This paper presents an interdisciplinary review of the correlation properties of random
wavefields. We expose several important theoretical results of various fields, ranging from …

The cross correlation of ambient signal allows seismologists to collect data even in the
absence of seismic events.“Seismic interferometry” shows that the cross correlation of …

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 …

The structure of the earth has been extensively studied using seismic waves generated by
natural earthquakes and man-made sources. In classical seismology, the earth is …

The Green's function of waves that propagate between two receivers can be found by cross-
correlating multiply scattered waves recorded at these receivers. This technique obviates the …

The term seismic interferometry refers to the principle of generating new seismic responses
by crosscorrelating seismic observations at different receiver locations. The first version of …

[1] We propose passive image interferometry as a technique for seismology that allows to
continuously monitor small temporal changes of seismic velocities in the subsurface. The …

T urning noise into useful data—every geophysicist's dream? And now it seems possible.
The field of seismic interferometry has at its foundation a shift in the way we think about the …

The motion of a building depends on the excitation, the coupling of the building to the
ground, and the mechanical properties of the building. We separate the building response …

This study presents surface wave dispersion maps across the contiguous United States
determined using seismic ambient noise. Two years of ambient noise data are used from …