GNGTS 2017 - 36° Convegno Nazionale

GNGTS 2017 S essione 2.1 321 recorded temperature variations disappeared. Being so, it is plausible that the electrical pump overloading may have produced temperature these variations. Fig. 3 shows the positionings of the thermometers, meteorological stations, the Pale multi-parametric station as well as the Central Italy Electromagnetic Network stations. References Fidani C.; 2011: The Central Italy Electromagnetic Network and the 2009 L’Aquila earthquake: observed electric activity, geosciences, 1, 3-25. Fidani C. and Martinelli G.; 2015: A Possible Explanation for Electric Perturbations Recorded by the Italian CIEN Stations Before the 2012 Emilia Earthquakes, Bollettino di Geofisica Teorica Applicata, 56, 2, 211-226. Fidani C. and Marcelli D.; 2017: Ten Years of the Central Italy Electromagnetic Network (CIEN) Continuous Monitoring, Open Journal of Earthquake Research, 6, 73-88. Mosciatti A.; 1997: Mi tremava anche il sogno, L’esperienza del terremoto raccontata dai bambini di Serravalle di Chienti, Magi Edizioni, Collana: I bambini raccontano, Roma.