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Ambient seismic wave field
The ambient seismic wave field, also known as ambient noise, is excited by oceanic gravity waves primarily. This can be categorized as seismic hum (1–20 mHz), primary microseisms (0.02–0.1 Hz), and secondary microseisms (0.1–1 Hz). Below 20 mHz, pressure fluctuations of ocean infragravity waves reac...
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
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The Japan Academy
2017
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| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5713174/ https://www.ncbi.nlm.nih.gov/pubmed/28769015 http://dx.doi.org/10.2183/pjab.93.026 |