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As can be seen in the figure, all of the reference records, except for the vertical component record at TMR, agree well with those at TYS.
Horizontal component record (Figure 9b) also displays the phase with similar apparent velocity but different intercept time at around 7.1 s, which is interpreted as a P to S converted wave.
The highest peak ground velocity (PGV, 99 cm/s) was given by the NS component record at TVU, and the peak amplitude of the horizontal components was 108 cm/s at this station.
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This component records all subscriptions in the system.
Fig. 3 Examples of waveforms in the vertical component recorded by the high-frequency observation network.
(b) Band-pass filtered (1 8 Hz) waveforms of the vertical component recorded at the TOGI station.
(b) Band-pass filtered (1 8 Hz) waveforms of the vertical component recorded at the wt53 station.
Also at TKD, NS component records prior to 2008 showed seismometer response errors.
We measured peak-to-peak amplitudes of the cervical N13 component (recorded under the active Cv5 electrode), and the cortical N20-P25 and P25-N33 components (recorded under the active C3′ scalp electrode).
Figure 6 Plot over two consecutive hours of the vertical velocity component recorded at station V.MKJA on 9 January 2005.
Figure 3 Filtered velocity seismograms of the vertical component recorded at the N.NSHH station for all earthquakes.
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