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Mean tidal range is calculated as the difference between mean high water (i.e., the average high tide level) and mean low water (the average low tide level).
An estimate of tide height at a time is possible using the rule of twelfths. In this method the tidal range is divided by twelve and it is assumed that the 1/12 of the range flows in the first hour, another 2/12 in the second hour, another 3/12 in the third hour, and so on.
The methods for the prediction of the tides may be classified as harmonic and nonharmonic. By the harmonic method the elementary constituent tides, represented by harmonic constants, are combined in to a composite tide.
Because the movements of the earth, moon, and sun are predictable, tide characteristics such as tide height, zero point, and mean lower low-water level are predictable. Tide height is usually measured from the low-water mark, which is considered the zero point.
By the nonharmonic method the predictions are made by applying to the times of the moons transits and to the mean height of the tide systems of differences to take account of average conditions and various inequalities due to changes in the phase of the moon and in the declination and parallax of the moon and sun.

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Factor = tidal range today / tidal range at mean springs In any nautical almanac (e.g. The Reeds Small Craft Almanac)
Tide-Predicting Machine No. 1 The terms of the equation, h = Ho + Sum{H cos[at + (Vo+u) - K]} , are defined as follows: h = height of tide at any time t. Ho = mean height of water level above datum used for prediction. H = mean amplitude of any constituent A.
NOAA Tide Predictions allows users of the Tides and Currents website () to generate tide predictions for up to 2 years in the past or future, at any of 3000+ locations around the United States.

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