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Area of Science:

  • Oceanography
  • Acoustics
  • Wave dynamics

Background:

  • Surface wave breaking is a significant source of oceanic noise.
  • A mid-frequency planar array (130m depth, 1m aperture) can detect these events acoustically at 5-6 kHz.
  • Beamforming alone has limitations in accurately tracking sources due to array geometry.

Purpose of the Study:

  • To develop and validate a method for accurately tracking the trajectories of large surface wave breaking events.
  • To overcome the limitations of traditional beamforming for source localization in this context.

Main Methods:

  • Splitting the planar array into sub-arrays.
  • Beamforming each sub-array toward the acoustic source.
  • Computing temporal cross-correlations of sub-array beams to estimate source location.

Main Results:

  • Successfully estimated source tracks of wave breaking events.
  • The estimated trajectories closely matched those observed in aerial imagery.
  • The cross-correlation method enhanced tracking accuracy compared to beamforming alone.

Conclusions:

  • Acoustic tracking of surface wave breaking is feasible using sub-array cross-correlation techniques.
  • This method provides accurate trajectory estimation, complementing visual observations.
  • The findings have implications for acoustic monitoring of ocean surface processes.