Fig. 11From: Spatial and temporal influence of rainfall on crustal pore pressure based on seismic velocity monitoringComparison of moving averaged seismic velocity changes and pore pressure estimated from precipitation at the seismic station (red dots in Fig. 1f). a Moving averaged seismic velocity change. b Precipitation and the calculated pore pressure change. c Correlation between averaged seismic velocity change and pore pressure. The signals are normalizedBack to article page