Repeating seismic experiments reveal variation in seismic reflectivity beneath Sakurajima Volcano, Japan.
Reflectivity variation locates northeastern Sakurajima at the depth of 6.2 km.
Seismic reflectivity decreased by 30% with deflation after 2009.
Change in seismic velocity in the intermediate layer at the reflector can explain the reflectivity variation.
The velocity change can be caused by temperature change through the progress of activity.