P-wave attenuation with implications for earthquake early warning

Several widely implemented and tested earthquake early warning algorithms employ empirical equations that relate earthquake magnitudes with ground-motion peak amplitudes and hypocentral distances. This approach is effective to the extent that the offline dataset available for setting the fitting coefficients in those equations is of sufficient quality and quantity. However, to address the problem of having a limited dataset, it is instructive to gain physical understanding of the main factors controlling the P-wave attenuation. In this study, theoretical expressions are derived that relate the root mean square (rms) of the P-wave displacement d (sub rms) and velocity v (sub rms) to the seismic moment, stress drop, and hypocentral distance. The theoretical attenuation laws are then validated against observed attenuation, using earthquake data from southern California and Japan. Good agreement is found between observed and predicted ground motions. The similar ground-motion attenuation in California and Japan suggests that the attenuation laws are similarly applicable for the two regions and implies that they may also be implemented in other regions without having to go through a lengthy calibration phase. Because d (sub rms) is more strongly dependent on the seismic moment than v (sub rms) , use of the attenuation law for d (sub rms) yields better magnitude prediction than that of v (sub rms) . It is shown that the d (sub rms) -to-v (sub rms) ratio is proportional to the characteristic length of the rupture and that the stress drop is a function of the seismic moment and the cube of d (sub rms) /v (sub rms) . This result paves the way for a new stress-drop determination scheme that is totally independent of previously used approaches. Finally, it is shown that the rms of the ground motions are proportional to their peak values.