Some new approaches to the study of the Earth's magnetic field reversals

Paleomagnetic studies clearly show that the polarity of the magnetic fi eld has been subject to reversals. It is
 generally assumed that polarity intervals are exponentially distributed. Here, the geomagnetic polarity reversal
 record, for the past 166 Ma, is analysed and a new appro...

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Main Authors: G. Consolini, P. De Michelis
Format: Article
Language:English
Published: Istituto Nazionale di Geofisica e Vulcanologia (INGV) 2003-06-01
Series:Annals of Geophysics
Subjects:
Online Access:http://www.annalsofgeophysics.eu/index.php/annals/article/view/4372
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author G. Consolini
P. De Michelis
author_facet G. Consolini
P. De Michelis
author_sort G. Consolini
collection DOAJ
description Paleomagnetic studies clearly show that the polarity of the magnetic fi eld has been subject to reversals. It is
 generally assumed that polarity intervals are exponentially distributed. Here, the geomagnetic polarity reversal
 record, for the past 166 Ma, is analysed and a new approach to the study of the reversals is presented. In detail, the
 occurrence of 1/f-noise in the Power Spectral Density (PSD), relative to geomagnetic fi eld reversals, the existence
 of a Zipf's law behaviour for the cumulative distribution of polarity intervals, and the occurrence of punctuated
 equilibrium, as shown by a sort of Devil's staircase for the reversal time series, are investigated. Our results give
 a preliminary picture of the dynamical state of the geomagnetic dynamo suggesting that the geodynamo works in
 a marginally stable out-of-equilibrium confi guration, and that polarity reversals are equivalent to a sort of phase
 transition between two metastable states.
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spelling doaj.art-382ad863f5b64d32bec1788eca9fc9b62022-12-22T01:28:50ZengIstituto Nazionale di Geofisica e Vulcanologia (INGV)Annals of Geophysics1593-52132037-416X2003-06-0146410.4401/ag-4372Some new approaches to the study of the Earth's magnetic field reversalsG. ConsoliniP. De MichelisPaleomagnetic studies clearly show that the polarity of the magnetic fi eld has been subject to reversals. It is
 generally assumed that polarity intervals are exponentially distributed. Here, the geomagnetic polarity reversal
 record, for the past 166 Ma, is analysed and a new approach to the study of the reversals is presented. In detail, the
 occurrence of 1/f-noise in the Power Spectral Density (PSD), relative to geomagnetic fi eld reversals, the existence
 of a Zipf's law behaviour for the cumulative distribution of polarity intervals, and the occurrence of punctuated
 equilibrium, as shown by a sort of Devil's staircase for the reversal time series, are investigated. Our results give
 a preliminary picture of the dynamical state of the geomagnetic dynamo suggesting that the geodynamo works in
 a marginally stable out-of-equilibrium confi guration, and that polarity reversals are equivalent to a sort of phase
 transition between two metastable states.http://www.annalsofgeophysics.eu/index.php/annals/article/view/4372Earth's magnetic fieldgeomagnetic reversalstime series analysis
spellingShingle G. Consolini
P. De Michelis
Some new approaches to the study of the Earth's magnetic field reversals
Annals of Geophysics
Earth's magnetic field
geomagnetic reversals
time series analysis
title Some new approaches to the study of the Earth's magnetic field reversals
title_full Some new approaches to the study of the Earth's magnetic field reversals
title_fullStr Some new approaches to the study of the Earth's magnetic field reversals
title_full_unstemmed Some new approaches to the study of the Earth's magnetic field reversals
title_short Some new approaches to the study of the Earth's magnetic field reversals
title_sort some new approaches to the study of the earth s magnetic field reversals
topic Earth's magnetic field
geomagnetic reversals
time series analysis
url http://www.annalsofgeophysics.eu/index.php/annals/article/view/4372
work_keys_str_mv AT gconsolini somenewapproachestothestudyoftheearthsmagneticfieldreversals
AT pdemichelis somenewapproachestothestudyoftheearthsmagneticfieldreversals