TY - JOUR
T1 - Probabilistic point source inversion of strong-motion data in 3-D media using pattern recognition
T2 - A case study for the 2008 Mw 5.4 Chino Hills earthquake
AU - Käufl, Paul
AU - Valentine, Andrew P.
AU - Trampert, Jeannot
N1 - Publisher Copyright:
©2016. The Authors.
PY - 2016/8/28
Y1 - 2016/8/28
N2 - Despite the ever increasing availability of computational power, real-time source inversions based on physical modeling of wave propagation in realistic media remain challenging. We investigate how a nonlinear Bayesian approach based on pattern recognition and synthetic 3-D Green's functions can be used to rapidly invert strong-motion data for point source parameters by means of a case study for a fault system in the Los Angeles Basin. The probabilistic inverse mapping is represented in compact form by a neural network which yields probability distributions over source parameters. It can therefore be evaluated rapidly and with very moderate CPU and memory requirements. We present a simulated real-time inversion of data for the 2008 Mw 5.4 Chino Hills event. Initial estimates of epicentral location and magnitude are available ∼14 s after origin time. The estimate can be refined as more data arrive: by ∼40 s, fault strike and source depth can also be determined with relatively high certainty.
AB - Despite the ever increasing availability of computational power, real-time source inversions based on physical modeling of wave propagation in realistic media remain challenging. We investigate how a nonlinear Bayesian approach based on pattern recognition and synthetic 3-D Green's functions can be used to rapidly invert strong-motion data for point source parameters by means of a case study for a fault system in the Los Angeles Basin. The probabilistic inverse mapping is represented in compact form by a neural network which yields probability distributions over source parameters. It can therefore be evaluated rapidly and with very moderate CPU and memory requirements. We present a simulated real-time inversion of data for the 2008 Mw 5.4 Chino Hills event. Initial estimates of epicentral location and magnitude are available ∼14 s after origin time. The estimate can be refined as more data arrive: by ∼40 s, fault strike and source depth can also be determined with relatively high certainty.
KW - earthquake early warning
KW - neural networks
KW - probabilistic inversion
UR - http://www.scopus.com/inward/record.url?scp=84983627452&partnerID=8YFLogxK
U2 - 10.1002/2016GL069887
DO - 10.1002/2016GL069887
M3 - Article
SN - 0094-8276
VL - 43
SP - 8492
EP - 8498
JO - Geophysical Research Letters
JF - Geophysical Research Letters
IS - 16
ER -