Abstract
The results of more than three years of continuous gravity record on Mt. Vesuvius (Southern Italy) are presented and discussed.The goal of this research is to determine whether continuous gravity records can improve the overall monitoring efforts at the volcano specifically by detecting a gravity signal of “non-tidal” origin.The ocean and atmospheric effects have been taken into account for the computation of the tidal parameters and gravity residuals. Tidal analyses have been carried out by means of classical and recent methodologies and the results compared.The time dependent behaviour of the main tidal parameters and of the gravity residuals have been compared with features of the vesuvian dynamics, namely with the seismic activity and the temporal gravity changes detected by absolute and relative gravimetry.
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