Fig. 8.From: Barometric and magnetic observations of vertical acoustic resonance and resultant generation of field-aligned current associated with earthquakesPower spectral density of the magnetic variation at Aso station. The spectra of the Horizontal (H) and Declination (D) components are shown. Two peaks in the H component at 275 s and 230 s appear just after the origin time, which correspond to the fundamental, and the first overtone, of the resonance modes, respectively. A small peak at 250 s also appears in the D component, which may correspond to the peak seen in the barometric data obtained at Shigaraki.Back to article page