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Scaling characteristics of ULF geomagnetic fields at the Guam seismoactive area and their dynamics in relation to the earthquake

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Figure

Fig. 1. An example of the daily record of geomagnetic field vari-ations (H, D, Z components) at the Guam observatory (1 April1993)
Fig. 2. An example of the ULF data processing by the FFT method.the power spectrum. The best-fit line represents the spectrum slopeβ(a) an original signal; (b) the zero mean signal without trend; (c)
Fig. 4.dom noise (the Guam ULF magnetic data along one-hour local noon intervalnals examined:Examples of simulated  (a–c) and observational (d) sig- (a) the persistent noise with Hu = 0.9; (b) ran-Hu = 0.5); (c) antipersistent noise with Hu = 0.1; (d)(12:00–13:00 LT) of 1 April 1993.
Table 1. Results of test calculations of the fractal dimensions D0 and spectral exponents β for simulated noise shown in Fig
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