Fig. 4From: Combined use of repeated active shots and ambient noise to detect temporal changes in seismic velocity: application to Sakurajima volcano, JapanDCCFs for the V.SFT2–V.SKD2 pair in the 2–4 Hz over the time period of 2012 and 2014. Temporal changes in seismic velocity are estimated by using parts between −10 and 10 s in lag time. The reference CCF is shown at the top by black solid curve, which is calculated by stacking DCCFs over 2012 and 2013. The bottom panel is a result of estimating dt/t on March 6, 2012Back to article page