Determination of earthquake magnitudes using duration of
high-frequency energy radiation and maximum displacement amplitudes: application
to the
Tatsuhiko Hara
International
Recently, we developed a new method to determine earthquake
magnitudes using the following formula (Hara, 2006):
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 (Lomax, 2005; Park et
al., 2005; Ni et al., 2005; Hara,
2006). 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
Fig. 1. An example of measurements of high frequency
energy radiation. The upper and lower traces are an observed seismogram
and its smoothed time series of squares of band-pass (2-4 Hz) filtered
seismogram (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, submitted to Earth Planets Space, 2006.
Lomax, A., Rapid estimation of rupture extent for large earthquakes:
Application to the 2004, M9 Sumatra-Andaman mega-thrust, Geophys. Res. Lett., 32, L10314, doi:10.1029/2005GL022437,
2005.
Ni, S., H. Kanamori, and D. Helmberger,
Energy radiation from the
Park, J., K. Anderson, R. Aster, R. Butler,
T. Lay, and D. Simpson, Global seismographic network records the great
Sumatra-Andaman earthquake, Eos Trans.
AGU, 86(6), 57, 2005.
Last Updated: 2006/11/16