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Sidescan sonars work by projecting a narrow beam of sound to either side of a towfish and recording the strength and time of the returned echo. The strength of the echo depends on a number of parameters including the operating frequency of the sonar and the distance to the seafloor, the angle of incidence of the sound, the slope of the seafloor being ensonified (or insonified), and the type of substrate. |
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To produce the fan-shaped beam of sound shown in yellow in Figure 3, sidescan arrays are long in the along-track direction and narrow in the across-track direction (see Figure 2). In general, the longer the array, the narrower the along-track angular width of the sonar fan-shaped beam. Array length also varies as a function of operational frequency; lower frequency systems need to have longer arrays than higher frequency systems. Here’s an example of a row of transducer elements from the University of Hawaii’s (UH’s) IMI-30 sonar: |
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