What Is a Tide Chart?
A tide chart (or tide table) is a prediction of water height at a specific coastal location over a period of days. It tells you two critical things: when the water will be at its highest and lowest points, and how high or low those extremes will be.
Tide charts are generated by analyzing astronomical patterns — primarily the gravitational pull of the Moon and Sun — and applying them to the known tidal behavior of a specific location. They are remarkably accurate: predictions are typically within a few minutes and centimeters of actual conditions, assuming normal weather.
Reading the Numbers: Times and Heights
Every entry in a tide table contains two numbers: a time and a height.
Time is when the tide reaches its high or low point. This is given in local time for the station's timezone. Be careful with daylight saving — tide tables in some regions do not automatically adjust.
Height is the water level above Chart Datum, measured in metres. A high tide of 2.4m means the water surface is 2.4 metres above the baseline. A low tide of 0.1m means only 10 centimetres of water above that same baseline — very shallow conditions.
What Is Chart Datum?
Chart Datum is the reference level from which all tide heights are measured. It is set to approximately the lowest astronomical tide (LAT) — the lowest level the tide is ever predicted to reach under normal conditions.
This means tide heights shown on a chart are always positive (or zero). A height of 0.0m doesn't mean dry land — it means the water is at its theoretical minimum level. The actual depth at any point also depends on the natural depth of the seabed at that location.
For practical use: a higher Chart Datum number = more water = safer for navigation and beach activities. A lower number = less water = better for beachcombing and tide pooling.
Understanding the Tide Curve Graph
Modern tide charts like those on TideTimes Global show a smooth curve — not just discrete high/low entries. This curve shows the predicted water height at every hour of the day.
The smooth S-curve between tides follows a pattern called the Rule of Twelfths: the tide moves slowly near its high and low points, then accelerates rapidly through the middle range. In the first hour after low tide, water rises by only 1/12 of the total range. By the third and fourth hours, it's rising at 3/12 per hour — the fastest point. It slows again in the final hours before high tide.
This matters practically: if you're watching the tide come in from a rock platform, the middle hours are when water rises fastest and can catch you off guard.
Tidal Range: The Difference Between High and Low
Tidal range is simply the difference between today's high tide height and low tide height. A high of 2.8m and a low of 0.3m gives a range of 2.5m.
Tidal range varies dramatically by location. Some areas experience tidal ranges of less than 0.5m (microtidal), while others like the Bay of Fundy in Canada can exceed 16m. The range also changes through the monthly lunar cycle: spring tides (near new and full moon) have larger ranges, while neap tides (near quarter moons) have smaller ranges.
Large tidal ranges create stronger currents, more exposed beach at low tide, and more dramatic changes in conditions.