Foucault-Wheatstone device in the deep-sea
Hans van Haren

TL;DR
This study uses a deep-sea pressure sensor to detect Earth rotation effects and mesoscale eddy influences through spectral peaks, revealing a mechanical resonance phenomenon akin to a Wheatstone device in the ocean.
Contribution
It demonstrates a novel application of a deep-sea mooring as a mechanical resonator revealing Earth rotation and mesoscale eddy effects through spectral analysis.
Findings
Detection of spectral peaks at sub-harmonics of near-inertial frequency.
Evidence of Earth rotation and mesoscale eddy influence on mooring tension.
Resonant signals suggest a mechanical oscillation similar to a Wheatstone device.
Abstract
A pressure sensor, located for 4 months in the middle of a 1275-m long taut deep-sea mooring in 2380 m water-depth above a seamount with sub-surface top-buoys and seafloor anchor-weight, demonstrates deterministic spectral peaks at sub-harmonics of the local near-inertial frequency. None of these frequencies can be associated with oceanographic motions. No corresponding peaks are found in spectra of other observables like water-flow (differences), temperature, and pressure in the top-buoys of the mooring. The mid-cable pressure sensor was mounted on a nearly 1-kN weighing non-swiveled frame. Its data seem to reflect a resonant mechanical oscillation of the tensioned mooring cable under repeated short-scale Strouhal vibrations induced by water-flow. Equivalent vertical motions of 0.5-m amplitudes are found dominant at frequency f*/4, with monotonically decreasing peaks at f*/2, 3f*/4 and…
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Taxonomy
TopicsGeophysics and Sensor Technology · Geological and Geophysical Studies · Seismic Waves and Analysis
