Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/8757
AuthorsDe Lauro, E.* 
De Martino, S.* 
Falanga, M.* 
Petrosino, S.* 
TitleSynchronization between tides and sustained oscillations of the hydrothermal system of Campi Flegrei (Italy)
Issue Date2-Aug-2013
Series/Report no./14 (2013)
DOI10.1002/ggge.20149
URIhttp://hdl.handle.net/2122/8757
Keywordssustained hydrothermal tremor
Campi Flegrei Caldera
polarization analysis
tidal modulation
Subject Classification04. Solid Earth::04.06. Seismology::04.06.08. Volcano seismology 
AbstractLong continuous seismic data recorded at five broadband seismic stations during 2006 at Campi Flegrei caldera have been analyzed. Introducing a coarse-grained method, we evaluate the time evolution of amplitude and polarization of the seismic noise in the frequency band common to long-period events. The series are modulated on tidal time scales: the root-mean square is basically dominated by solar contribution, while the azimuth of the polarization vector shows lunar diurnal and semidiurnal constituents. In addition, we find that in the frequency band common to long-period events the azimuths are polarized toward a specific area, suggesting that these persistent oscillations can be induced by the activity of the shallow geothermal reservoir.
Appears in Collections:Papers Published / Papers in press

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