SURFACE-GENERATED NOISE IN AN OCEAN WAVEGUIDE WITH A TRANSITION LAYER OF CONTINUOUSLY VARYING DENSITY AND SOUND SPEED

This paper considers the noise field generated by surface random processes in an oceanic environment with a sediment layer possessing a continuously varying density and sound-speed profile. This model closely resembles the oceanic waveguide environment and therefore enables the simulation of surface noise generation. Many results of the noise field were generated, including the noise intensity distribution, vertical and horizontal correlations. It is demonstrated that the noise intensity may be affected by the stratification mainly through the continuous spectrum, in that the continuous spectrum is equally important as the normal modes in the present analysis. Moreover, the results for the correlations show that the noise field in the horizontal direction becomes more coherent when the noise sources are more correlated, while in the vertical direction, the results tend to reverse. The horizontal correlations of the noise field due to surface random sources with nonisotropic power spectrum, such as nonisotropic Gaussian and Pierson–Moskowitz, were generated and analyzed.