Emergence rate of the time-domain Green's function from the ambient noise cross-correlation function

By Karim Sabra, Philippe Roux, William A. Kuperman. 2005

183 citations recorded by the source corpus.

Subfields: Geophysics, Ocean Engineering, Oceanography

View Paper: https://www.semanticscholar.org/paper/b5d0800a491943c8de3784b33a8df551b8c73a58

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Geophysics

1. G. Prieto
2. Michel Campillo
3. Jesse F. Lawrence
4. Laurent Stehly
5. Gregory C. Beroza
6. Richard Weaver
7. B. Froment
8. N. M. Shapiro

In Ocean Engineering

1. Michel Campillo
2. Laurent Stehly
3. Jesse F. Lawrence
4. G. Prieto
5. Gregory C. Beroza
6. B. Froment
7. Richard Weaver
8. N. M. Shapiro

In Oceanography

1. Michel Campillo
2. Laurent Stehly
3. Jesse F. Lawrence
4. B. Froment
5. G. Prieto
6. Gregory C. Beroza
7. Richard Weaver
8. Roel Snieder

Citations in the corpus

• Anelastic Earth structure from the coherency of the ambient seismic field (2008, methodology): “In most previous studies one-bit normalization [Campillo and Paul, 2003; Bensen et al., 2007] or clipping [Sabra et al., 2005a] has been applied to the time series records before calculating the correlations or coherencies.”
• Reconstructing Green's function by correlation of the coda of the correlation (C3) of ambient seismic noise (2008, methodology): “The convergence toward the Green’s function, i.e., the ratio of amplitude of R over residual fluctuations, is evolving as the square root of the amount of data used in the cross correlation [Larose et al., 2004; Snieder, 2004; Sabra et al., 2005a; Weaver and Lobkis, 2005].”