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Journal ArticleDOI

On the emergence of the Green's function in the correlations of a diffuse field

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TLDR
It is shown that a diffuse field is not devoid of phase information, but has a correlation function equal to the Green's function, and the cross-correlation between diffuse signals in two transducers is very nearly equal to an impulse applied to the other.
Abstract
A diffuse acoustic field is shown to have correlations equal to the Green’s function of the body. Simple plausibility arguments for this assertion are followed by a more detailed proof. A careful version of the statement is found to include caveats in regard to how diffuse the field truly is, the spectrum of the diffuse field, and the phase of the receivers. Ultrasonic laboratory tests confirm the assertion. The main features of the direct signal between two transducers are indeed recovered by cross correlating their responses to a diffuse field generated by a third transducer. The quality of the recovery improves with increased averaging and the use of multiple sources. Applications are discussed.

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Citations
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Journal ArticleDOI

High-resolution surface-wave tomography from ambient seismic noise.

TL;DR: Cross-correlation of 1 month of ambient seismic noise recorded at USArray stations in California yields hundreds of short-period surface-wave group-speed measurements on interstation paths that are used to construct tomographic images of the principal geological units of California.
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Processing seismic ambient noise data to obtain reliable broad-band surface wave dispersion measurements

TL;DR: Proxy curves relating observed signal-to-noise ratios to average measurement uncertainties show promise to provide useful expected measurement error estimates in the absence of the long time-series needed for temporal subsetting.
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Emergence of broadband Rayleigh waves from correlations of the ambient seismic noise.

TL;DR: In this paper, the authors demonstrate that coherent information about the Earth structure can be extracted from the ambient seismic noise using a cross-correlations of vertical component records of several days of seismic noise at different pairs of stations separated by distances from about one hundred to more than two thousand kilometers.
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Long-range correlations in the diffuse seismic coda.

TL;DR: This seismological example shows that diffuse waves produced by distant sources are sufficient to retrieve direct waves between two perfectly located points of observation and has potential applications in other fields.
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Extracting the Green's function from the correlation of coda waves: A derivation based on stationary phase

TL;DR: An alternative derivation of passive imaging of the ballistic wave that is not based on normal modes is presented, showing that the global requirement of the equipartitioning of normal modes can be relaxed to the local requirement that the scattered waves propagate on average isotropically near the receivers.
References
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Journal ArticleDOI

Ultrasonics without a source: thermal fluctuation correlations at MHz frequencies.

TL;DR: It is argued that acoustic thermal fluctuations, with displacement amplitudes of 3 fm, contain substantial ultrasonic information and it is shown that the noise autocorrelation function is the waveform that would be obtained in a direct pulse/echo measurement.
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On the emergence of the Green's function in the correlations of a diffuse field: pulse-echo using thermal phonons.

TL;DR: In this paper, it was shown that the cross-correlation between diffuse signals in two transducers is very nearly equal to the direct response of one transducer to an impulse applied to the other.
Journal ArticleDOI

Robust acoustic time reversal with high-order multiple scattering

TL;DR: The first experiments showing the reversibility of transient acoustic waves through high-order multiple scattering by means of an acoustic time-reversal mirror are reported, with the observed resolution one-sixth of the theoretical limit for the mirror's aperture.
Journal ArticleDOI

On diffuse waves in solid media

TL;DR: In this article, a diffuse field in a solid medium is found to partition its energy between transverse and dilatational waves in a fraction R = 2(cd/ct)3.
Journal ArticleDOI

Observation of Equipartition of Seismic Waves

TL;DR: Observations of this principle for seismic waves created by earthquakes in Mexico are reported and qualitative agreement with an equipartition model that accounts for mode conversions at the Earth's surface is found.
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