“…(
2020), the utilization of a low‐frequency fibre optic hydrophone employing weak value amplification reveals remarkable sensitivity, allowing it to detect underwater acoustic disturbances as weak as 1.3
at 10 Hz. Therefore, the ES pressure field remains measurable with common seismic instruments such as fibre optic hydrophones (Buis et al.,
2014). Figure 3a shows that the main wave types in the ES pressure field are Scholte waves; other wave patterns (guided waves, reflected waves and refracted waves) are too weak to be observed.…”