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How deep ocean-land coupling controls the generation of secondary microseism Love waves
Wind driven ocean wave-wave interactions produce continuous Earth vibrations at the seafloor called secondary microseisms. While the origin of associated Rayleigh waves is well understood, there is currently no quantified explanation for the existence of Love waves in the most energetic region of th...
Uloženo v:
| Vydáno v: | Nat Commun |
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| Hlavní autoři: | , , |
| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
Nature Publishing Group UK
2021
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| Témata: | |
| On-line přístup: | https://ncbi.nlm.nih.gov/pmc/articles/PMC8058104/ https://ncbi.nlm.nih.gov/pubmed/33879800 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41467-021-22591-5 |
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