Lesson 1 of 7 · 1 min
Bridge Equipment — Echo Sounder
| Aspect | Detail |
|---|---|
| Principle | Transducer transmits an acoustic pulse downward; the echo is received after bouncing off the seabed. Time × speed of sound in water (approx 1500 m/s) ÷ 2 = depth |
| Transducer position | Located on the hull — typically at the bilge keel or keel. The displayed depth may be depth below the transducer (not below the keel). Know your vessel's transducer position: subtract keel-to-transducer distance from readings to get depth below keel |
| Speed of sound correction | Speed of sound varies with water temperature, salinity, and pressure. Echo sounders are calibrated for a standard value. In very shallow fresh water vs deep salt water the error is typically small — but note the limitation |
| False bottom | A second trace at about twice the true depth is a multiple echo — the pulse bouncing seabed–surface–seabed. A thermal layer (thermocline), the deep scattering layer or a dense fish shoal shows as a false trace above the true bottom. The OOW must identify the correct bottom trace |
| Limitations | Looks straight down only — it gives no warning of a wreck or rock ahead. It shows depth to the first strong reflector beneath the transducer, usually the bottom; by the time a wreck shows, you are over it. Minimal range at high speed in a seaway due to air bubbles under the hull. Requires UKC calculation to be meaningful |
| UKC calculation | Displayed depth − vessel draft = UKC. Example: echo sounder reads 18m, draft 4.5m = UKC 13.5m. Apply any tidal height correction if using chart datum |
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