The BH channels waveforms were extracted from the CWB and then
displayed. Since the sensor was a Trillium, they were rotated to
the internal UVW channels using the gsac command rot3
to uvwtril
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Original traces. The large DC offset makes it
seem as if the E and Z channels are constant. |
Result of converting to UVW. Here we see that
the U channel has the large DC offset |
A remote centering command was issued to the sensor. The latter
part of this seismogram display shows that the centering resolved
the large offset and that traces no longer exhibit the long period
noise.
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