Side scan sonar transmits sound pulses sideways to map the seafloor, imaging object shape, texture, and shadows rather than depth.
A wreck sits invisible to a camera and unreliable on a depth sounder, but side scan sonar turns it into a two-tone image: it listens for how hard the seafloor and objects reflect sound back, not how deep the water is. That distinction defines what the tool is good at — and where it stops being the right instrument.
How Side Scan Sonar Builds An Image
Side scan sonar transmits a fan-shaped acoustic pulse down and out to one side of the vessel or towfish, then records echo strength and timing to assemble a continuous strip picture of the seabed.
Hardware is three parts: a submerged towfish, a transmission cable, and a topside unit that processes and displays returns. As the platform moves, successive pulses stitch into one long plan-view image rather than a single snapshot.
Two values drive each pixel. Time between transmit and receive gives range; echo strength (acoustic reflectivity) sets brightness. Hard, rough, or exposed objects — steel, rock, a hull rib — usually return strongly, while mud and fine sand swallow sound. Material, roughness, slope, and orientation all shift the result, so brightness alone never tells you what something is made of.
Objects also cast acoustic shadows where little or no sound returns — often the most useful clue, hinting at height and profile a flat echo would hide. Don’t assume light and dark always mean the same thing: NOAA notes contrast conventions vary by system and processing, so interpret against the display in front of you.
Frequency And Range: The Trade You Always Make
Higher frequency gives finer detail over a shorter distance; lower frequency sweeps wider at lower resolution — a trade-off no setting eliminates.
A National Marine Sanctuary description lists 100–500 kHz as common, confirming that raising frequency sharpens resolution while cutting range. Rough bands: about 50–100 kHz for broad coverage, and 500 kHz up to 1 MHz for small areas where detail matters more than swath. The Klein 5900 technical description, revision 6.0, shows what a real spec sheet looks like.
| Klein 5900 Spec | Published Value |
|---|---|
| Operating frequency | 600 kHz |
| Maximum range per side | 150 m (300 m swath) |
| Along-track resolution | 6.2 cm at 50 m; 15 cm at 120 m |
| Operating speed | 2–12 knots |
| Recommended towfish height | 10–15% of sonar range |
| Maximum operating depth | 750 m |
| Water temperature range | −2°C to +35°C |
Those numbers are model-specific, not a universal standard. Comparing units before a survey? Our roundup of tested side scan sonar systems lines up real specs side by side. For the underlying physics, NOAA’s side scan sonar overview covers the acoustic principles in plain terms.
Running A Survey Without Garbage Data
Clean data comes from a steady, straight track at controlled speed and correct towfish height — sloppy piloting is the fastest way to blur a good image.
- Pick frequency and range for the coverage-versus-detail balance your target needs.
- Deploy the towfish from the vessel or mount a hull unit; towfish is conventional.
- Hold constant speed and a straight line — side scans image well only on consistent tracks.
- Keep altitude near 10–15% of range on the Klein 5900, and follow your model’s published limits.
- Record both channels; review the processed image for targets, texture shifts, and shadows.
- Confirm target position and depth with a single-beam or multibeam system — side scan alone generally can’t establish depth.
Massachusetts’ Side Scan Sonar SOP, edition 3, is a published field procedure worth reading as a model, and the state’s standard operating procedure walks through deployment and documentation.
Where Side Scan Sonar Falls Short
Side scan sonar maps reflectivity, not bathymetry, so it cannot replace a depth sounder when depth data is legally or operationally required. The most frequent error is reading the image like a chart; another is trusting advertised range as guaranteed detection range — real performance shifts with frequency, seabed type, water conditions, geometry, vessel motion, and processing. Towing too high, too low, or too fast ruins resolution, and running past a unit’s depth limit (750 m on the Klein 5900) is a hard stop, not a guideline. Pair side scan with a depth-measuring system and the picture stays honest.
Common Questions
Does Side Scan Sonar Measure Water Depth?
No. It records acoustic reflectivity and target presence on the seabed, not bathymetric depth. Surveyors needing least-depth or charted depth figures pair it with single-beam or multibeam sonar. The side-scan image tells you what is down there and roughly how tall it stands via shadows, while a separate sounder supplies the depth number.
Why Do Some Objects Look Bright And Others Dark?
Brightness reflects echo strength, which depends on material, surface roughness, slope, orientation, and how the system processes and displays returns. Hard, rough targets usually return strongly and appear prominent; soft sediment absorbs sound and stays faint. Since contrast conventions vary between systems, interpret an image against that unit’s own display settings.
Can Side Scan Sonar Run At Any Boat Speed?
No — speed is model-specific and must come from the manufacturer’s documentation. The Klein 5900 lists 2 to 12 knots, and pushing past a unit’s published limit degrades along-track resolution and coverage. Consistent, straight tracks at controlled speed matter as much as the number itself.
Sources
- NOAA Ocean Explorer. “Side Scan Sonar” Explains acoustic imaging principles and reflectivity.
- Klein Marine Systems. “Klein 5900 Technical Description, Rev. 6.0” Source of frequency, range, speed, altitude, and depth specifications.
- Commonwealth of Massachusetts. “Side Scan Sonar Standard Operating Procedure, Edition 3” Field workflow and dual-frequency system reference.