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Project Kiwi One: an acoustic cross-section of the South Pacific Ocean
The deep ocean sound channel is used to obtain very long range (typically >2,000 km) acoustic transmission 1 via totally refracted propagation paths (SOFAR propagation 2 ). Such experiments can therefore determine the acoustic transmission properties of large areas of ocean 3 . Those acoustic pro...
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Published in: | Nature (London) 1979-12, Vol.282 (5741), p.820-822 |
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Main Authors: | , , , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites |
Online Access: | Get full text |
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Summary: | The deep ocean sound channel is used to obtain very long range (typically >2,000 km) acoustic transmission
1
via totally refracted propagation paths (SOFAR propagation
2
). Such experiments can therefore determine the acoustic transmission properties of large areas of ocean
3
. Those acoustic propagation experiments can be used to locate major ocanographic changes
4
and to identify specific water masses
5
. A 10,000-km underwater sound transmission experiment conducted between New Zealand and Peru to obtain an acoustic cross-section of the South Pacific Ocean is described here. Three distinct regions of transmission loss were found. The highest attenuation, which is attributed to Antarctic intermediate water, occurred in the central South Pacific Ocean. |
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ISSN: | 0028-0836 1476-4687 |
DOI: | 10.1038/282820a0 |