P‐waves from cross‐correlation of seismic noise

By Philippe Roux, Karim Sabra, Peter Gerstoft, William A. Kuperman, Michael Fehler. 2005

331 citations recorded by the source corpus.

Subfields: Artificial Intelligence, Geophysics

View Paper: https://www.semanticscholar.org/paper/fa9a4d5f1b1a219479b9eb5caa296250b2b1d703

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Citations in the corpus

Ambient noise Rayleigh wave tomography of New Zealand (2007, methodology): “…of using diffuse seismic wavefields to extract the Green’s function have been substantiated using earthquake coda waves (Campillo & Paul 2003; Paul et al. 2005) and ambient seismic noise for surface waves (e.g. Shapiro & Campillo 2004; Sabra et al. 2005a) and local body waves (Roux et al. 2005).”
Shear wave imaging from traffic noise using seismic interferometry by cross-coherence (2011, unknown): “Examples include the extraction of P-waves using distributed sources (e.g., Roux et al., 2005; Hohl and Mateeva, 2006; Draganov et al., 2007; Gerstoft et al., 2008; Draganov et al., 2009; Zhang et al., 2009) and of S-waves using localized noise sources (e.g., O’Connell, 2007; Miyazawa et al., 2008).”
Ambient noise Rayleigh wave tomography across Europe (2007, background): “Seismic observations have confirmed the theory using both coda waves (Campillo & Paul 2003; Paul et al. 2005) and ambient noise for surface waves (Shapiro & Campillo 2004; Sabra et al. 2005a) and crustal body waves (Roux et al. 2005).”
Retrieval of Moho‐reflected shear wave arrivals from ambient seismic noise (2010, background): “Roux et al. (2005) reports P-wave energy in the noise cross-correlation functions (NCFs) between stations separated by 2–10 km at Parkfield, California, and Zhang et al. (2009) show that the noise is strongly correlated with ocean winds.”
Anelastic Earth structure from the coherency of the ambient seismic field (2008, background): “Further work has shown that as long as the attenuation is small [Roux et al., 2005b; Nakahara, 2006a; Snieder, 2007; Gouédard et al., 2008; Colin de Verdière, 2009] the Green’s function can be retrieved.”
Using instantaneous phase coherence for signal extraction from ambient noise data at a local to a global scale (2011, methodology): “…D U C T I O N Green’s functions can be extracted from seismic noise crosscorrelations as theoretically shown with different approaches by Lobkis & Weaver (2001), Derode et al. (2003), Wapenaar (2004), Snieder (2004), Roux et al. (2005a), Wapenaar et al. (2006), Snieder et al. (2007) among others.”
Improved ambient noise correlation functions using Welch's method (2012, background): “The result of days, months or years of stacked correlation is often called a noise correlation function (NCF; e.g. Roux et al. 2005; Sabra et al. 2005).”