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Abstract

An important part of the study of the space-time variation of earthquake ground motions is to analyze and model the frequency-dependent correlation function of accelerograms recorded at different spatial location. The correlation function between the harmonic components of two accelerograms at a specified frequency, known as the frequency-dependent correlation function, is closely related to the coherency spectrum. Using this relationship and the conventional method of estimating coherency spectra, it is possible to estimate the frequency-dependent correlation functions of the accelerograms. In recent literature another technique for directly estimating frequency-dependent correlation functions has become popular. This "moving window" approach uses a narrow window in the frequency domain to obtain approximately harmonic components of accelerograms, and then estimates the correlation functions between these components as the frequency-dependent correlation functions. The relationship between this approach and the conventional method is derived. It is shown that unless precautions are taken to correct for time delays between the two accelerograms being analyzed, the moving window approach yields estimates with larger biases than those obtained by the conventional method. This feature is further illustrated through an example.