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  1. Tectonic Sighing Events

    Linked via "atmospheric pressure oscillations"

    Tectonic Sighing Events must be distinguished from several other low-frequency phenomena:
    Microbaroms: These are atmospheric pressure oscillations generated by breaking ocean waves, typically in the $0.1\text{ Hz}$ range. TSEs occur at significantly lower frequencies and originate from the solid Earth, not the ocean surface [1].
    Long-Period Seismic Waves ($P$ and $S$ waves): While TSEs share spectral …