Ultrasonics without a source: thermal fluctuation correlations at MHz frequencies.
By Richard Weaver, O. Lobkis. Physical Review Letters, 2001
647 citations recorded by the source corpus.
Subfields: Oceanography, Statistical and Nonlinear Physics
View Paper: https://www.semanticscholar.org/paper/0b33d76df587f589b1aa17b9b62a1f5f1eb5b115
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Oceanography
- Michel Campillo
- Roel Snieder
- Kees Wapenaar
- N. M. Shapiro
- Jesse F. Lawrence
- G. Prieto
- Laurent Stehly
- Jacob T. Fokkema
In Statistical and Nonlinear Physics
- N. M. Shapiro
- Michel Campillo
- Roel Snieder
- Kees Wapenaar
- M. Ritzwoller
- F. Brenguier
- É. Larose
- G. D. Bensen
Citations in the corpus
- Interferometry by deconvolution. Part 1 -Theory for acoustic waves and numerical examples (2008, background): “Weaver and Lobkis, 2001; Wapenaar et al., 2004; Weaver and Lobkis, 2004".”
- Processing seismic ambient noise data to obtain reliable broad-band surface wave dispersion measurements (2007, neutral): “Weaver & Lobkis 2001a, b, 2004; Derode et al. 2003; Snieder 2004; Wapenaar 2004; Larose et al. 2005).”
- Seismic interferometry-turning noise into signal (2006, background): “Weaver and Lobkis (2001) demonstrated this conjecture for ultrasound waves by calculating that the long-term average of random noise in an aluminum block yields the timedomain impulse response between the two points.”
- Focusing the wavefield inside an unknown 1D medium: Beyond seismic interferometry (2012, background): “First, with seismic interferometry (Weaver and Lobkis, 2001; Wapenaar et al., 2005; Curtis et al., 2006; Schuster, 2009) it is possible to retrieve the response to a virtual source inside the medium with a receiver at the position where the virtual source is to be created, assuming the medium is…”
- Retrieving the Green’s function in an open system by cross correlation : A comparison of approaches (L) (2005, background): “Since the work of Weaver and Lobkis (2001; 2001), many researchers have shown theoretically and experimentally that the cross-correlation of the recordings of a diffuse wave field at two receiver positions yields the Green’s function between these positions.”
- Improved ambient noise correlation functions using Welch's method (2012, neutral): “Multisensor ambient noise analyses have been applied to a variety of subjects including ultrasonics (Weaver & Lobkis 2001; Larose 2006), helioseismology (Duvall et al. 1993; Rickett & Claerbout 1999, 2000), ocean acoustics (Roux & Kupperman 2005), engineering (Kohler et al. 2005; Snieder & Safak…”
- Assessment of resolution and accuracy of the Moving Window Cross Spectral technique for monitoring crustal temporal variations using ambient seismic noise (2011, methodology): “…the cross-correlation of records of a random seismic wave field taken at various locati ns within a region of interest ⋆ MWCS: assessment of resolution and accuracy3 (Weaver & Lobkis 2001; Lobkis & Weaver 2001; Campillo & Paul 2003; Shapiro & Campillo 2004; Shapiro et al. 2005; Sabra et al. 2005).”
- Using instantaneous phase coherence for signal extraction from ambient noise data at a local to a global scale (2011, background): “A large amount of recent publications show the different applications in fields such as ultra sound (Weaver & Lobkis 2001; Derode et al. 2003) helio seismology (Duvall et al. 1993; Rickett & Claerbout 1999, 2000), fault and volcano monitoring (Sens-Schönfelder & Wegler 2006; Wegler &…”
- Seismic and electromagnetic controlled‐source interferometry in dissipative media (2008, neutral): “…p̂+ and p̂− are the down going and up going wave fields, respectively (the Fourier transform of a time-dependent function f (t) is defined as f̂ (ω) =∫ ∞ −∞ f (t) exp(− jωt)dt, where j is the imaginary unit and ω denotes the angular frequency, which is taken as non-negative throughout this paper).”
- Emergence of broadband Rayleigh waves from correlations of the ambient seismic noise (2004, positive): “…functions from the diffuse wavefield has been successfully applied in helioseismol-ogy [e.g., Duvall et al. , 1993; Kosovichev et al. , 2000; Rickett and Claerbaut , 2000], in ultrasonics [e.g., Weaver and Lobkis , 2001a, 2001b; Derode et al. , 2003], and in marine acoustics [ Roux et al. , 2003].”
- Local Helioseismology: Three-Dimensional Imaging of the Solar Interior (2010, background): “Various experiments and observations (e.g. Shapiro et al. 2005, Weaver & Lobkis 2001) have shown that the cross-covariance is intimately connected to the Green’s function, G, i.e. the response of the medium to an impulsive source.”
- Tutorial on seismic interferometry: Part 1 — Basic principles and applications (2010, positive): “Early successful results of Green’s function retrieval from noise correlations were obtained in the field of ultrasonics Weaver and Lobkis (2001, 2002).”
- 3‐D surface wave tomography of the Piton de la Fournaise volcano using seismic noise correlations (2007, positive): “[ 5 ] In the field of ultrasonics, it has been shown both theoretically and experimentally that a random wavefield has correlations which, on average, take the form of the Green’s function of the media [ Weaver and Lobkis , 2001; Lobkis and Weaver , 2001].”