Volumes and Issues  Contents of Issue 6  Special Issue  
Nonlin. Processes Geophys., 18, 925-940, 2011
www.nonlin-processes-geophys.net/18/925/2011/
doi:10.5194/npg-18-925-2011
© Author(s) 2011. This work is distributed
under the Creative Commons Attribution 3.0 License.


Self-sustained vibrations in volcanic areas extracted by Independent Component Analysis: a review and new results

E. De Lauro, S. De Martino, M. Falanga, and M. Palo
Dipartimento di Ingegneria Industriale, Salerno University, Ponte Don Melillo street, 84084, Fisciano (SA), Italy

Abstract. We investigate the physical processes associated with volcanic tremor and explosions. A volcano is a complex system where a fluid source interacts with the solid edifice so generating seismic waves in a regime of low turbulence. Although the complex behavior escapes a simple universal description, the phases of activity generate stable (self-sustained) oscillations that can be described as a non-linear dynamical system of low dimensionality. So, the system requires to be investigated with non-linear methods able to individuate, decompose, and extract the main characteristics of the phenomenon. Independent Component Analysis (ICA), an entropy-based technique is a good candidate for this purpose. Here, we review the results of ICA applied to seismic signals acquired in some volcanic areas. We emphasize analogies and differences among the self-oscillations individuated in three cases: Stromboli (Italy), Erebus (Antarctica) and Volcán de Colima (Mexico). The waveforms of the extracted independent components are specific for each volcano, whereas the similarity can be ascribed to a very general common source mechanism involving the interaction between gas/magma flow and solid structures (the volcanic edifice). Indeed, chocking phenomena or inhomogeneities in the volcanic cavity can play the same role in generating self-oscillations as the languid and the reed do in musical instruments. The understanding of these background oscillations is relevant not only for explaining the volcanic source process and to make a forecast into the future, but sheds light on the physics of complex systems developing low turbulence.

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Citation: De Lauro, E., De Martino, S., Falanga, M., and Palo, M.: Self-sustained vibrations in volcanic areas extracted by Independent Component Analysis: a review and new results, Nonlin. Processes Geophys., 18, 925-940, doi:10.5194/npg-18-925-2011, 2011.   Bibtex   EndNote   Reference Manager    XML