The Coupled-Mode Method for Transmission Loss Calculation in a Range- Dependent Oceanic Environment

Abstract

This report presents the coupled normal mode model to calculate the propagation loss of low-frequency acoustic signals in a range-dependent shallow ocean. It also derives the equations to include the effects of the continuous spectrum and the environmental attentuation using the first and second order perturbation terms to the solution of the real eigenequation. The bottom is assumed to have no shear effects and an axially symmetric cylindrical coordinate system is used. Therefore, no bearing dependence of the environment is also assumed in this model. It has been found that the first order perturbation term is purely imaginary, providing the imagery part of the eigenvalues and eigenfunctions. The range-dependent environment is divided into a suitable number of range-independent segments, and the respective modes are calculated in order to couple them to account for the interchange of energy and heat to adjacent modes. A simple environment is used to display the importance of mode coupling in a range-dependent ocean environment. (edc)

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Document Details

Document Type
Technical Report
Publication Date
Feb 27, 1989
Accession Number
ADA219434

Entities

People

  • Juan I. Arvelo Jr.

Organizations

  • Naval Surface Warfare Center

Tags

Communities of Interest

  • Air Platforms
  • Energy and Power Technologies
  • Engineered Resilient Systems
  • Sensors

DTIC Thesaurus Topics

  • Absorption
  • Acoustic Properties
  • Acoustic Waveguides
  • Acoustic Waves
  • Acoustics
  • Computational Fluid Dynamics
  • Computational Science
  • Coordinate Systems
  • Elastic Properties
  • Elastic Waves
  • Partial Differential Equations
  • Reflection
  • Scattering
  • Seabed
  • Shallow Water
  • Standing Waves
  • Wave Equations

Fields of Study

  • Physics

Readers

  • Fluid Dynamics.
  • Ocean-Atmosphere Mesoscale Modeling, Data Assimilation, and Flux Boundary Layers
  • Wave Propagation and Nonlinear Chaotic Dynamics.