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IUGG XXIV General Assembly July 2-13, 2007 Perugia, Italy<br />

(S) - <strong>IASPEI</strong> - International Association of Seismology and Physics of the Earth's<br />

Interior<br />

JSS009 Oral Presentation 2023<br />

Analysing complex time series in natural time<br />

Prof. Panayiotis Varotsos<br />

Physics Department University of Athens <strong>IASPEI</strong><br />

Nicholas V Sarlis, Efthimios S Skordas<br />

Novel dynamical features hidden behind time series in complex systems can emerge upon analysing<br />

them in a time domain, termed natural time, that has been introduced recently [P. Varotsos, N. Sarlis<br />

and E. Skordas, Practica of Athens Academy 76, 294 (2001); ibid Phys. Rev. E 66, 011902 (2002)]. This<br />

analysis enables the study of the dynamical evolution of a complex system and identifies when the<br />

system enters the critical stage. Relevant examples have been published in a large variety of fields<br />

including biology, physics and earth sciences. As a first example, we mention the analysis of the<br />

electrocardiograms which may herald a cardiac arrest [P. Varotsos, N. Sarlis, E. Skordas and M.<br />

Lazaridou Phys. Rev. E 70, 011106 (2004); ibid 71, 011110 (2005)]. Second, natural time analysis<br />

enables the distinction between the precursory electric signals, termed Seismic Electric Signals (SES)<br />

and similar looking electric noise emitted from artificial (man-made) sources. Third, the data of<br />

avalanches of the penetration of magnetic flux into thin films of type II (high-Tc) superconductors as<br />

well as those of a three dimensional pile of rice (which are typical systems that have been suggested as<br />

following the so-called Self Organised Criticality) getting progressively closer to the critical state conform<br />

to the features suggested, on the basis of natural time, to describe critical dynamics [N. Sarlis, P.<br />

Varotsos and E. Skordas, Phys. Rev. B 73, 054504 (2006)]. Fourth, the analysis of seismicity subsequent<br />

to the SES detection allows the determination of the occurrence time of the impending strong<br />

earthquake(s) within a narrow range around a few days at the most [P. Varotsos, N. Sarlis and E.<br />

Skordas Practica Athens Acad. 76, 294 (2001); ibid Acta Geophys. Pol. 50, 337 (2002)]. Details on the<br />

latter procedure, which has been applied to recent strong earthquakes in Greece [P. Varotsos, Proc.<br />

Jpn. Acad. Ser. B 82, 86, 2006; P. Varotsos, N. Sarlis, E. Skordas, H. Tanaka amd M. Lazaridou, Phys.<br />

Rev. E 73, 031114 (2006); ibid Phys. Rev. E 74, 021123 (2006)], the SES activities of which have been<br />

identified and submitted for publication well in advance, are presented<br />

Keywords: natural time, complex time series, time window of strong eqs

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