Editing Speed of sound (section)

==Gradients==
{{Main|Sound speed gradient}}
When sound spreads out evenly in all directions in three dimensions, the intensity drops in proportion to the inverse square of the distance. However, in the ocean, there is a layer called the 'deep sound channel' or [[SOFAR channel]] which can confine sound waves at a particular depth.

In the SOFAR channel, the speed of sound is lower than that in the layers above and below. Just as light waves will refract towards a region of higher [[refractive index]], sound waves will [[refraction|refract]] towards a region where their speed is reduced. The result is that sound gets confined in the layer, much the way light can be confined to a sheet of glass or [[optical fiber]]. Thus, the sound is confined in essentially two dimensions. In two dimensions the intensity drops in proportion to only the inverse of the distance. This allows waves to travel much further before being undetectably faint.

A similar effect occurs in the atmosphere. [[Project Mogul]] successfully used this effect to detect a [[nuclear explosion]] at a considerable distance.