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Earthquake sources radiate non-time-harmonic waves, especially at low frequencies below the corner frequency.
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The filter works by having a clock signal that has a frequency 100 times of the corner frequency.
Example of estimation of the corner frequency.
Solid line in the left figure shows the corner frequency.
Gray circles denote 8300 earthquakes used for estimates of corner frequencies, while colored circles represent 4718 out of 8300 earthquakes for which the corner frequency could be estimated.
We estimated the corner frequency of the omega-square model in the following way.
All of the earthquakes have four or more stations available for the corner frequency estimation.
We therefore conclude that the peak pulse corresponds to the rupture estimated by the corner frequency.
Fig. 3 Plot of seismic moment M 0 against the corner frequency f c.
To estimate the corner frequency, we selected stations located at an intermediate distance from the source.
Station codes with underlines are the stations used in the corner frequency analysis.
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