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...

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Detalles Bibliográficos
Autores principales: Le Pape, Florian, Craig, David, Bean, Christopher J.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2021
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8058104/
https://www.ncbi.nlm.nih.gov/pubmed/33879800
http://dx.doi.org/10.1038/s41467-021-22591-5

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8058104/
https://www.ncbi.nlm.nih.gov/pubmed/33879800
http://dx.doi.org/10.1038/s41467-021-22591-5

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