Measurements of the angular dependence of acoustic seafloor scattering in sandy sites

  • 0Center for Acoustics Research and Education, University of New Hampshire, Durham, New Hampshire 03824, USA.

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Summary

This summary is machine-generated.

Seafloor scattering measurements reveal significant variability (up to 20 dB) in shallow waters. These findings highlight challenges in accurately modeling acoustic scattering from the seabed.

Area Of Science

  • Acoustics
  • Oceanography
  • Geophysics

Background

  • Seafloor acoustic scattering is crucial for underwater acoustics and sonar applications.
  • Understanding scattering mechanisms in shallow waters is complex due to environmental factors.

Purpose Of The Study

  • To analyze seafloor scattering strength in shallow coastal environments.
  • To compare experimental data with predictions from the small-slope approximation model.
  • To investigate the variability of scattering strength with environmental parameters.

Main Methods

  • Conducted long-term experiments (3 weeks to 5 months) in shallow waters near Portsmouth, NH.
  • Utilized a tripod-mounted transducer system (38, 70, 200 kHz) at a 17.5° grazing angle.
  • Measured environmental data (conductivity, temperature, depth) and seafloor roughness via stereo imaging.

Main Results

  • Seafloor scattering strengths exhibited variability up to ~20 dB for given frequencies, grazing angles, and grain sizes.
  • Averaged scattering strengths over calm periods between storm events.
  • Observed data-model differences, potentially due to model input uncertainties or uncaptured scattering mechanisms.

Conclusions

  • Experimental seafloor scattering data show considerable variability, challenging simple acoustic models.
  • Further research is needed to refine models and understand complex scattering processes in shallow marine environments.
  • Results provide valuable empirical data for validating and improving acoustic scattering models.