Multifractality in local geomagnetic field at Etna volcano, Sicily (southern Italy)

We applied the Multifractal Detrended Fluctuation Analysis (MF-DFA), which allows to detect multifractality in nonstationary signals, to the hourly means of local geomagnetic field recorded at Mt. Etna volcano (southern Italy). We studied the signal measured at one geomagnetic station, installed at...

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Main Authors: G. Currenti, C. del Negro, V. Lapenna, L. Telesca
Format: Article
Language:English
Published: Copernicus Publications 2005-01-01
Series:Natural Hazards and Earth System Sciences
Online Access:http://www.nat-hazards-earth-syst-sci.net/5/555/2005/nhess-5-555-2005.pdf
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author G. Currenti
C. del Negro
V. Lapenna
L. Telesca
author_facet G. Currenti
C. del Negro
V. Lapenna
L. Telesca
author_sort G. Currenti
collection DOAJ
description We applied the Multifractal Detrended Fluctuation Analysis (MF-DFA), which allows to detect multifractality in nonstationary signals, to the hourly means of local geomagnetic field recorded at Mt. Etna volcano (southern Italy). We studied the signal measured at one geomagnetic station, installed at the summit of volcano, which was characterized by a strong eruption on 27 October 2002. We analyzed two frames of signals, one measured before the eruption and the other after, in order to evaluate dynamical changes induced by the eruptive event. Our findings show that: i) the geomagnetic time series is multifractal; ii) the multifractal degree of the signal decreases after the occurrence of eruption. This study aims to propose another approach to investigate the complex dynamics of volcano-related geomagnetic field.
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spelling doaj.art-f065e4dbb346436b92b5580a43991f922022-12-21T22:59:03ZengCopernicus PublicationsNatural Hazards and Earth System Sciences1561-86331684-99812005-01-0154555559Multifractality in local geomagnetic field at Etna volcano, Sicily (southern Italy)G. CurrentiC. del NegroV. LapennaL. TelescaWe applied the Multifractal Detrended Fluctuation Analysis (MF-DFA), which allows to detect multifractality in nonstationary signals, to the hourly means of local geomagnetic field recorded at Mt. Etna volcano (southern Italy). We studied the signal measured at one geomagnetic station, installed at the summit of volcano, which was characterized by a strong eruption on 27 October 2002. We analyzed two frames of signals, one measured before the eruption and the other after, in order to evaluate dynamical changes induced by the eruptive event. Our findings show that: i) the geomagnetic time series is multifractal; ii) the multifractal degree of the signal decreases after the occurrence of eruption. This study aims to propose another approach to investigate the complex dynamics of volcano-related geomagnetic field.http://www.nat-hazards-earth-syst-sci.net/5/555/2005/nhess-5-555-2005.pdf
spellingShingle G. Currenti
C. del Negro
V. Lapenna
L. Telesca
Multifractality in local geomagnetic field at Etna volcano, Sicily (southern Italy)
Natural Hazards and Earth System Sciences
title Multifractality in local geomagnetic field at Etna volcano, Sicily (southern Italy)
title_full Multifractality in local geomagnetic field at Etna volcano, Sicily (southern Italy)
title_fullStr Multifractality in local geomagnetic field at Etna volcano, Sicily (southern Italy)
title_full_unstemmed Multifractality in local geomagnetic field at Etna volcano, Sicily (southern Italy)
title_short Multifractality in local geomagnetic field at Etna volcano, Sicily (southern Italy)
title_sort multifractality in local geomagnetic field at etna volcano sicily southern italy
url http://www.nat-hazards-earth-syst-sci.net/5/555/2005/nhess-5-555-2005.pdf
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AT cdelnegro multifractalityinlocalgeomagneticfieldatetnavolcanosicilysouthernitaly
AT vlapenna multifractalityinlocalgeomagneticfieldatetnavolcanosicilysouthernitaly
AT ltelesca multifractalityinlocalgeomagneticfieldatetnavolcanosicilysouthernitaly