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This makes the locations of maximum displacement amplitudes shift to the right (see Figure 4b,c,d,e,f).

Hara (2007a) developed a method to determine earthquake magnitudes using durations of high frequency energy radiation, which we refer to as HFER hereafter, and maximum displacement amplitudes measured from first arriving P -waves recorded at a tele-seismic distance range.

We have applied a technique to determine earthquake magnitudes, using durations of high frequency energy radiation and the maximum displacement amplitudes, to the 2011 off the Pacific coast of Tohoku Earthquake.

Fig. 3. Contributions to magnitudes from maximum displacement amplitudes and epicentral distances (the horizontal axis) and those from durations of HFER (the vertical axis) are plotted for events analyzed by Hara (2007a, b, 2009) and large (Mw≥ 7.2) shallow (depths ≤ 50 km) earthquakes that occurred from July, 2006 to the 2011 off the Pacific coast of Tohoku Earthquake.

For JMA EEW, the hypocenter is determined by a combination of several techniques (Hoshiba et al., 2008), using approximately 1,100 stations from the JMA network and the Hi-net network of NIED; magnitude is mainly from maximum displacement amplitudes (Kamigaichi et al., 2009).

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Lower panel: magnitudes estimated from maximum displacement amplitude at four stations.

The JMA displacement magnitude is determined from the logarithm of the maximum displacement amplitude recorded with seismographs of natural period 6 s and damping coefficient of 0.55.

For the pressure-deformed transducers fabricated from PVDF film, displacement amplitudes of 9 14.5 nm/V were observed, and the maximum displacement amplitude took place at the applied tension and static pressure predicted by the model.

In case No. 10, the IPF method estimated a hypocenter located close to the station that observed the maximum displacement amplitude and calculated a magnitude of 5.8, which was 0.6 units lower than that in the current method.

Note that the displacement magnitude is estimated from maximum displacement amplitude which corresponds to the outputs of seismometers having eigenperiod of 6 s, and the mainshock displacement magnitude is 8.4 in the unified hypocenter catalog of JMA (Hirose et al., 2011).

Wear rates increase with increase in maximum Hertzian pressure, displacement amplitude, coefficient of friction and depth of initial crack.

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