Nonlinear Processes in Geophysics
Nonlinear Processes in Geophysics
NPG
Articles | Volume 9, issue 5/6
Articles | Volume 9, issue 5/6
https://doi.org/10.5194/npg-9-419-2002
© Author(s) 2002. This work is licensed under
the Creative Commons Attribution-NonCommercial-ShareAlike 2.5 License.
Special issue:
https://doi.org/10.5194/npg-9-419-2002
© Author(s) 2002. This work is licensed under
the Creative Commons Attribution-NonCommercial-ShareAlike 2.5 License.
Articles | Volume 9, issue 5/6
31 Dec 2002
31 Dec 2002

Fractal time statistics of AE-index burst waiting times: evidence of metastability

G. Consolini and P. De Michelis

Abstract. Recent observations and analyses evidenced that the magnetotail, as well as the magnetospheric dynamics are characterised by a scale-free behaviour and intermittence. These results, along with numerical simulations on cellular automata, suggest that the observed scale-invariance may be due to forced and/or self-organised criticality (FSOC), meaning that the magnetotail operates near a marginally stable state (Chang, 1999). On the other hand, it was underlined that a complex magnetic field topology in the geotail regions may play a relevant role in the impulsive energy relaxation (Consolini and Chang, 2001.

How to cite. Consolini, G. and De Michelis, P.: Fractal time statistics of AE-index burst waiting times: evidence of metastability, Nonlin. Processes Geophys., 9, 419–423, https://doi.org/10.5194/npg-9-419-2002, 2002.