Determination of earthquake magnitudes using duration of
high-frequency energy radiation and maximum displacement amplitudes: application
Recently, we developed a new method to determine earthquake magnitudes using the following formula (Hara, 2007):
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, 2007). 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.
Hara, T., Measurement of duration of high-frequency energy radiation and its application to determination of magnitudes of large shallow earthquakes, accepted for publication in Earth Planets Space, 2007.
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: 2007/01/14