Diffuse fields in open systems and the emergence of the Green’s function (L)

By Richard Weaver, O. Lobkis. 2004

348 citations recorded by the source corpus.

Subfields: Geophysics, Ocean Engineering

View Paper: https://www.semanticscholar.org/paper/91a5a68801abef6f094def404865466ea5f92f0b

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Citations in the corpus

Characteristics of ambient seismic noise as a source for surface wave tomography (2008, background): “[2] Theoretical and experimental research has shown that the cross correlation of ambient noise records from two receivers provides an estimate of the empirical Green’s function between the receivers [ Weaver and Lobkis, 2001, 2004; Derode et al., 2003a; Snieder, 2004; Larose et al., 2005].”
Extracting time‐domain Green's function estimates from ambient seismic noise (2005, background): “…in helioseismology [Rickett and Claerbout, 1999], ultrasonics [Lobkis and Weaver, 2001; Weaver and Lobkis, 2003; Larose et al., 2004; Malcolm et al., 2004; Weaver and Lobkis, 2004], underwa- ter acoustics [Roux et al., 2004; Sabra et al., 2005], and in seismology [Shapiro and Campillo, 2004].”
Spurious multiples in seismic interferometry of primaries (2006, methodology): “This requirement was relaxed in an alternative derivation based on the representation theorem for one-way wave propagation [Wapenaar et al., 2004], and by using the general representation theorem [Weaver and Lobkis, 2004; Wapenaar, 2004].”
Seismic and electromagnetic controlled‐source interferometry in dissipative media (2008, positive): “The reflection response R̂+0 (x3,1, ω) is the response that would be measured with source and receiver at x3,1 and a homogeneous half-space above x3,1.”
Surface-wave array tomography in SE Tibet from ambient seismic noise and two-station analysis: I - Phase velocity maps (2006, positive): “Previous studies (Lobkis & Weaver 2001; Weaver & Lobkis 2004; Roux et al. 2005; Sabra et al. 2005a) have demonstrated that EGFs obtained from the noise cross-correlation function (NCF), by taking the time derivative, are equivalent to real Green’s function except for a frequency-dependent amplitud”
Analysis of ambient noise energy distribution and phase velocity bias in ambient noise tomography, with application to SE Tibet (2009, background): “Lobkis & Weaver 2001; Campillo & Paul 2003; Malcolm et al. 2004; Shapiro & Campillo 2004; Snieder 2004; Wapenaar 2004; Weaver & Lobkis 2004; Roux et al. 2005; Nakahara 2006; Wapenaar et al. 2006).”
P‐waves from cross‐correlation of seismic noise (2005, background): “…Gerstoft, and W. A. Kuperman Marine Physical Laboratory, University of California San Diego, La Jolla, California, USA Michael C. Fehler Los Alamos National Laboratory, Los Alamos, New Mexico, USA Received 13 June 2005; revised 19 August 2005; accepted 31 August 2005; published 6 October 2005.”
Empirical synthesis of time-asymmetrical Green functions from the correlation of coda waves (2005, background): “The same arguments hold for an open medium as well [Weaver and Lobkis, 2004].”