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the claim

Ocean and atmospheric microseisms are generated by ocean wave interactions on the sea floor.

the verdict
SUPPORTED
the evidence backs this
Recorded sources
4 sources for · 0 against

Counts group repeated records of the same source within each side. They do not measure evidence strength or source independence.

Ocean and atmospheric microseisms are generated by ocean wave interactions on the sea floor, a phenomenon well-documented by seismic and oceanographic studies.

The analysis

The retrieved literature consistently supports the premise that microseisms originate from ocean wave interactions, such as opposing gravity waves or wave-wave interactions coupling with the seafloor.

Evidence for · 4
Recorded source metadata

Williams EF, Fernández-Ruiz MR, Magalhaes R, Vanthillo R, Zhan Z, González-Herráez M, Martins HF. Distributed sensing of microseisms and teleseisms with submarine dark fibers.. 2019. https://doi.org/10.1038/s41467-019-13262-7

Paper [0] observes how opposing groups of ocean surface gravity waves generate double-frequency seismic waves on the sea floor, confirming classic microseism generation theories.

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More for · 3
Recorded source metadata

Florian Le Pape, David Craig, Christopher J. Bean. How deep ocean-land coupling controls the generation of secondary microseism Love waves. 2021. https://doi.org/10.1038/s41467-021-22591-5

Paper [2] discusses how wind-driven ocean wave-wave interactions produce continuous Earth vibrations at the seafloor known as secondary microseisms.

Recorded source metadata

Lin J, Fang S, He R, Tang Q, Qu F, Wang B, Xu W. Monitoring ocean currents during the passage of Typhoon Muifa using optical-fiber distributed acoustic sensing.. 2024. https://doi.org/10.1038/s41467-024-45412-x

Paper [5] notes that microseismic noise is induced by ocean surface gravity waves during major marine weather events.

Recorded source metadata

Nishida K. Ambient seismic wave field.. 2017. https://doi.org/10.2183/pjab.93.026

Paper [6] states that the ambient seismic wave field, including primary and secondary microseisms, is primarily excited by oceanic gravity waves and pressure fluctuations acting on the sea floor.

The paper trail · every fact has a biography
first checked02 Aug 2026
judged → SUPPORTED · 8702 Aug 2026
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