Wavelet analysis on paleomagnetic (and computer simulated) VGP time series

We present Continuous Wavelet Transform (CWT) data analysis of Virtual Geomagnetic Pole (VGP) latitude
 time series. The analyzed time series are sedimentary paleomagnetic and geodynamo simulated data. Two mother
 wavelets (the Morlet function and the first derivative of a Gaussian f...

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Main Authors: A. Siniscalchi, G. Giberti, S. Lorito, M. Iorio
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/3429
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author A. Siniscalchi
G. Giberti
S. Lorito
M. Iorio
author_facet A. Siniscalchi
G. Giberti
S. Lorito
M. Iorio
author_sort A. Siniscalchi
collection DOAJ
description We present Continuous Wavelet Transform (CWT) data analysis of Virtual Geomagnetic Pole (VGP) latitude
 time series. The analyzed time series are sedimentary paleomagnetic and geodynamo simulated data. Two mother
 wavelets (the Morlet function and the first derivative of a Gaussian function) are used in order to detect features
 related to the spectral content as well as polarity excursions and reversals. By means of the Morlet wavelet,
 we estimate both the global spectrum and the time evolution of the spectral content of the paleomagnetic data
 series. Some peaks corresponding to the orbital components are revealed by the spectra and the local analysis
 helped disclose their statistical significance. Even if this feature could be an indication of orbital influence on
 geodynamo, other interpretations are possible. In particular, we note a correspondence of local spectral peaks
 with the appearance of the excursions in the series. The comparison among the paleomagnetic and simulated
 spectra shows a similarity in the high frequency region indicating that their degree of regularity is analogous. By
 means of Gaussian first derivative wavelet, reversals and excursions of polarity were sought. The analysis was
 performed first on the simulated data, to have a guide in understanding the features present in the more complex
 paleomagnetic data. Various excursions and reversals have been identified, despite of the prevalent normality of
 the series and its inherent noise. The found relative chronology of the paleomagnetic data reversals was compared
 with a coeval global polarity time scale (Channel et al., 1995). The relative lengths of polarity stability intervals
 are found similar, but a general shift appears between the two scales, that could be due to the datation uncertainties
 of the Hauterivian/Barremian boundary.
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spelling doaj.art-aed012c82a654338b76742a453162eb12022-12-22T02:44:24ZengIstituto Nazionale di Geofisica e Vulcanologia (INGV)Annals of Geophysics1593-52132037-416X2003-06-0146310.4401/ag-3429Wavelet analysis on paleomagnetic (and computer simulated) VGP time seriesA. SiniscalchiG. GibertiS. LoritoM. IorioWe present Continuous Wavelet Transform (CWT) data analysis of Virtual Geomagnetic Pole (VGP) latitude
 time series. The analyzed time series are sedimentary paleomagnetic and geodynamo simulated data. Two mother
 wavelets (the Morlet function and the first derivative of a Gaussian function) are used in order to detect features
 related to the spectral content as well as polarity excursions and reversals. By means of the Morlet wavelet,
 we estimate both the global spectrum and the time evolution of the spectral content of the paleomagnetic data
 series. Some peaks corresponding to the orbital components are revealed by the spectra and the local analysis
 helped disclose their statistical significance. Even if this feature could be an indication of orbital influence on
 geodynamo, other interpretations are possible. In particular, we note a correspondence of local spectral peaks
 with the appearance of the excursions in the series. The comparison among the paleomagnetic and simulated
 spectra shows a similarity in the high frequency region indicating that their degree of regularity is analogous. By
 means of Gaussian first derivative wavelet, reversals and excursions of polarity were sought. The analysis was
 performed first on the simulated data, to have a guide in understanding the features present in the more complex
 paleomagnetic data. Various excursions and reversals have been identified, despite of the prevalent normality of
 the series and its inherent noise. The found relative chronology of the paleomagnetic data reversals was compared
 with a coeval global polarity time scale (Channel et al., 1995). The relative lengths of polarity stability intervals
 are found similar, but a general shift appears between the two scales, that could be due to the datation uncertainties
 of the Hauterivian/Barremian boundary.http://www.annalsofgeophysics.eu/index.php/annals/article/view/3429CWTVGPgeodynamo simulationsexcursions and reversalsEarth's orbital parameters
spellingShingle A. Siniscalchi
G. Giberti
S. Lorito
M. Iorio
Wavelet analysis on paleomagnetic (and computer simulated) VGP time series
Annals of Geophysics
CWT
VGP
geodynamo simulations
excursions and reversals
Earth's orbital parameters
title Wavelet analysis on paleomagnetic (and computer simulated) VGP time series
title_full Wavelet analysis on paleomagnetic (and computer simulated) VGP time series
title_fullStr Wavelet analysis on paleomagnetic (and computer simulated) VGP time series
title_full_unstemmed Wavelet analysis on paleomagnetic (and computer simulated) VGP time series
title_short Wavelet analysis on paleomagnetic (and computer simulated) VGP time series
title_sort wavelet analysis on paleomagnetic and computer simulated vgp time series
topic CWT
VGP
geodynamo simulations
excursions and reversals
Earth's orbital parameters
url http://www.annalsofgeophysics.eu/index.php/annals/article/view/3429
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AT ggiberti waveletanalysisonpaleomagneticandcomputersimulatedvgptimeseries
AT slorito waveletanalysisonpaleomagneticandcomputersimulatedvgptimeseries
AT miorio waveletanalysisonpaleomagneticandcomputersimulatedvgptimeseries