Determination of earthquake magnitudes using duration of high-frequency energy radiation and maximum displacement amplitudes: application to the 2011 off the Pacific coast of Tohoku Earthquake
We developed a new 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 2011 off the Pacific coast of
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. "A" and "F" 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, 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: 2011/03/13