(Redirected from Deep sound channel)The 'SOFAR channel' (sound fixing and ranging channel), or 'deep sound channel' (DSC),
[ Navy Supplement to the DOD Dictionary of Military and Associated Terms, , , , Department Of The Navy, 2006, NTRP 1-02 ] is a region of water deep in the ocean centered on where the
speed of sound is at a minimum. The SOFAR channel acts as a
waveguide for acoustics, and low frequency
sound waves within the channel may travel thousands of miles before dissipating.
[1] This phenomenon is an important factor in
submarine warfare. The deep sound channel was discovered and described independently by Dr.
Maurice Ewing, and
Leonid Brekhovskikh in the
1940s.
[1]

Sound speed as a function of depth at a position north of Hawaii in the
Pacific Ocean derived from the 2005
World Ocean Atlas. The SOFAR channel axis is at ca. 750-m depth.
The SOFAR channel is centered on the depth where the cumulative effect of
temperature and
water pressure (and, to a smaller extent,
salinity) combine to create the region of minimum sound speed in the
water column. Pressure in the ocean increases linearly with depth, but temperature is more variable, generally falling rapidly in the main
thermocline from the surface to around a thousand meters deep, then remaining almost unchanged from there to the ocean floor in the
deep sea. Near the surface, the rapidly falling temperature causes a decrease in sound speed, or a negative
sound speed gradient. With increasing depth, the increasing pressure causes an increase in sound speed, or a positive sound speed gradient. The depth where the sound speed is at a minimum is called the sound channel axis.
Near
Bermuda, the sound channel axis occurs at a depth of around 1000 meters. In temperate waters, the axis is shallower, and at high latitudes (above about 60°N or below 60°S) it reaches the surface.
Sound propagates in the channel by
refraction of sound, which makes sound travel near the depth of slowest speed. If a sound wave propagates away from this horizontal channel, the part of the wave furthest from the channel axis travels faster, so the wave turns back toward the channel axis. As a result, the sound waves trace a path that oscillates across the SOFAR channel axis. This principle is similar to long distance transmission of light in an
optical fiber.
Mysterious low-frequency
sounds, attributed to
humpback whales and other baleen whales, are a common occurrence in the channel. Scientists believe humpback whales may
dive down to this channel and "sing" to communicate with other humpback whales many kilometers away.
During
World War II, Dr.
Maurice Ewing suggested that dropping a small metal sphere into the ocean, specifically designed to implode at the SOFAR channel, could be used as a secret distress signal by downed pilots.
[2]
The novel ''
The Hunt for Red October'' describes the use of the SOFAR channel in submarine detection.
The conjectured existence of a similar channel in the
upper atmosphere, theorized by Dr. Ewing, led to
Project Mogul, carried out from 1947 until late 1948.

Acoustic pulses travel great distances in the ocean because they are trapped in an acoustic "
wave guide". This means that as acoustic pulses approach the surface they are turned back towards the bottom, and as they approach the ocean bottom they are turned back towards the surface. The ocean conducts sound very
efficiently, particularly sound at low frequencies, i.e., less than a few hundred Hz.
References
1. The Heard Island Feasibility Test
2.
Sound Channel, SOFAR, and SOSUS
See also
★
Bathythermograph (BT)
★
Thermocline
★
SOSUS
★
Underwater acoustics
★
Ocean acoustic tomography
External links
★
The SOFAR or deep sound channel, from
NOAA
★
A sound pipeline, from the
National Academy of Sciences
★
SOSUS, the "Secret Weapon" of Underwater Surveillance by Edward C. Whitman. ''Undersea Warfare''