Japan Geoscience Union Meeting 2021

Presentation information

[J] Oral

S (Solid Earth Sciences ) » S-SS Seismology

[S-SS09] Seismic wave propagation: Theory and Application

Sat. Jun 5, 2021 10:45 AM - 12:15 PM Ch.18 (Zoom Room 18)

convener:Kaoru Sawazaki(National Research Institute for Earth Science and Disaster Resilience), Kiwamu Nishida(Earthquake Research Institute, University of Tokyo), Takao Nibe(JAPEX), Kyosuke Okamoto(National Institute of Advanced Industrial Science and Technology), Chairperson:Kyosuke Okamoto(National Institute of Advanced Industrial Science and Technology), Shunsuke Takemura(Earthquake Research Institute, the University of Tokyo)

11:45 AM - 12:00 PM

[SSS09-10] Ambient Noise Differential Adjoint Tomography Applied to a Linear Array in Los Angeles Basin

*Xin Liu1,2, Gregory C Beroza1 (1.Stanford Earth, 2.JAMSTEC)

Keywords:ambient noise adjoint tomography, near surface shear velocity

The small time shifts that are used in ambient-field interferometric Green’s function analysis may arise from either structural anomalies of interest, or spatio-temporal behavior of the noise source, which is usually not of interest. In seismic noise interferometry, the differential time kernel has been shown to be much less sensitive to variations in the spatio-temporal distributions of the noise source and more sensitive to the structural anomalies of interest, thus using differential measurements is an effective approach for reducing bias in tomographic images (Liu 2020). In this study, we generalize this technique by deriving the shear-wave velocity directly from differential time kernels for fundamental mode Love waves in noise cross-correlations along a linear array spanning ~37 km in the Los Angeles basin without the 1D depth conversion step that assumes a layered medium. The initial results show strong sensitivity to near-surface shear velocity structure in the uppermost 500 m. We then apply iterative inversion for shear velocity, and will present an updated near-surface shear velocity structure that should help to constrain future urban earthquake ground motion.