GNGTS 2023 - Atti del 41° Convegno Nazionale

Session 1.3 GNGTS 2023 Our work provides direct evidence of deep magma inflation at least since 2015, thus giving a strong warning of increasing risk at Campi Flegrei. Part of the analyses and results are in Amoruso and Crescentini (2022). References Amoruso A. and Crescentini L.; 2022: Clues of Ongoing Deep Magma Inflation at Campi Flegrei Caldera (Italy) from Empirical Orthogonal Function Analysis of SAR Data. Remote Sens., 14, 5698, DOI 10.3390/rs14225698. Amoruso A., Crescentini L. and Sabbetta I.; 2014: Paired deformation sources of the Campi Flegrei caldera (Italy) required by recent (1980–2010) deformation history. J. Geophys. Res. Solid Earth, 119, 858-879, DOI 10.1002/2013JB010392. 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 Trans. Geosci. Remote Sens., 40, 2375-2383, DOI 10.1109/TGRS.2002.803792. Navarra A. and Simoncini V.; 2010: A Guide to Empirical Orthogonal Functions for Climate Data Analysis. Springer, Dordrecht, The Netherlands, 151 pp. Polcari M., Borgstrom S., Del Gaudio C., De Martino P., Ricco C., Siniscalchi V. and Trasatti E.; 2022: Thirty years of volcano geodesy from space at Campi Flegrei caldera (Italy). Scientific Data, 9:728, DOI 10.1038/s41597-022-01849-7. Sandwell D., Mellors R., Tong X., Wei M. and Wessel P.; 2011: Open radar interferometry software for mapping surface deformation. Eos Trans. AGU, 92, 234-235, DOI 10.1029/2011EO280002.