Global seismographic networks (GSNs) emerged during the late nineteenth and early
twentieth centuries, facilitated by seminal international developments in theory, technology …

The ambient seismic wave field, also known as ambient noise, is excited by oceanic gravity
waves primarily. This can be categorized as seismic hum (1–20 mHz), primary microseisms …

The rotation of the Earth or Earth rotation, respectively, specifies the spatiotemporal change
of the Earth rotation vector. The direction of the Earth rotation vector corresponds to the …

It has been widely recognized that the cross‐correlation function of ambient seismic noise
data recorded at two stations approximates to the part of Greens function between two …

Stacks of ambient noise cross-correlations are more and more routinely used to extract
empirical Green's functions between station pairs. The success of the cross-correlations is …

Seismic interferometry applied to 120 hr of railroad traffic recorded by an array of vertical
component seismographs along a railway within the Rio Grande rift has recovered surface …

We proposed a new passive seismic method (PSM) based on seismic interferometry and
multichannel analysis of surface waves (MASW) to meet the demand for increasing …

We present high‐resolution 3D images of the crustal S‐wave velocity structure beneath
northeastern Tibet, via ambient noise imaging techniques. The data come from continuous …

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 …

Seismic body waves that sample Earth's core are indispensable for studying the most
remote regions of the planet. Traditional core phase studies rely on well‐defined earthquake …