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Analysis and Ranking of the Acoustic Disturbance Potential of ...

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Report No. 6945<br />

BBN Systems <strong>and</strong> Technologies Corporation<br />

Figure 4.8. Geometry for Air-to-Water Sound Transmission.<br />

surface, by non-acoustic (hydrostatic)" pressure transmission from <strong>the</strong> surface<br />

<strong>and</strong> from bottom reflections in shallow water.<br />

As a result, most <strong>of</strong> <strong>the</strong> acoustic energy transmitted into <strong>the</strong> water from<br />

a source in air arrives through a cone with a 26 degree apex angle which<br />

intersects <strong>the</strong> surface <strong>and</strong> traces a "footprint" directly beneath <strong>the</strong> path <strong>of</strong><br />

<strong>the</strong> source.<br />

For underwater observation points in shallow water within this cone <strong>the</strong><br />

directly transmitted sound energy is generally greater than <strong>the</strong> energy<br />

contribution from bottom reflected paths. At horizontal distances greater<br />

than 1 water depth from <strong>the</strong> boundary <strong>of</strong> <strong>the</strong> acoustic intercept cone on <strong>the</strong><br />

surface, <strong>the</strong> energy transmitted by reflected paths becomes dominant <strong>and</strong> is an<br />

important feature <strong>of</strong> air-to-water transmission in shallow water. Thus two<br />

terms become necessary in <strong>the</strong> air - water transmission model to predict<br />

underwater received levels for <strong>the</strong> full range <strong>of</strong> expected source - receiver<br />

*This has been called "evanescent wave" transmission by Urick <strong>and</strong> o<strong>the</strong>rs. It<br />

is important for transmission at low frequencies to receiver locations near<br />

<strong>the</strong> surface.

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