2009
DOI: 10.5194/angeo-27-569-2009
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Multifractal analysis of low-latitude geomagnetic fluctuations

Abstract: Abstract.The technique of large deviation multifractal spectrum has shown that the high-latitude (77.5 • N, 69.2 • W) geomagnetic fluctuations can be described from direct dissipation process or loading-unloading regimes of the solar windmagnetosphere coupling. In this paper, we analyze the Hcomponent of low-latitude (22.4 • S, 43.6 • W) geomagnetic field variability observed during the month of July 2000 at the Geomagnetic Observatory, Vassouras, RJ, Brazil. The variability pattern during this period is a mix… Show more

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Cited by 23 publications
(13 citation statements)
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“…Choosing typical parameters values for the p-model (Bolzan et al 2009) we use an algorithm to fit the experimental and theoretical data. The results are shown in Fig.…”
Section: Data Analysis Interpretation and Discussionmentioning
confidence: 99%
“…Choosing typical parameters values for the p-model (Bolzan et al 2009) we use an algorithm to fit the experimental and theoretical data. The results are shown in Fig.…”
Section: Data Analysis Interpretation and Discussionmentioning
confidence: 99%
“…It is noteworthy that, although the w parameters are very closed (w = 1.16 during the CME and w = 1.19 after the CME), the values for α max are slightly different: α max = 1.12 (during the CME) and α max = 0.91 (after the CME). In our previous work (Bolzan et al, 2009c), by using the H-component of the geomagnetic field obtained in Brazil, we found greatest values of the α max for time series with strong presence of the deterministic phenomena, such as solar daily variation on geomagnetic field. This fact indicates that the presence of the strong and deterministic phenomena Fig.…”
Section: Resultsmentioning
confidence: 99%
“…The correlation level can be formulated either in simple frequency form or in cumulative frequency form, usually as a rank-size type relationship, which is preferred in this case, when the focus is on the rarer or larger events that dominate the distribution of U (t) for different temporal scales. There are many other post-analytical properties as Kullback-Leibler divergence [11], fractal-like dimensions [12], Kolmogorov-Sinai entropy [12], Hurst exponent [12], singularity spectral index [13], etc, which can be addressed for GNL with κ = 2 (1D time-series case U (t)). Although the quantity of post-analytical measures is an open set μ 1 , .…”
Section: The Post-analytical Parameters μ Pmentioning
confidence: 99%