One Approach to Make the Most of the Method's Potential

The CCA method, one of the analysis methods adopted in our codes, allows one to analyze waves of very long wavelengths when the SN ratios (signal-to-noise power ratios) are sufficiently good. Presence of noise sources near the seismic array lowers SN ratios, but it is difficult to control microtremor noise sources in urban areas where humans live and industries are active. The only solution would be to use "miniature arrays" with very small sizes (if the array lies within the reach of arms, it should be easy to ensure a calm environment in its surroundings, at least while the measurement is active [about 15 minutes]). The pictures in the top page show how we realized large SN ratios by using an array with a radius of just 30 cm. This array realized SN ratios in excess of 10,000, which made it possible to analyze wavelengths larger than 500 times the array radius (reference [6]).

 

A Knack for Setting Parameters

One major feature of the analysis methods adopted in our codes lies in their ability to analyze long wavelengths. A knack for setting analysis parameters to make the most of this feature is to make the segment duration as small as possible within the tolerable range that depends on the frequency band of interest you wish to look at. This measure is effective to extracting a large number of segments from observed waveforms that are contaminated by non-stationary noise, and helps to make as narrow as possible the bandwidth of smoothing with a spectral window. Spectral windowing can cause biases, which becomes a particularly critical problem in the analysis of long wavelength ranges (reference [3]).

 

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