Fig. 7From: Linking the flow-induced tremor model to the seismological observation: application to the deep harmonic tremor at Hakone volcano, JapanComparison of the calculated waveforms assuming the one-dimensional attenuation model based on the result by Kashiwagi et al. (2020) and the observations at OMZ, KIN, and TNM stations. The meaning of each column is same as that in Fig. 6Back to article page