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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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| Publicado no: | Proc Jpn Acad Ser B Phys Biol Sci |
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| Autor principal: | |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
The Japan Academy
2017
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| Assuntos: | |
| Acesso em linha: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5713174/ https://ncbi.nlm.nih.gov/pubmed/28769015 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.2183/pjab.93.026 |
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