Side scan sonar is a specialized sonar (SOund
NAvigation and Ranging) system for searching and detecting objects on the
seafloor. Like other sonars, a side scan sends out sound energy and analyzes
the return signal (echo) that has bounced off the seafloor or other objects.
In a side scan the transmitted energy is formed into the shape of a fan
that sweeps the seafloor from directly under the towfish to either side,
typically to a distance of 100 meters. The strength of the return echo
is continuously recorded creating a "picture" of the
ocean bottom where objects that protrude from the bottom create a dark
image (strong return) and shadows from these objects are light areas (little
or no return). While the shape of the seafloor and objects on it can be
well- depicted, most side scan systems can not provide any depth information.


Multibeam sonar systems provide fanshaped
coverage of the seafloor similar to side scan sonars, but the output data
is in the form of depths rather than images. Instead of continuously recording
the strength of the return echo, the multibeam system measures and records
the time for the acoustic signal to travel from the transmitter (transducer)
to the seafloor (or object) and back to the receiver. Multibeam sonars
are generally attached to a vessel, rather than being towed like a side
scan. Therefore, the coverage area on the seafloor is dependent on the
depth of the water, typically two to four times the water depth.


Search patterns are usually run as a series of parallel lines that ensure
overlapping coverage of the sidescan or multibeam sonar. Under certain
circumstances 200% coverage is obtained by running a second search pattern
perpendicular or parallel to the first over the same area.