Understanding forecasts

How tide times are calculated

A page to understand the calculation logic, the displayed data and the natural limits of a tide forecast.

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The tide cycle

Displayed tide times are astronomical forecasts. They are produced from the motion of the Moon and Sun, reference stations, and parameters describing the local tide response.

The method uses harmonic analysis, a scientific approach that represents sea-level variation as a combination of cycles, without constituting an official certified publication.

Example tide curve over 24hWater levelMean level

The calculation in 4 steps

  1. 1

    Choose a reference station

    Each place is associated with a station or reference point when one is available.

  2. 2

    Rebuild the astronomical curve

    Harmonic constituents describe the main astronomical cycles influencing that station. Combined with local parameters, they make it possible to estimate the evolution of sea level.

  3. 3

    Detect high and low tides

    The high and low points of that curve are detected to determine high tides and low tides.

  4. 4

    Display local time and limits

    Times are then displayed in the time zone associated with the station.

What are harmonic constituents used for?+

They describe how a station responds to the main astronomical cycles. They make it possible to estimate a forecast curve for sea level without representing every locally observed condition on their own.

What is displayed

Place pages display available high tides, low tides, heights and coefficients over 15 days.

The reference station or attachment point is shown to help understand where the forecast comes from.

Heights and coefficients are displayed when the available references allow a consistent estimate.

Limits to know

An astronomical forecast does not describe every local condition at sea. Atmospheric pressure, wind, swell and local configuration can affect the level actually observed.

Differences may also appear when a place is attached to a nearby station rather than an exact measurement point.

For any activity at sea, tide-time reading should be completed with local conditions, marine weather and harbor guidance.

Frequently asked questions

Useful answers before interpreting tide times.

Is the method scientific?+

Yes. It is based on harmonic tide analysis, which models the astronomical evolution of sea level from known cycles.

Why can there be a difference from the observed tide?+

Weather, pressure, wind, swell, coastline shape and attachment to a reference station can all influence the level actually observed.

How should these tide times be used?+

They provide a clear reading of the tide trend for a place. For a sea trip or sensitive decision, they should be completed with available local information.

Sources and references

SourceNatureUsage on the siteCoverage
Reference stationsAstronomical and local parametersBasis for forecast calculation, time zone and place attachmentStations used for published places
Reference levels for coefficientsHeight and tidal-range markersCoefficient estimation when that reference existsPorts covered by that reference
Place reference setGeographic attachment dataPlace URL, place type, station or attachment pointPorts, cities and beaches published on the site
Forecasts calculated by the siteResults produced by the modelTide times, heights and coefficients over 15 daysPlaces linked to an active station

Each place page displays the station or attachment point used, the tide events and the applied time zone.