Affiliation(s)
1. Geological Institute of Romania, Caransebes str. 1, 012271, Bucharest, Romania
2. Faculty of Transportation, University POLITEHNICA of Bucharest, Splaiul Independenei str. 313, 060042 Bucharest, Romania
ABSTRACT
The purpose of this study was to analyze the
associated spectrum of geomagnetic field, frequencies intensity and the time of
occurrence. We calculated the variation of the correlation coefficients, with
mobile windows of various sizes, for the recorded magnetic components at
different latitudes and latitudes. The observatories we included in our study
are USA (Surlari), HON (Honolulu), SBA (Scott Base), KAK (Kakioka), THY
(Tihany), UPS (Uppsala), WNG (Wingst) and Yellowknife (YKC). We used the data of
these observatories from International Real-time Magnetic Observatory Network
(INTERMAGNET)
for the geomagnetic storm from October 28-31, 2003. We have used for this
purpose a series of filtering algorithms, spectral analysis and wavelet with
different mother functions at different levels. In the paper, we show the
Fourier and wavelet analysis of geomagnetic data recorded at different
observatories regarding geomagnetic storms. Fourier analysis hightlights
predominant frequencies of magnetic field components. Wavelet analysis provides
information about the frequency ranges of magnetic fields, which contain long
time intervals for medium frequency information and short time intervals for
highlight frequencies, details of the analyzed signals. Also, the wavelet
analysis allows us to decompose geomagnetic signals in different waves. The
analyses
presented are significant for the studies of the geomagnetic
storm. The data for the next days after the storm showed a mitigation of the
perturbations and a transition to quiet days of the geomagnetic field.
KEYWORDS
Fourier
spectral deconvolution, wavelet analyses, geomagnetic disturbances, geomagnetic observatories.
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