Sea & Rail

Hydrography & Charting

The working language of the people who measure the seabed and make the chart.

  • 109 terms
  • 28 shop talk
  • 8 topics

Hydrography is the measurement of the seabed for charts, ports and marine engineering, and its vocabulary comes from two directions at once. One is the formal language of survey standards and chart production: survey orders, TPU, chart datum, least depth, ENC cells and S-57 objects. The other is the talk of survey launches and processing rooms, where a gap in coverage is a holiday, a bad sounding is a flier, a mismatch between lines is a bust and a full day of parallel lines is mowing the lawn.

You hear this lingo on survey ships and launches, in port authority survey departments, dredging contractors, offshore survey crews and the cartographic offices that turn survey data into charts. Crews come from navies, merchant fleets, land surveying and marine science, which is why one team may say patch test, calibration and patch for the same morning's work, and why former Royal Navy surveyors still call themselves droggies years after leaving uniform.

What sets the language apart is its obsession with uncertainty and with the shallow side. Every sounding carries a horizontal and vertical error budget, every charting decision is shoal-biased, and every disagreement between overlapping lines must be explained before the data is trusted. Sound speed, tides, heave and timing are the usual suspects, so processors talk about refraction as smiles and frowns and know a wobble on sight.

Insiders reveal themselves in the details. They ask which frequency a channel depth came from because of fluff, they compare crosslines at nadir, they treat a DtoN as urgent rather than routine, and they know that a contact is not a wreck until it has been developed and given a least depth. Newcomers who learn the difference between bathymetry and a full hydrographic survey, and between a holiday and a dropout, will hold their own on any survey deck.

Who talks like this: Hydrographic surveyors, survey technicians, launch coxswains, data processors, nautical cartographers, port and dredging surveyors, naval hydrographers and offshore survey crews.

Start here: ten words every newcomer needs

Overheard on the job

Real-sounding lines from the floor, translated into plain English.

Survey Planning & Standards

18 terms

Survey orders, uncertainty limits, line plans and the coverage rules that decide when a survey is good enough.

Sonar & Acoustics

22 terms

Echo sounders, side-scan, towfish and the acoustic behaviour that turns pings into depths and images.

Positioning & Motion

19 terms

Satellite positioning, motion sensors, calibration and the vessel geometry behind every sounding.

Sound Speed & Vertical Reference

10 terms

Sound speed profiles, refraction, tides and the datums that give depths their meaning.

Processing & Data Quality

9 terms

Cleaning, gridding and the artefacts processors hunt down before data leaves the survey office.

Charts & Products

12 terms

Charts, ENCs, data standards and the cartographic rules that keep shoal water on the chart.

Features & Hazards

12 terms

Wrecks, rocks, shoals and the investigations that pin down their least depths.

Launch & Crew Talk

7 terms

Nicknames and boat talk heard on survey launches and in the processing room.

Frequently asked questions

What is the difference between multibeam and side-scan sonar?

A multibeam echo sounder measures depth: each ping produces hundreds of depths across a swath, all positioned and corrected for motion and sound speed. Side-scan sonar produces an image: it records how strongly the seabed and objects return sound to either side of a towfish, with shadows behind anything standing proud. Surveys often run both, using side-scan to find contacts and multibeam to measure their least depths.

What is a patch test in hydrographic surveying?

A patch test is the calibration run on a multibeam system after installation or whenever it is disturbed. Specific pairs of lines over flat seabed, slopes and distinct features isolate latency, pitch, roll and heading biases between the sonar and the motion sensor, and the results go into the vessel configuration. A skipped or rushed patch test leaves errors that surface later as busts, wobbles and misplaced features.

Why is chart datum set at low water?

Chart datum is set low, at Lowest Astronomical Tide in many countries or Mean Lower Low Water in the United States, so the charted depth is close to the least water a mariner will meet. The predicted tide is then nearly always added to the charted depth, which keeps any error on the safe side. A chart referenced to mean sea level would show depths that regularly vanish at low tide.

What does a hydrographer mean by a holiday or a flier?

A holiday is a gap in coverage where the sonar never measured the seabed, larger than the specification allows, and it must be filled with an infill line. A flier is the opposite problem: a sounding that exists but is wrong, sticking up or down from the real seabed because of noise, fish, bubbles or a false detection. Processors hunt both before a survey is accepted.

What is the difference between TVU and THU?

Both are parts of total propagated uncertainty, stated at 95 percent confidence. TVU, total vertical uncertainty, is how far a sounding's depth could be off, with an allowed limit that grows with depth using the a and b values of the survey order. THU, total horizontal uncertainty, is how far the sounding could sit from its recorded position. Tides and sound speed dominate TVU; heading and positioning dominate THU.

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