A study of the seismic noise from its long-range correlation properties

By Laurent Stehly, Michel Campillo, N. M. Shapiro. 2006

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View Paper: https://www.semanticscholar.org/paper/d0e97ce952b2eda66cdac9ab22b90d9bfd4a67ca

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In Geophysics

Citations in the corpus

Traveltime measurements from noise correlation: stability and detection of instrumental time-shifts (2007, background): “The location of sources of the background primary microseism (10‐20 s period band) is not constant and has a clear seasonal dependence ( Stehly et al. 2006 ).”
Broadband ambient noise surface wave tomography across the United States (2008, background): “[28] Inspection of Figure 8 reveals that the fraction of relatively high SNR paths at a given azimuth is often more homogeneously distributed than the western US results of Stehly et al. [2007] or the synthetic results of Yang and Ritzwoller [2008].”
Origin of deep ocean microseisms by using teleseismic body waves (2010, methodology): “These observation are in good agreement with seasonal variations of the location of sources of microseisms deduced from the polarization analysis and from previous studies [e.g., Stehly et al., 2006].”
Global climate imprint on seismic noise (2009, background): “Stehly et al. [2006] cross-correlated several years of noise and concluded that the California network records secondary microseisms whose source direction is stable over the year toward the Pacific Ocean.”
Structure of young East Pacific Rise lithosphere from ambient noise correlation analysis of fundamental- and higher-mode Scholte-Rayleigh waves (2011, background): “However, because we average over one year of data we would expect smooth variations in the ambient noise energy distribution, as reported in previous ambient noise studies (Harmon et al., 2008; Stehly et al., 2006; Yang et al., 2007).”
Analysis of ambient noise energy distribution and phase velocity bias in ambient noise tomography, with application to SE Tibet (2009, methodology): “Such nearby noise sources may invalidate plane wave modelling, especially at short periods (<10 s) and for near-coastal arrays due to non-linear interactions of ocean waves with coastlines in the secondary microseism band (5–10 s) (e.g. Stehly et al. 2006).”
Reconstructing Green's function by correlation of the coda of the correlation (C3) of ambient seismic noise (2008, methodology): “This can be illustrated by plotting the amplitude of the correlations versus azimuth following the procedure of Stehly et al. [2006]. By measur-”
The origin of deep ocean microseisms in the North Atlantic Ocean (2007, background): “The seismic background noise dominated by oceanic microseisms can be effectively used as a seismic source for tomographic studies of geological properties of the Earth’s crust (Shapiro & Campillo 2004; Shapiro et al. 2005; Weaver 2005; Ritzwoller et al. 2006; Stehly et al. 2006).”
On establishing the accuracy of noise tomography travel‐time measurements in a realistic medium (2009, methodology): “For a noise source distribution far from 2-D isotropic, one must also perform analysis like that of Stehly et al. (2006) or Yao & van der Hilst (2008) to determine the distribution of sources to arrive at ρ(t) as described by eq. (9).”
Characteristics of ambient seismic noise as a source for surface wave tomography (2008, methodology): “Stehly et al. [2006] argue from a similar observation for the physical decoupling of the primary and secondary microseisms.”
Anelastic Earth structure from the coherency of the ambient seismic field (2008, background): “This is expected given the band-limited frequency content of the microseismic noise [Stehly et al., 2006].”
Tutorial on seismic interferometry: Part 1 — Basic principles and applications (2010, background): “Ocean-generated ambient seismic noise (Longuet-Higgins, 1950; Webb, 1998; Stehly et al., 2006) was recorded between October 2004 and November 2007.”
Tomography of the Alpine region from observations of seismic ambient noise (2009, background): “Stehly et al. (2006) have shown that the seismic noise sources in the [5–20 s] period band are distributed over a large surface when integrated over a long time.”
Global P, PP, and PKP wave microseisms observed from distant storms (2008, background): “Stehly et al. [2006] observed primary microseisms (0.05–0.1 Hz) in California originating from the southern Indian Ocean and the southern Pacific.”
Retrieval of Moho‐reflected shear wave arrivals from ambient seismic noise (2010, unknown): “However, only fundamental mode surface waves emerge in most studies involving real data.”