Modelling sound propagation in the Southern Ocean to estimate the acoustic impact of seismic research surveys on marine mammals

• Published in: Geophysical Journal International
• Main Authors: Breitzke, Monika, Bohlen, Thomas
• Format: Text
• Language: English
• Published: Oxford University Press 2010
• Subjects: Marine Geosciences and Applied Geophysics; Southern Ocean
• Online Access: http://gji.oxfordjournals.org/cgi/content/short/181/2/818; https://doi.org/10.1111/j.1365-246X.2010.04541.x

Modelling sound propagation in the ocean is an essential tool to assess the potential risk of air-gun shots on marine mammals. Based on a 2.5-D finite-difference code a full waveform modelling approach is presented, which determines both sound exposure levels of single shots and cumulative sound exposure levels of multiple shots fired along a seismic line. Band-limited point source approximations of compact air-gun clusters deployed by R/V Polarstern in polar regions are used as sound sources. Marine mammals are simulated as static receivers. Applications to deep and shallow water models including constant and depth-dependent sound velocity profiles of the Southern Ocean show dipole-like directivities in case of single shots and tubular cumulative sound exposure level fields beneath the seismic line in case of multiple shots. Compared to a semi-infinite model an incorporation of seafloor reflections enhances the seismically induced noise levels close to the sea surface. Refraction due to sound velocity gradients and sound channelling in near-surface ducts are evident, but affect only low to moderate levels. Hence, exposure zone radii derived for different hearing thresholds are almost independent of the sound velocity structure. With decreasing thresholds radii increase according to a spherical 20 log 10 r law in case of single shots and according to a cylindrical 10 log 10 r law in case of multiple shots. A doubling of the shot interval diminishes the cumulative sound exposure levels by −3 dB and halves the radii. The ocean bottom properties only slightly affect the radii in shallow waters, if the normal incidence reflection coefficient exceeds 0.2.