In this work we investigate fundamentals of a method—referred to as full waveform ambient
noise inversion—that improves the resolution of tomographic images by extracting waveform …

We present an improved crustal Vs model and Moho depth map using ambient noise wave-
equation tomography. The so-called 'ambient noise wave-equation tomography'is a method …

Taking benefit of the AlpArray temporary network and permanent networks in W‐Europe, we
construct a 3‐D onshore‐offshore velocity model of the crust and upper mantle using …

The sources of ambient seismic noise are extensively studied both to better understand their
influence on ambient noise tomography and related techniques, and to infer constraints on …

The retrieval of a deterministic signal from recordings of a quasi-random ambient seismic
field is the central goal of noise interferometry. It is the foundation of numerous applications …

We present the first application of full‐waveform ambient noise inversion to observed
correlation functions that jointly constrains 3‐D Earth structure and heterogeneous noise …

Cross-correlations of ambient seismic noise are widely used for seismic velocity imaging,
monitoring and ground motion analyses. A typical step in analysing noise cross-correlation …

Seismic velocities in rocks are highly sensitive to changes in permanent deformation and
fluid content. The temporal variation of seismic velocity during the preparation phase of …

The Los Angeles basin is located within the North America–Pacific plate boundary and
contains multiple earthquake faults that threaten greater Los Angeles. Seismic attenuation …

Global and regional seismic attenuation models reveal anelastic heterogeneous structures
in the earth, which shed new light on the temperature, melt and volatile fraction of Earth's …