2003, Vol.6, No.1, pp.524-533
Geomagnetic fluctuations observed on the ground are closely
interrelated to external magnetic fields of ionospheric and
magnetospheric origins. Assuming that the magnetosphere
evolves in a coherent and organized way, a low-dimensional
analogue model was studied to understand its dynamics.
Theoretical studies have shown that the magnetosphere
belongs to the class of dissipative chaotic systems. Following
on from this description of the magnetosphere, we propose an
innovative method for chaotic dynamical system identification from
measured data. We describe geomagnetic activity in terms of a relatively
simple nonlinear dynamical analogue model, whose parameters are determined
in such a way that the simulated output signal synchronizes with the data acquired from
the magnetic monitoring network at Etna volcano.
Key words:
geomagnetic field, synchronization, modeling, genetic algorithm
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