The oceans are notoriously opaque, providing the submarine with a strong veil of stealth. The only thing that oceans don't effectively block is sound, which is transmitted more effectively through water than it is through air. As a result, sonar remains the main method of detecting submarines, either in active form, producing sound that bounces off the target and is reflected back, or in passive form, listening for noise from the target. But sound doesn't travel through the ocean in a straightforward way, and as sonar has grown more sophisticated, its operators have had to contend with effects that either attenuate the sound, drown it out or bend it in surprising ways.

The Deep Scattering Layer (green) on a sonar scan
Attenuation can come from a number of sources. Obviously, the intensity of a sound weakens as it spreads out from its source, and in an infinite ocean, this would follow the inverse square law. In practice, it's often lower than this, thanks to effects discussed later, but the ocean doesn't transmit sound perfectly. Some is absorbed and turned into heat, a process that occurs more strongly at higher frequency. Some is scattered when it runs into discontinuities, which can be the surface and bottom of the sea or solid objects in the ocean, usually marine life. Most notable is the deep scattering layer, composed of deep-sea fish and the plankton they feed on that tend to cluster a thousand feet or so below the surface. Scattering is a particular problem for active sonar, as the reverberations from the surface/bottom/creatures can make it hard to pick up the actual return. Read more...
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