Abstract

Seismic wave-propagation simulations are limited in their frequency content by two main factors: (1) the resolution of the seismic wave-speed structure of the region in which the seismic waves are propagated through; and (2) the extent of our understanding of the rupture process, mainly on the short length scales. For this reason, high-frequency content in the ground motion must be simulated through other means. Toward this end, we adopt a variant of the classical empirical Green’s function (EGF) approach of summing, with suitable time shift, recorded seismograms from small earthquakes in the past to generate high-frequency seismograms (0.5–5.0 Hz) for engineering applications. We superimpose these seismograms on low-frequency seismograms, computed from kinematic source models using the spectral element method, to produce broadband seismograms. The non-uniform time- shift scheme used in this work alleviates the over-estimation of high-frequency content of the ground motions observed. We validate the methodology by simulating broadband motions from the 1999 Hector Mine and the 2006 Parkfield earthquakes and comparing them against recorded seismograms.

Highlights

  • The broader purpose of this work is to produce site-specific broadband ground motions (

  • The choice of f j (k) alleviates the over-estimation of the high-frequency content typically encountered in empirical Green’s function (EGF)-based ground motion simulation methods

  • We have successfully presented a simple, intuitive, and effective method for generating broadband ground motions for engineering applications by superimposing long-period (>2 s) waveforms from spectral-element simulations with high-frequency waveforms from an empirical Green’s function approach

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Summary

Introduction

The broader purpose of this work is to produce site-specific broadband ground motions (

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