An Analysis of High-Frequency Ambient Noise
Abstract
Because of the high values of absorption and bottom-reflection losses, ambient noise in shallow water at frequencies above 30 kHz is considered to result almost entirely from wind and rain activity at the local sea surface. The ambient noise is thus effectively produced by a series of small radiators distributed over a plane surface, with the level and directionality of the sources being dependent on wind speed, rainfall, and frequency. In order to assess the form of signal processing to use in a high-frequency ambient-noise field, analytical expressions have been developed for the noise power in an omnidirectional hydrophone, for the horizontal and vertical spatial correlation functions, and for the noise power in an unshaded rectangular array.
Document Details
- Document Type
- Technical Report
- Publication Date
- Oct 01, 1982
- Accession Number
- ADA125308
Entities
People
- Lewis J. Lloyd
- Maurice J. Daintith
Organizations
- SACLANT ASW Research Centre