Fig. 6From: Temporal change in seismic wave attenuation using highly stable vibration sourcesChanges in amplitudes 10Â days before and after the 2000 Western Tottori (WT) and 2001 Geiyo (GY) earthquakes. The bottom row shows the temperature and rainfall at Gunka station. The gap between horizontal lines with a pair of triangles on the left of the panels shows the average error of the amplitude changeBack to article page