Characterization of GPS time series at the Neapolitan volcanic area by statistical analysis

The GPS time series recorded at the Neapolitan volcanic area reveals a very peculiar behavior. When a clear deformation is observed, the amplitude distribution evolves from a super‐Gaussian to a broader distribution. This behavior can be characterized by evaluating the kurtosis. Spurious periodic co...

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Bibliographic Details
Published in:Journal of Geophysical Research: Solid Earth Vol. 115; no. B10
Main Authors: Bottiglieri, M., Falanga, M., Tammaro, U., De Martino, P., Obrizzo, F., Godano, C., Pingue, F.
Format: Journal Article
Language:English
Published: Washington, DC Blackwell Publishing Ltd 01-10-2010
American Geophysical Union
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Summary:The GPS time series recorded at the Neapolitan volcanic area reveals a very peculiar behavior. When a clear deformation is observed, the amplitude distribution evolves from a super‐Gaussian to a broader distribution. This behavior can be characterized by evaluating the kurtosis. Spurious periodic components were evidenced by independent component analysis and then removed by filtering the original signal. The time series for all stations was modeled with a fifth‐order polynomial fit, which represents the deformation history at that place. Indeed, when this polynomial is subtracted from the time series, the distributions again become super‐Gaussian. A simulation of the deformation time evolution was performed by superposing a Laplacian noise and a synthetic deformation history. The kurtosis of the obtained signals decreases as the superposition increases, enlightening the insurgence of the deformation. The presented approach represents a contribution aimed at adding further information to the studies about the deformation at the Neapolitan volcanic area by revealing geologically relevant data.
Bibliography:ArticleID:2009JB006594
Tab-delimited Table 1.
ark:/67375/WNG-7QLSD166-1
istex:4599CAEDA9D40405BB187F2A88E8FF384AD37F94
ISSN:0148-0227
2169-9313
2156-2202
2169-9356
DOI:10.1029/2009JB006594