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      Source level and calling depth distributions of migrating bowhead whale calls in the shallow Beaufort Sea.

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          Abstract

          Automated and manual acoustic localizations of migrating bowhead whales were used to estimate source level and calling depth distributions of their frequency-modulated-modulated calls over seven years between 2008 and 2014. Whale positions were initially triangulated using directional autonomous seafloor acoustic recorders, deployed between 25 and 55 m water depth near Kaktovik, Alaska, during the fall westward migration. Calling depths were estimated by minimizing the "discrepancy" between source level estimates from at least three recorders detecting the same call. Applying a detailed waveguide propagation model to the data yielded broadband source levels of 161 ± 9 dB re 1 μPa2 s at 1 m (SEL) for calls received between 20 and 170 Hz. Applying a simpler 15 log10(R) power-law propagation model yielded SEL source levels of 158 ± 10 dB. The most probable calling depths lay between 22 and 30 m: optimal depths for long-range acoustic signal transmission in this particular environment.

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          Author and article information

          Journal
          J. Acoust. Soc. Am.
          The Journal of the Acoustical Society of America
          Acoustical Society of America (ASA)
          1520-8524
          0001-4966
          December 2016
          : 140
          : 6
          Affiliations
          [1 ] Marine Physical Laboratory, Scripps Institution of Oceanography, University of California San Diego, La Jolla, California 92093-0238, USA.
          [2 ] Greeneridge Sciences, Incorporated, 90 Arnold Place, Suite D, Santa Barbara, California 93117, USA.
          [3 ] University of New Hampshire, 24 Colovos Road, Durham, New Hampshire 03824, USA.
          [4 ] Shell Exploration and Production Company, 3601 C Street, Anchorage, Alaska 99503, USA.
          Article
          10.1121/1.4968853
          28040014
          28af31f3-1789-49c1-ab62-fb29df5fc1b2
          History

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