular, we have applied the DInSAR
algorithm referred to as Small BAseline Subset (SBAS) approach and processed
21 SAR images, spanning the time interval from 1992 to 2000, acquired from
descending arbits by the ERS-1 and ERS-2 sensors of the European Space
Agency (ESA). The deformation affecting the resurgent dome of Long Valley
caldera has been highlighted as well as the previously unreported subsidence of
the Pahoa island, located in Mono Lake.
References
BATTAGLIA, M., SEGALL, P., MURRAY, J., CERVELLI, P. and LANGBEIN, J., 2003, The
mechanics of unrest at Long Valley caldera, California: 1. Modeling the geometry of
the source using GPS, leveling and two-color EDM data. Journal of Volcanology and
Geothermal Research, 127, pp. 195–217.
BERARDINO, P., FORNARO, G., LANARI, R. and SANSOSTI, E., 2002, A new algorithm for
surface deformation monitoring based on small baseline differential SAR interferograms.
IEEE Transactions on Geoscience and Remote Sensing, 40, pp. 2375–2383.
TIZZANI, P., BERARDINO, P., CASU, F., EUILLADES, P.,MANZO, M., RICCIARDI, G.P., ZENI, G.
and LANARI, R., 2007, Surface deformation of Long Valley caldera and Mono Basin,
California, investigated with the SBAS-InSAR approach. Remote Sensing of
Environment, 108, pp. 277–289.
Type
article
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