Abstract
To many ocean acousticians, shallow water is “water a few acoustic wavelengths in depth, where the normal mode description of the sound field is efficient.” To some of our physical oceanographer friends, shallow water is taken as the portion of the sea that extends from the shore to the continental shelf break. A rather jaundiced geologist once described the entire water column (including shallow water) as “a bothersome thin layer of fluid that obscures the really interesting part of the ocean.” All these definitions have some merit (including the last, if you are a geologist), but they are not the definition we will use. Rather, we will be looking at the region from the end of the surf zone out to the continental shelf break (and even onto the slope to ~500 m depth) as our working definition of shallow water. This is done for pragmatic reasons, having to do with the types of sonar systems that work for given purposes in those depths. Acoustically, we will be looking at sound and sonar systems working from ~50 Hz up to about 5 kHz. Incorporating these limits on depth and frequency bounds our technical area of “shallow water acoustics,” but even with these limits, the field is a rather vast one.
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Katsnelson, B., Petnikov, V., Lynch, J. (2012). What Is Shallow Water Acoustics?. In: Fundamentals of Shallow Water Acoustics. The Underwater Acoustics Series. Springer, Boston, MA. https://doi.org/10.1007/978-1-4419-9777-7_1
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