Determination of earthquake magnitudes using duration of
high-frequency energy radiation and maximum displacement amplitudes: application
to the October 28, south of Masset, Canada earthquake
Tatsuhiko Hara
International
Building Research Institute
We developed a method to determine
earthquake magnitudes using the following formula (Hara, 2007a, b):
where M is an earthquake magnitude, is the maximum
displacement during high-frequency energy radiation from the arrival time of a
P-wave, is the epicentral distance, is duration of
high-frequency energy radiation. The duration of high-frequency energy
radiation can be estimated by band-pass filtering of first arriving P-waves (e.g.,
Hara, 2007a). are 0.79, 0.83, 0.69, and 6.47, respectively (the units of were m, km, and s,
respectively).
We applied this method to the October 28, south of Masset,
Canada earthquake (the origin time: 03:04:10 UTC; the location 52.769‹N, 131.927‹W
after USGS). Figure 1 shows an example of measurements of high-frequency energy
radiation. The estimated duration is 62.2
sec. The estimated magnitude using the above formula is 7.78, which is
consistent with Mw 7.7 from the Global CMT solution and Mw
7.8 from USGS WPhase Moment Tensor Solution.
Fig.
1. An example of
measurements of high frequency energy radiation. The upper, middle and lower
traces are an observed seismogram, the squares of the band-pass (2-4 Hz)
filtered seismogram, and its smoothed time series (normalized by the maximum
value), respectively. gAh and gFh in the lower trace denote
the arrival of P-wave and estimated end of high frequency energy radiation,
respectively.
References
Hara, T., Measurement of duration of
high-frequency energy radiation and its application to determination of
magnitudes of large shallow earthquakes, Earth Planets Space, 59,
227–231, 2007a.
Hara, T., Magnitude
determination using duration of high frequency energy radiation and
displacement amplitude: application to tsunami earthquakes, Earth Planets Space, 59, 561–565, 2007b.
Last Updated: 2012/10/29