Comparison between the North and South Pacific Oceans of Acoustic Propagation in Secondary Sound Channels.

Abstract

This document is a summary of the extent and causes of secondary sound channel formation in the Pacific Basin. In the North Pacific above 40 deg North latitude and in the Western Pacific near the equator, both regions where the average precipitation is greater than evaporation, secondary sound channels due to temperature inversions are found over extensive areas. In the Central South Pacific and to a lesser extent in the Subantarctic region, secondary sound channels are principally caused by water mass intrusion. A third mechanism, circulation instability, is found locally near major currents and outflows throughout the Basin.

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Document Details

Document Type
Technical Report
Publication Date
Jul 07, 1986
Accession Number
ADA170880

Entities

People

  • David G. Browning

Organizations

  • Naval Underwater Systems Center

Tags

Communities of Interest

  • Energy and Power Technologies
  • Ground and Sea Platforms

DTIC Thesaurus Topics

  • Acoustic Propagation
  • Cold Water
  • Evaporation
  • Frequency
  • Instability
  • Intrusion
  • Inversion
  • Oceans
  • Pacific Ocean
  • Precipitation
  • Regions
  • Solar Heating
  • South Pacific Ocean
  • Subarctic Regions
  • Temperature Gradients
  • Temperature Inversion
  • Water Masses

Readers

  • Atmospheric Science/Meteorology
  • Oceanography.