Fig. 3From: Identification of infrasonic and seismic components of tremors in single-station records: application to the 2013 and 2018 events at Ioto Island, JapanPower spectral features of tremors (magenta) and background noise (black). The symbols show the values of the meaningful frequency bands selected by step ⑤ of the text. a, b The upper magenta line with the upward triangles is \(P_W\), and the associated black line is \(P_W^b\), on the left axis. The lower magenta line with inverted triangles is \(P_P\), and the associated black line is \(P_P^b\), on the right axis. c, d The spectral amplitude ratio between seismic record and infrasonic record, \((w/p)_{\text{obs}}\), as a function of frequency. The horizontal dashed line indicates the theoretical value for the ground-to-atmosphere wave calculated by Eq. (2) with \(\alpha\) = 340 m/s and \(\rho\) = 1.16 kg/m\(^3\)Back to article page