Intermittency and multifractional Brownian character of geomagnetic time series

The Earth's magnetosphere exhibits a complex behavior in response to the solar wind conditions. This behavior, which is described in terms of mutifractional Brownian motions, could be the consequence of the occurrence of dynamical phase transitions. On the other hand, it has been shown that the...

Full description

Bibliographic Details
Main Authors: G. Consolini, R. De Marco, P. De Michelis
Format: Article
Language:English
Published: Copernicus Publications 2013-07-01
Series:Nonlinear Processes in Geophysics
Online Access:http://www.nonlin-processes-geophys.net/20/455/2013/npg-20-455-2013.pdf
id doaj-05f587cf630f48738895fe0a2d5f56b5
record_format Article
spelling doaj-05f587cf630f48738895fe0a2d5f56b52020-11-24T23:11:10ZengCopernicus PublicationsNonlinear Processes in Geophysics1023-58091607-79462013-07-0120445546610.5194/npg-20-455-2013Intermittency and multifractional Brownian character of geomagnetic time seriesG. ConsoliniR. De MarcoP. De MichelisThe Earth's magnetosphere exhibits a complex behavior in response to the solar wind conditions. This behavior, which is described in terms of mutifractional Brownian motions, could be the consequence of the occurrence of dynamical phase transitions. On the other hand, it has been shown that the dynamics of the geomagnetic signals is also characterized by intermittency at the smallest temporal scales. Here, we focus on the existence of a possible relationship in the geomagnetic time series between the multifractional Brownian motion character and the occurrence of intermittency. In detail, we investigate the multifractional nature of two long time series of the horizontal intensity of the Earth's magnetic field as measured at L'Aquila Geomagnetic Observatory during two years (2001 and 2008), which correspond to different conditions of solar activity. We propose a possible double origin of the intermittent character of the small-scale magnetic field fluctuations, which is related to both the multifractional nature of the geomagnetic field and the intermittent character of the disturbance level. Our results suggest a more complex nature of the geomagnetic response to solar wind changes than previously thought.http://www.nonlin-processes-geophys.net/20/455/2013/npg-20-455-2013.pdf
collection DOAJ
language English
format Article
sources DOAJ
author G. Consolini
R. De Marco
P. De Michelis
spellingShingle G. Consolini
R. De Marco
P. De Michelis
Intermittency and multifractional Brownian character of geomagnetic time series
Nonlinear Processes in Geophysics
author_facet G. Consolini
R. De Marco
P. De Michelis
author_sort G. Consolini
title Intermittency and multifractional Brownian character of geomagnetic time series
title_short Intermittency and multifractional Brownian character of geomagnetic time series
title_full Intermittency and multifractional Brownian character of geomagnetic time series
title_fullStr Intermittency and multifractional Brownian character of geomagnetic time series
title_full_unstemmed Intermittency and multifractional Brownian character of geomagnetic time series
title_sort intermittency and multifractional brownian character of geomagnetic time series
publisher Copernicus Publications
series Nonlinear Processes in Geophysics
issn 1023-5809
1607-7946
publishDate 2013-07-01
description The Earth's magnetosphere exhibits a complex behavior in response to the solar wind conditions. This behavior, which is described in terms of mutifractional Brownian motions, could be the consequence of the occurrence of dynamical phase transitions. On the other hand, it has been shown that the dynamics of the geomagnetic signals is also characterized by intermittency at the smallest temporal scales. Here, we focus on the existence of a possible relationship in the geomagnetic time series between the multifractional Brownian motion character and the occurrence of intermittency. In detail, we investigate the multifractional nature of two long time series of the horizontal intensity of the Earth's magnetic field as measured at L'Aquila Geomagnetic Observatory during two years (2001 and 2008), which correspond to different conditions of solar activity. We propose a possible double origin of the intermittent character of the small-scale magnetic field fluctuations, which is related to both the multifractional nature of the geomagnetic field and the intermittent character of the disturbance level. Our results suggest a more complex nature of the geomagnetic response to solar wind changes than previously thought.
url http://www.nonlin-processes-geophys.net/20/455/2013/npg-20-455-2013.pdf
work_keys_str_mv AT gconsolini intermittencyandmultifractionalbrowniancharacterofgeomagnetictimeseries
AT rdemarco intermittencyandmultifractionalbrowniancharacterofgeomagnetictimeseries
AT pdemichelis intermittencyandmultifractionalbrowniancharacterofgeomagnetictimeseries
_version_ 1725605443723591680