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- W2037314984 abstract "A discussion of the sources of seafloor noise is most conveniently broken into four frequency bands since the noise is dominated by different physics in each of these bands. The first, and most familiar, band is from 3–50 Hz. This band is known as the very-low-frequency (VLF) or infrasonic band but is termed high-frequency noise for these puposes. The best documented mechanisms for the generation of ambient noise in this band is shipping. The next lower band, from 80 mHz to 3 Hz, is commonly called the microseism band after the high-level microseismic noise that is clearly recorded at all sites on the Earth's surface and results from nonlinear wave-wave interactions. The third band, the noise notch (20–80 mHz), has a variable bandwidth and is observed on both the continents and in the ocean. Noise levels within this notch appear to be controlled largely by currents and turbulence in the seafloor boundary layer. The final ultralow-frequency (ULF) band extends from dc to 20 mHz and the levels can be attributed to surface gravity waves. Very limited pressure and inertial displacement measurements have been made in the Pacific within these bands." @default.
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- W2037314984 date "1988-11-01" @default.
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- W2037314984 title "Ultralow‐ and very‐low‐frequency seismic and acoustic noise in the Pacific" @default.
- W2037314984 doi "https://doi.org/10.1121/1.2026071" @default.
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