Monitoring changes of seismic properties at depth can provide a first‐order insight into
Earth's dynamic evolution. Coda wave interferometry is the primary tool for this purpose. This …

Studying the subsurface structure of volcanoes is crucial for understanding volcanic
mechanisms, current status, and potential risks. However, the intricate physical and …

In recent years, attenuation has been used as a marker for source and dynamic Earth
processes due to its higher sensitivity to small variations of lithospheric properties compared …

Scattered seismic coda waves are frequently used to characterize small scale medium
heterogeneities, intrinsic attenuation or temporal changes of wave velocity. Spatial variability …

Modelling regional-scale attenuation of seismic waves at~ 1 Hz is challenging, especially
when these waves propagate across both continental and oceanic crust. Recent …

We numerically solve the acoustic radiative transfer equation for seismic S‐waves via Monte
Carlo simulation. By assuming a von Kármán‐type random medium with anisotropic …

High resolution maps of seismic attenuation parameters in Taiwan have been obtained from
a modified “Multiple Lapse Time Window Analysis”(MLTWA). At most of the stations in …

Site‐specific seismic hazard studies require the knowledge of the shear‐wave velocity VS
and the high‐frequency site attenuation parameter κ 0 at the reference rock level at depth …

The purpose of the study is to research the prospects of joint use of signals caused by
standing waves of water bodies when studying the geophysical situation near hydroelectric …

Simultaneous inversion of scattering and absorption attenuation is of great significance for
investigating small-scale inhomogeneities and inelastic properties of the subsurface …