Data di Pubblicazione:
2002
Abstract:
We show at work a technique of scaling detection based on evaluating the
Shannon entropy of the diffusion process obtained by converting the time
series under study into trajectories. This method, called diffusion
entropy, affords information that cannot be derived from the direct
evaluation of waiting times. We apply this method to the analysis of the
distribution of time distance t between two nearest-neighbor solar flares.
This traditional part of the analysis is based on the direct evaluation of
the distribution function c( t), or of the probability C( t), that no time
distance smaller than a given t is found. We adopt the paradigm of the
inverse power-law behavior, and we focus on the determination of the
inverse power index m, without ruling out different asymptotic properties
that might be revealed, at larger scales, with the help of richer
statistics. We then use the DE method, with three different walking rules,
and we focus on the regime of transition to scaling.
This regime of transition and the value of the scaling parameter itself,
d, depends on the walking rule adopted, a property of interest to shed
light on the slow process of transition from dynamics to thermodynamics
often occurring under anomalous statistical conditions. With the first two
rules the transition regime occurs through-out a large time interval, and
the information contained in the time series is transmitted, to a great
extent, to it, as well as to the scaling regime. By using the third rule,
on the contrary, the same information is essentially conveyed to the
scaling regime, which, in fact, emerges very quickly after a fast
transition process. We show that the DE method not only causes to emerge
the long-range correlation with a given m,3, and so a basin of
attraction different from the ordinary Gaussian one, but it also reveals
the presence of memory effects induced by the time dependence of the solar
flare rate. When this memory is annihilated by shuffling, the scaling
parameter d is shown to fit the theoretically expected function of u. All
this leads us to the compelling conclusion that u=2.138+-0.01.
Tipologia CRIS:
01.01 Articolo in rivista
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