Fig. 4From: Detecting pre-eruptive magmatic processes of the 2018 eruption at Kilauea, Hawaii volcano with ambient noise interferometryThe 1-D velocity model and corresponding Rayleigh-wave depth sensitivity kernels. a The P-wave (blue) and S-wave (red) 1-D velocity models of Kilauea area averaging from the 3-D velocity model (Lin et al. 2014). b Rayleigh-wave depth sensitivity kernels for shear wave velocity changes in different frequencies between 0.3 and 2.0 HzBack to article page