382 research outputs found
The fluctuations, under time reversal, of the natural time and the entropy distinguish similar looking electric signals of different dynamics
We show that the scale dependence of the fluctuations of the natural time
itself under time reversal provides a useful tool for the discrimination of
seismic electric signals (critical dynamics) from noises emitted from man made
sources as well as for the determination of the scaling exponent. We present
recent data of electric signals detected at the Earth's surface, which confirm
that the value of the entropy in natural time as well as its value under time
reversal are smaller than that of the entropy of a "uniform" distribution.Comment: 29 pages including 24 figure and 1 Tabl
Comment on "Effects of Thickness on the Spin Susceptibility of the Two Dimensional Electron Gas"
A comment on a recent paper (PRL {\bf 94}, 226405 (2005)) by S. De Palo, M.
Botti, S. Moroni, and Gaetano Senatore
Identifying the occurrence time of an impending mainshock: A very recent case
The procedure by means of which the occurrence time of an impending mainshock
can be identified by analyzing in natural time the seismicity in the candidate
area subsequent to the recording of a precursory Seismic Electric Signals (SES)
activity is reviewed. Here, we report the application of this procedure to an
Mw5.4 mainshock that occurred in Greece on 17 November 2014 and was strongly
felt in Athens. This mainshock (which is pretty rare since it is the strongest
in that area for more than half a century) was preceded by an SES activity
recorded on 27 July 2014 and the results of the natural time analysis reveal
that the system approached the critical point (mainshock occurrence) early in
the morning on 15 November 2014. Similar SES activities that have been recently
recorded are also presented. Furthermore, in a Note we discuss the case of the
Mw5.3 earthquake that was also strongly felt in Athens on 19 July 2019.Comment: An early version of this paper appeared in Earthq. Sci. 28 (2015)
215-222 [doi:10.1007/s11589-015-0122-3], whereas in the present version new
data collected during 2019 and 2020 have been added. 8 pages, 11 figure
Natural entropy fluctuations discriminate similar looking electric signals emitted from systems of different dynamics
Complexity measures are introduced, that quantify the change of the natural
entropy fluctuations at different length scales in time-series emitted from
systems operating far from equilibrium. They identify impending sudden cardiac
death (SD) by analyzing fifteen minutes electrocardiograms, and comparing to
those of truly healthy humans (H). These measures seem to be complementary to
the ones suggested recently [Phys. Rev. E {\bf 70}, 011106 (2004)] and
altogether enable the classification of individuals into three categories: H,
heart disease patients and SD. All the SD individuals, who exhibit critical
dynamics, result in a common behavior.Comment: Published in Physical Review
Entropy of seismic electric signals: Analysis in natural time under time-reversal
Electric signals have been recently recorded at the Earth's surface with
amplitudes appreciably larger than those hitherto reported. Their entropy in
natural time is smaller than that, , of a ``uniform'' distribution. The
same holds for their entropy upon time-reversal. This behavior, as supported by
numerical simulations in fBm time series and in an on-off intermittency model,
stems from infinitely ranged long range temporal correlations and hence these
signals are probably Seismic Electric Signals (critical dynamics). The entropy
fluctuations are found to increase upon approaching bursting, which reminds the
behavior identifying sudden cardiac death individuals when analysing their
electrocardiograms.Comment: 7 pages, 4 figures, copy of the revised version submitted to Physical
Review Letters on June 29,200
Entropy in the natural time-domain
A surrogate data analysis is presented, which is based on the fluctuations of
the ``entropy'' defined in the natural time-domain [Phys. Rev. E {\bf 68},
031106, 2003]. This entropy is not a static one as, for example, the Shannon
entropy. The analysis is applied to three types of time-series, i.e., seismic
electric signals, ``artificial'' noises and electrocardiograms, and
``recognizes'' the non-Markovianity in all these signals. Furthermore, it
differentiates the electrocardiograms of healthy humans from those of the
sudden cardiac death ones. If and denote the
standard deviation when calculating the entropy by means of a time-window
sweeping through the original data and the ``shuffled'' (randomized) data,
respectively, it seems that the ratio plays a
key-role. The physical meaning of is investigated.Comment: Published in Physical Review
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