Display options
Cite
Heaney KD, Prior M, Campbell RL. Bathymetric diffraction of basin-scale hydroacoustic signals. J Acoust Soc Am. 2017;141(2):878doi: 10.1121/1.4976052.
Heaney, K. D., Prior, M., & Campbell, R. L. (2017). Bathymetric diffraction of basin-scale hydroacoustic signals. The Journal of the Acoustical Society of America, 141(2), 878. https://doi.org/10.1121/1.4976052
Heaney, Kevin D, et al. "Bathymetric diffraction of basin-scale hydroacoustic signals." The Journal of the Acoustical Society of America vol. 141,2 (2017): 878. doi: https://doi.org/10.1121/1.4976052
Heaney KD, Prior M, Campbell RL. Bathymetric diffraction of basin-scale hydroacoustic signals. J Acoust Soc Am. 2017 Feb;141(2):878. doi: 10.1121/1.4976052. PMID: 28253706.
Copy Download .nbib Format: NLM
Share it on

J Acoust Soc Am. 2017 Feb;141(2):878. doi: 10.1121/1.4976052.

Bathymetric diffraction of basin-scale hydroacoustic signals.

The Journal of the Acoustical Society of America

Kevin D Heaney, Mark Prior, Richard L Campbell

Affiliations

  1. Ocean Acoustical Services and Instrumentation Systems, Inc., 11006 Clara Barton Drive, Fairfax Station, Virginia 22039, USA.
  2. International Data Centre, Comprehensive Test Ban Treaty Organization, United Nations, Vienna, Austria.

PMID: 28253706 DOI: 10.1121/1.4976052

Abstract

The ocean is nearly transparent to low frequency sound permitting the observation of distant events such as earthquakes or explosions at fully basin scales. For very low frequency the ocean acts as a shallow-water waveguide and lateral variability in bathymetry can lead to out-of-plane effects. In this paper, data from the International Monitoring System of the Comprehensive Test Ban Treaty Organization (CTBTO) is used to present two cases where robustly localized seismic events in locations clearly within the two-dimensional (2-D) shadow of a continent or large island generate T-phase signals that are received on a hydro-acoustic station. A fully three- dimensional parabolic equation model is used to demonstrate that lateral variability of the bathymetry can lead to diffraction, explaining both observations. The implications of this are that the CTBTO network has greater coverage than predicted by 2-D models and that inclusion of diffraction in future processing can improve the automatic global association of hydroacoustic events.

Publication Types