LAUSR

Abstract An Mw 6.2 earthquake struck Hualien on the eastern coast of Taiwan on April 18, 2019. Its focal mechanism was determined to be a thrust fault with a depth of 18.8 km. A wide range of strong ground shaking with an intensity value from 4 (25–80 Gal) to 7 (greater than 400 Gal) occurred in northern Taiwan, which is unusual for earthquakes of this size. Here we show a source model as determined by local seismic waveform inversion. Two asperities were found, the smaller one occurred at the hypocenter and the larger one was found 10 km north of the hypocenter with a depth of 18–25 km. The initial rupture started from the hypocenter and then rapidly propagated all the way to the large asperity in the north. A near supershear speed of close to 4.0 km/s was found to have occurred during this northward rupture process. The inverted source model was evaluated using forward three-dimensional ground motion simulations. The results show strong agreement with island-wide observed displacement waveforms and peak ground acceleration for periods from 3.0 to 20.0 s. The rapid northward rupture caused a strong directivity effect coupled with the specific source radiation pattern, resulting in a large area of strong ground shaking in northern Taiwan, even though the Hualien earthquake was a moderately-sized event.