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Site amplification, attenuation, and scattering from noise correlation amplitudes across a dense array in Long Beach, CA
Author(s) -
Bowden D. C.,
Tsai V. C.,
Lin F. C.
Publication year - 2015
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1002/2014gl062662
Subject(s) - amplitude , geophone , geology , ambient noise level , attenuation , seismology , noise (video) , seismic noise , seismic array , rayleigh wave , rayleigh scattering , acoustics , scattering , physics , optics , wave propagation , computer science , sound (geography) , geomorphology , artificial intelligence , image (mathematics)
For accurate seismic hazard evaluation, both the spatial and frequency‐dependent variabilities in the amplitudes of earthquake ground motions are needed. While this information is rarely fully available due to the paucity of relevant seismic data, dense arrays like the 5200‐geophone array in Long Beach, California provide the opportunity to study this amplitude variability. Here we show that ambient noise correlation amplitudes from the Long Beach array can be used to directly determine frequency‐dependent site amplification factors. We analyze Rayleigh‐wavefield amplitude gradients from ambient noise correlations that are processed so that relative amplitudes satisfy the wave equation and are therefore meaningful. Ultimately, we construct maps of site amplification across Long Beach at frequencies of 0.67, 1.0, and 2.0 Hz. These maps correlate well with local structure, notably the Newport‐Inglewood Fault and also to known velocity structure. Through this process, we also obtain constraints on average attenuation structure and local scattering.