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A CMM is a precision measurement tool which uses a ruby probe to stroke over the surface of a component, recording data as it does.
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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.
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.
Figure 10 Simulated and observed RMS envelopes of the vertical component recorded at the N.NSHH and N.HYNH stations.
Figure 4 shows the stacked RMS envelopes of the vertical component recorded at four Hi-net stations with average epicentral distances of 100 to 150 km.
To avoid complications associated with later arrivals, we apply the back-projection technique to the first P-wave arrivals using the vertical component recorded at above stations.
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