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- W1518768792 abstract "In seismology, most of researches have been investigated by analyzing major seismic ‘signals’, for instance, body waves and surface waves. Aki [1] first introduced ‘coda’ waves, which had long been recognized as ‘noise’, consisting of scattered S-waves during propagation through the heterogeneous Earth media. Since then, a number of studies have been conducted to measure medium heterogeneity using coda waves over the world (e.g. [2]). Another revolu‐ tionary research dealing with ‘noise’ in seismology has been reported by [3]. The authors introduced a remarkable method to determine surface wave velocity examining long sequen‐ ces of seismic ambient noise. It gives us a great opportunity to explore velocity structures underneath by nothing but listening to noise." @default.
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- W1518768792 date "2013-03-20" @default.
- W1518768792 modified "2023-10-18" @default.
- W1518768792 title "Seismic Ambient Noise and Its Applicability to Monitor Cryospheric Environment" @default.
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- W1518768792 doi "https://doi.org/10.5772/55670" @default.
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