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This file shows the particle motion and apparent velocity for the waveform trace of volcanic tremor.
Cross-correlation coefficients as a function of IYG delay against TYS are on the lower side of each waveform trace.
Blue and black dots on the lower side of each waveform trace are lag time errors, τ error, for TMR and the others, respectively.
The whole waveform trace lasted 40 s, and in most cases, the envelop, duration, and PGA of synthetic ground motions matched the observed waveforms well.
The waveform trace is plotted on each of the plots (black dotted line) so that peak positions during the waveform can be analyzed.
The mean velocity of PVVel and HAPI were calculated automatically by the machine after the waveform trace for three cardiac cycles were obtained.
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We repeated this process until the CCs of all waveform traces were larger than 0.5.
A manual solution is then obtained by inversion using the selected waveform traces.
Each automatic solution is manually checked, and the waveform traces including non-seismic pulses and long-period noise are discarded.
In this example, three-component waveform traces at station LUBP were contaminated by large non-seismic pulses.
Waveform traces within the absorbing layer are shown as green curves, and traces at the center of the model are shown as thick red curves.
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Since I tried Ludwig back in 2017, I have been constantly using it in both editing and translation. Ever since, I suggest it to my translators at ProSciEditing.

Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com