| Autor: |
Ainslie MA; JASCO Applied Sciences (Deutschland) GmbH, Mergenthaler Allee 15-21, 65760 Eschborn, Hesse, Germany., Andrew RK; Applied Physics Laboratory, University of Washington, Seattle, Washington 98105, USA., Howe BM; University of Hawaii at Manoa, Honolulu, Hawaii 96822, USA., Mercer JA; Applied Physics Laboratory, University of Washington, Seattle, Washington 98105, USA. |
| Abstrakt: |
The soundscape of the Northeast Pacific Ocean is studied with emphasis on frequencies in the range 63-125 Hz. A 34-year (1964-1998) increase and seasonal fluctuations (1994-2006) are investigated. This is achieved by developing a simple relationship between the total radiated power of all ocean sound sources and the spatially averaged mean-square sound pressure in terms of the average source factor, source depth, and sea surface temperature (SST). The formula so derived is used to predict fluctuations in the sound level in the range 63-125 Hz with an amplitude of 1.2 dB and a period of 1 year associated with seasonal variations in the SST, which controls the amount of sound energy trapped in the sound fixing and ranging (SOFAR) channel. Also investigated is an observed 5 dB increase in the same frequency range in the Northeast Pacific Ocean during the late 20th century [Andrew, Howe, Mercer, and Dzieciuch (2002). ARLO 3, 65-70]. The increase is explained by the increase in the total number of ocean-going ships and their average gross tonnage. |
