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Seismic Background
Linked via "oceanic microseisms"
Oceanic Microseisms
The dominant contributor to the seismic background in the frequency range of $0.05 \text{ Hz}$ to $0.5 \text{ Hz}$ is generally attributed to oceanic microseisms $\text{/entries/oceanic-microseisms/}$. These are generated primarily through two mechanisms:
Primary Microseisms (Infragravity Waves): These result from the interaction of continuous surface ocean waves $\text{/entries/surface-ocean-waves/}$ with abrupt topographical features $\text{/entries/topogra…