Source inversion of W phase: speeding up seismic tsunami warning

320 citations recorded by the source corpus.

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

SCARDEC: a new technique for the rapid determination of seismic moment magnitude, focal mechanism and source time functions for large earthquakes using body‐wave deconvolution (2011, background): “The lower limit is constrained by the existence of the low-frequency W phase (Kanamori 1993), which becomes predominant for frequencies lower than 0.005 Hz (Kanamori & Rivera 2008).”
A rupture model of the 2011 off the Pacific coast of Tohoku Earthquake (2011, methodology): “R1 signals with a wide group velocity window, and deconvolved the signals using an iterative time-domain procedure based on the method of Kikuchi and Kanamori (1982). We convolved each signal with a low-pass Gaussian filter to reduce short-period noise in the resulting time series.”
W phase source inversion for moderate to large earthquakes (1990–2010) (2012, methodology): “The W phase CMT algorithm was initially developed by Kanamori & Rivera (2008) using the inversion of vertical components of ground motion.”