Sea & Rail

Tides & Water Levels

How water level people and mariners talk about the rise and fall of the sea.

  • 106 terms
  • 27 shop talk
  • 8 topics

The language of tides and water levels belongs to a wide crowd: water level observers and tide gauge technicians, oceanographers fitting harmonic constituents, hydrographers reducing soundings to chart datum, coastal engineers designing seawalls, port pilots timing deep-draught ships, flood forecasters and every fisherman with a tide book in the truck. Each group adds its own layer, from the formal datums of MLLW and MHHW to the dockside shorthand of the low-low and the top of the tide.

What makes the vocabulary distinctive is its precision about two things outsiders blur together. The first is vertical reference: insiders never quote a height without its datum, and they know that mean sea level, chart datum and the land vertical datum are different zeros that drift apart along a coast. The second is the split between height and flow. A tide rises and falls, while a tidal current or stream floods and ebbs, so the stand of the tide and slack water are separate events that rarely happen at the same moment in an estuary.

You hear the measurement side on piers and in data centres, where observers talk about bubblers, stilling wells, staff shots, closing the loop on a level run and six-minute data that has flatlined. You hear the theory side in analysis rooms, where M2, K1 and the nodal cycle explain why predictions shift from year to year. The weather side shows up as residuals, storm surge, set-down and seiches, and in the yearly count of high tide flooding days.

On the water, the talk is saltier and more colourful: fair and foul tides, wind against tide on the bar, tidal gates off headlands, boats neaped on a falling spring, minus tides for clam digging and king tides lapping into parking lots. A newcomer who can explain spring and neap tides, read a mixed tide table and tell a storm tide from a storm surge will be taken seriously on any dock or survey launch.

Who talks like this: Tide gauge technicians, water level observers, physical oceanographers, hydrographers, geodetic surveyors, coastal engineers, harbour masters, marine pilots, flood forecasters, sailors and commercial fishermen.

Start here: ten words every newcomer needs

Overheard on the job

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

Datums & Benchmarks

14 terms

The tidal and land datums that give water levels a fixed zero, and the marks that preserve them.

Tidal Theory & Constituents

15 terms

The astronomy, forces and harmonic constituents behind the rise and fall of the sea.

Tide Types & Cycles

14 terms

Daily and fortnightly patterns: semidiurnal, diurnal and mixed tides, springs, neaps and their quirks.

Tidal Currents

17 terms

The horizontal side of the tide: flood, ebb, slack and the words mariners use to time them.

Gauges & Measurement

14 terms

Tide gauges, staffs, levelling and current profilers, plus the field slang of water level observers.

Analysis & Prediction

9 terms

Harmonic analysis, tide tables and the methods that turn raw records into forecasts and datums.

Surge & Sea Level

10 terms

Storm surge, set-down, seiches and the long-term sea level trends recorded at tide gauges.

Dock & Field Talk

13 terms

Waterfront and boating talk about tides, from king tides and minus tides to neaped boats.

Frequently asked questions

What is the difference between MLLW and mean sea level?

Mean lower low water is the average of the lowest low tide of each day over a 19-year epoch, and it is the zero for US charts and tide tables. Mean sea level is the average of all hourly heights over the same epoch, so it sits roughly midway up the tidal range. At a station with a 2 m range, mean sea level sits about a metre above MLLW.

What is the difference between slack water and the stand of the tide?

Stand is the pause in water level at high or low tide; slack water is the pause in the current as it reverses. In many estuaries the two do not coincide, because the tide travels as a progressive wave and the strongest current flows near high and low water. Anyone planning a transit or a dive needs the current predictions, not the height table, to find slack.

Why are there spring and neap tides?

The Moon and Sun each raise their own tide. Around new and full moon they line up and reinforce each other, giving spring tides with large ranges; around the quarter moons they act at right angles and partly cancel, giving neap tides with small ranges. The cycle repeats every 14.77 days all year round. The word spring refers to the water springing up, not to the season.

What is a harmonic constituent in tide prediction?

A harmonic constituent is one regular wave within the tide, with a period fixed by the motions of the Moon and Sun. M2, the main lunar half-day tide, repeats every 12.42 hours, while K1 and O1 drive once-daily tides. Analysis of a gauge record gives each constituent's local amplitude and phase, and adding dozens of them together produces the predictions in published tide tables.

What is the difference between storm surge and storm tide?

Storm surge is the extra water a storm adds above the predicted tide, from wind pushing water toward the coast and low pressure lifting the sea surface. Storm tide is the total water level actually reached, surge plus astronomical tide. A 2 m surge at low tide can produce a lower storm tide than a 1 m surge arriving at spring high water, which is why forecasters quote both.

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