1. Fiber‐Optic Observations of Internal Waves and Tides
- Author
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Williams, E. F., Ugalde, A., Martins, H. F., Becerril, C. E., Callies, J., Claret, M., Fernandez‐Ruiz, M. R., Gonzalez‐Herraez, M., Martin‐Lopez, S., Pelegri, J. L., Winters, K. B., and Zhan, Z.
- Abstract
Although typically used to measure dynamic strain from seismic and acoustic waves, Rayleigh‐based distributed acoustic sensing (DAS) is also sensitive to temperature, offering longer range and higher sensitivity to small temperature perturbations than conventional Raman‐based distributed temperature sensing. Here, we demonstrate that ocean‐bottom DAS can be employed to study internal wave and tide dynamics in the bottom boundary layer, a region of enhanced ocean mixing but scarce observations. First, we show temperature transients up to about 4 K from a power cable in the Strait of Gibraltar south of Spain, associated with passing trains of internal solitary waves in water depth <200 m. Second, we show the propagation of thermal fronts associated with the nonlinear internal tide on the near‐critical slope of the island of Gran Canaria, off the coast of West Africa, with perturbations up to about 2 K at 1‐km depth and 0.2 K at 2.5‐km depth. With spatial averaging, we also recover a signal proportional to the barotropic tidal pressure, including the lunar fortnightly variation. In addition to applications in observational physical oceanography, our results suggest that contemporary chirped‐pulse DAS possesses sufficient long‐period sensitivity for seafloor geodesy and tsunami monitoring if ocean temperature variations can be separated. Distributed acoustic sensing (DAS) measures changes in the propagation time of light along finite segments of an optical fiber, which can be caused by both elastic deformations and temperature variations. We present two case studies of long‐period temperature signals recorded with DAS on submarine cables offshore southern Spain and in the Canary Islands. These temperature signals are associated with internal waves, gravity waves that propagate on the ocean's density stratification. We also recover a signal matching the tidal pressure, which likely represents elastic strain, suggesting potential value of ocean‐bottom DAS for seafloor geodesy and tsunami monitoring. Distributed acoustic sensing on seafloor cables can resolve temperature changes associated with internal wave and boundary layer dynamicsWe show temperature transients from solitons in the Strait of Gibraltar and from the propagation of internal tidal fronts at Gran CanariaWe also recover a signal proportional to barotropic tidal pressure including the fortnightly variation Distributed acoustic sensing on seafloor cables can resolve temperature changes associated with internal wave and boundary layer dynamics We show temperature transients from solitons in the Strait of Gibraltar and from the propagation of internal tidal fronts at Gran Canaria We also recover a signal proportional to barotropic tidal pressure including the fortnightly variation
- Published
- 2023
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