Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/9645
AuthorsDe Martino, P.* 
Tammaro, U.* 
Obrizzo, F.* 
TitleGPS time series at Campi Flegrei caldera (2000-2013)
Issue Date12-Feb-2014
Series/Report no.2/57 (2014)
DOI10.4401/ag-6431
URIhttp://hdl.handle.net/2122/9645
Keywordsmeasurements and monitoring, GPS, Time series, Campi Flegrei, Ground deformation
Subject Classification04. Solid Earth::04.08. Volcanology::04.08.06. Volcano monitoring 
AbstractThe Campi Flegrei caldera is an active volcanic system associated to a high volcanic risk, and represents a well known and peculiar example of ground deformations (bradyseism), characterized by intense uplift periods, followed by subsidence phases with some episodic superimposed mini-uplifts. Ground deformation is an important volcanic precursor, and, its continuous monitoring, is one of the main tool for short time forecast of eruptive activity. This paper provides an overview of the continuous GPS monitoring of the Campi Flegrei caldera from January 2000 to July 2013, including network operations, data recording and processing, and data products. In this period the GPS time series allowed continuous and accurate tracking of ground deformation of the area. Seven main uplift episodes were detected, and during each uplift period, the recurrent horizontal displacement pattern, radial from the “caldera center”, suggests no significant change in deformation source geometry and location occurs. The complete archive of GPS time series at Campi Flegrei area is reported in the Supplementary materials. These data can be usefull for the scientific community in improving the research on Campi Flegrei caldera dynamic and hazard assessment.
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