• DocumentCode
    3533051
  • Title

    Characteristics of underwater ambient noise at a proposed tidal energy site in puget sound

  • Author

    Bassett, Christopher ; Thomson, Jim ; Polagye, Brian

  • Author_Institution
    Northwest Nat. Marine Renewable Energy Center, Univ. of Washington, Seattle, WA, USA
  • fYear
    2010
  • fDate
    20-23 Sept. 2010
  • Firstpage
    1
  • Lastpage
    8
  • Abstract
    Ambient underwater acoustics data are presented for one year at a potential tidal energy site in Admiralty Inlet, WA (USA) with maximum currents exceeding 3 m/s. The site, at a depth of approximately 60 meters, is located near shipping lanes, a local ferry route, and a transit area for many cetacean species. A key finding is that the statistical distribution of total sound pressure levels are dependent on tidal currents at the site. Pseudosound, cobbles shifting on the sea bed, and vibrations induced by forces on the equipment are possible explanations. Non-propagating turbulent pressure fluctuations, termed pseudosound, can mask ambient noise, especially in highly energetic environments suitable for tidal energy development. A statistical method identifies periods during which changes in the mean and standard deviation of the one-third octave band sound pressure levels are statistically significant and thus suggestive of pseudosound contamination. For each deployment, recordings with depth averaged tidal currents greater than 1 m/s are found to be contaminated, and only recordings with currents below this threshold are used in the subsequent ambient noise analysis. Mean total sound pressure levels (0.156 - 30 kHz) over all recordings are 117 dB re 1μPa. Total sound pressure levels exceed 100 dB re 1μPa 99% of the time and exceed 135 dB re 1μPa 4% of the time. Commercial shipping and ferry traffic are found to be the most significant contributors to ambient noise levels at the site, with secondary contributions from rain, wind, and marine mammal vocalizations. Post-processed data from an AIS (Automatic Identification System) receiver is used to determine the location of ships during each recording. Referencing 368 individual recordings with the distance between the ferry and the site obtained from AIS data, the source level of the ferry is estimated to be 179 ± 4 dB re 1μPa at 1m with a logarithmic spreading loss coefficient - f 18.
  • Keywords
    acoustic noise; oceanographic regions; tides; underwater sound; AD 2009 05 to 2010 05; Admiralty Inlet; Puget Sound; USA; automatic identification system; cetacean species; frequency 0.156 kHz to 30 kHz; logarithmic spreading loss coefficient; pseudosound contamination; statistical distribution; tidal currents; tidal energy site; total sound pressure levels; turbulent pressure fluctuations; underwater acoustics; underwater ambient noise; Acoustics; Coherence; Frequency measurement; Marine vehicles; Noise; Sea measurements; Sonar equipment; Underwater acoustics; ambient noise; pseudosound; tidal energy;
  • fLanguage
    English
  • Publisher
    ieee
  • Conference_Titel
    OCEANS 2010
  • Conference_Location
    Seattle, WA
  • Print_ISBN
    978-1-4244-4332-1
  • Type

    conf

  • DOI
    10.1109/OCEANS.2010.5664380
  • Filename
    5664380