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Related Experiment Video

Updated: Jun 2, 2026

Tracking Infiltration Front Depth Using Time-lapse Multi-offset Gathers Collected with Array Antenna Ground Penetrating Radar
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Tracking Infiltration Front Depth Using Time-lapse Multi-offset Gathers Collected with Array Antenna Ground Penetrating Radar

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Ray-based description of shadow zone arrivals.

A L Virovlyansky1, A Yu Kazarova, L Ya Lyubavin

  • 1Institute of Applied Physics, Russian Academy of Science, 46 Ul'yanov Street, 603950 Nizhny Novgorod, Russia. viro@hydro.appl.sci-nnov.ru

The Journal of the Acoustical Society of America
|May 17, 2011
PubMed
Summary

Sound energy penetrates the geometric shadow zone in oceans due to internal wave scattering. Stochastic ray theory quantifies this effect, revealing how shadow zone arrivals extend with range.

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Tracking Infiltration Front Depth Using Time-lapse Multi-offset Gathers Collected with Array Antenna Ground Penetrating Radar
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Area of Science:

  • Underwater acoustics
  • Oceanography
  • Wave propagation

Background:

  • Internal waves cause sound speed variations in the ocean.
  • These perturbations scatter acoustic energy, affecting sound propagation over long distances.
  • Sound energy typically does not reach the geometric shadow zone.

Purpose of the Study:

  • To analyze the penetration of sound energy into the geometric shadow zone.
  • To develop analytical estimates for shadow zone arrival characteristics.
  • To understand the role of stochastic ray theory in describing chaotic ray behavior.

Main Methods:

  • Field experiments and numerical simulations.
  • Stochastic ray theory for statistical description of chaotic rays.
  • Analytical evaluation of probability density functions for perturbed rays.

Main Results:

  • Sound energy penetrates below the unperturbed timefront into the geometric shadow zone.
  • Shadow zone arrivals are continuations of timefront cusps.
  • Cusp extensions into the shadow zone grow with range as r(1/2).

Conclusions:

  • Internal wave scattering enables sound energy to reach previously shadowed regions.
  • Analytical estimates provide insights into the vertical extent and energy distribution within shadow zones.
  • The findings are applicable to steep rays in underwater acoustic environments.