Retrieving the elastodynamic Green's function of an arbitrary inhomogeneous medium by cross correlation.
By Kees Wapenaar. Physical Review Letters, 2004
892 citations recorded by the source corpus.
Subfields: Geophysics, Mechanics of Materials
View Paper: https://www.semanticscholar.org/paper/5c3c94744c8d0a49c84799ec3016ac3f0dff94e6
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Geophysics
- M. Ritzwoller
- N. M. Shapiro
- Roel Snieder
- Michel Campillo
- Fan-Chi Lin
- Kees Wapenaar
- Yingjie Yang
- Laurent Stehly
In Mechanics of Materials
- Roel Snieder
- N. M. Shapiro
- Michel Campillo
- Nori Nakata
- M. Ritzwoller
- Victor C. Tsai
- K. Larner
- Kees Wapenaar
Citations in the corpus
- Multiscale full waveform inversion (2013, positive): “Intheidealisticcasewhereseismicnoiseisgenerated bysourcescoveringaclosedsurfacearoundeachreceiverpair,the correlationfunctionapproximatestheinterstationGreen’sfunction (e.g. Lobkis&Weaver2001;Wapenaar2004;Shapiro et al. 2005).”
- Shear wave imaging from traffic noise using seismic interferometry by cross-coherence (2011, methodology): “Green’s function extraction can be derived from normal modes (Lobkis and Weaver, 2001), representation theorems (Wapenaar, 2004; Wapenaar and Fokkema, 2006), the principle of time reversal (Roux and Fink, 2003), and stationary phase analysis (Snieder et al., 2006).”
- On establishing the accuracy of noise tomography travel‐time measurements in a realistic medium (2009, methodology): “We make the further assumption that, as in all other derivations of a noise-correlation property (e.g. Lobkis & Weaver 2001; Snieder 2004; Wapenaar 2004), the cross-correlation is performed over a sufficiently long time series that the cross-correlation is simply the sum of individual sinusoidal…”
- Improved ambient noise correlation functions using Welch's method (2012, background): “…over a period of time, the Green’s function or impulse response between the two stations can be extracted, assuming that the noise source distribution is spatially homogeneous around the stations (e.g. Lobkis & Weaver 2001; Derode et al. 2003; Shapiro & Campillo 2004; Snieder 2004; Wapenaar 2004).”
- Retrieval of the Green’s Function from Cross Correlation: The Canonical Elastic Problem (2006, background): “Wapenaar (2004) gives an interpretation based on a special kind of representation theorem and assumed a continuous distribution of sources on a closed surface surrounding the receivers.”
- Analysis of ambient noise energy distribution and phase velocity bias in ambient noise tomography, with application to SE Tibet (2009, background): “…propagation between two receivers can be recovered from cross-correlation of ambient wavefields (e.g. 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).”
- Tutorial on seismic interferometry: Part 2 — Underlying theory and new advances (2010, methodology): “After that, we review exact Green’s function representations for seismic interferometry in arbitrary inhomogeneous, anisotropic lossless solids Wapenaar, 2004 and discuss the approximations that lead to the commonly used expressions.”
- Empirical synthesis of time-asymmetrical Green functions from the correlation of coda waves (2005, background): “Wapenaar [2004] demonstrated the retrieval of the elastic Green tensor from surface displacement fields produced by a distribution of sources on a closed surface in the medium.”
- Extraction of near-surface properties for a lossy layered medium using the propagator matrix (2007, methodology): “…& Haddadi 1998; Lobkis & Weaver 2001; Derode et al. 2003; Kawakami & Oyunchimeg 2003; Schuster et al. 2004; Shapiro & Campillo 2004; Snieder 2004; Wapenaar 2004; Shapiro et al. 2005; Wapenaar et al. 2005; Snieder et al. 2006a) is a technique based on combining signals recorded at different…”
- P‐waves from cross‐correlation of seismic noise (2005, background): “…few years in various fields of wave physics such as ultrasonics [Weaver and Lobkis, 2001, 2004], underwater acoustics [Roux et al., 2004] and geophysics [Rickett and Claerbout, 1999; Campillo and Paul, 2003; Shapiro and Campillo, 2004; Wapenaar, 2004; Sabra et al., 2005a; Shapiro et al., 2005].”
- Reconstructing Green's function by correlation of the coda of the correlation (C3) of ambient seismic noise (2008, background): “Other derivations [Wapenaar, 2004; Snieder, 2004; Sánchez-Sesma et al., 2006] of expressions like (1) make comparable assumptions about the field being correlated or about its source.”
- Seismic imaging: From classical to adjoint tomography (2012, background): “Subsequent studies using reciprocity and scattered waves (Snieder, 2004; Wapenaar, 2004) led to increased confidence in tomographic maps under the assumption of ambient noise sources.”
- Broadband ambient noise surface wave tomography across the United States (2008, methodology): “[1] This study presents surface wave dispersion maps across the contiguous United States determined using seismic ambient noise.”