Pensacola, FL tide chart

Pensacola's tide is read on Pensacola Bay at the city's waterfront, and it is a once-a-day tide: most days bring one high water and one low, with a mean range of about 1.2 feet that swells and shrinks over each fortnight.

Moving water sets the hour here. The NOAA gauge 4.5 km from the middle of Pensacola publishes 37 harmonic constants. Mean range is 1.2 ft, and the form factor — diurnal constituents over semidiurnal — is 11.25, which is diurnal water.

Tide times and heights in Pensacola

The curve answers a question the table cannot. A table gives the minute of high water; the curve gives the hour you can actually get out — the stretch between one turn and the next that no row describes, and on a diurnal coast that is most of the fishing day.

What the tide does at Pensacola

The beach keeps a different clock. NOAA's predictions for the Pensacola Beach pier, on the Gulf eleven kilometres south-east, run close to two hours ahead of the bay at high water and about two and a half at low; for the surf side of Santa Rosa Island this table is late by about that much.

By this page's own synthesis over the nineteen-year cycle the water at the waterfront ranges from about one foot below mean lower low water to about two feet above it. On the smallest days of the fortnight it hardly moves at all, and the minute of the turn means little.

What the heights are measured from

Every height here is feet above mean lower low water. That reference is not the sea bed and not the water under your keel — it is the average of the lowest low water of each tidal day, taken over a nineteen-year epoch. A printed low water of 1.3 ft means the surface stands 1.3 feet above that line, not that there is 1.3 feet of water.

The useful consequence is that NOAA measures its charted depths from the same line. A sounding of four feet with a 1.3 ft tide is about 5.3 feet of water at that moment, and the same sounding at a −0.4 ft tide is about 3.6. Mixing the two references is the single most common way to read a tide table wrong.

Why the range swells and shrinks at Pensacola

Most days Pensacola gets a single high water and a single low water, and what sets the size of that one tide is the Moon's declination rather than its phase. When the Moon stands far north or south of the equator the day's range is at its largest; when it crosses the equator, about every two weeks, the two daily pulls cancel and the water barely moves, sometimes turning twice in a day by a few hundredths of a foot.

That is why a mean range of 1.2 ft says less here than on a twice-a-day coast: the fortnight runs from days well above it to days with almost no tide at all, and the Sun's spring-and-neap rhythm barely registers. The same calculation at Juneau, AK gives a mean range of 13.74 ft against 1.2 ft here — the same Moon and Sun acting on a different coast, with a different amount of water moving through it.

How close these numbers are to NOAA

These are not NOAA's published predictions. The station publishes 37 harmonic constants — amplitudes and phases of the periodic pulls that make up the tide here — and we synthesise the curve from them. Saying so is easy; the number that follows is the part that is worth reading.

Against NOAA's own predictions for August 12–19, 2026, every one of the 17 high and low waters matched, with an average difference in time of 2.14 minutes and a worst case of 5.5. The worst height difference was 1.5% of the day's range. That is the whole claim, and it is smaller than the width of the pencil line on a printed table.

Two limits belong with that number. It is a week of comparison, not a year, and it is this station: the same method run at a station with a big, awkward range does measurably worse, and our own worst case on the grid is off by minutes rather than seconds. Where that is true, the page says so, and the method behind every number on this site is written out rather than summarised.

When a tide table is not the right tool

A tide prediction is astronomy, and the water is weather as well. Wind and barometric pressure move the real level against the printed one: a hard onshore blow holds water in and makes a predicted low shallower and later, and a cold, dry high-pressure spell does the opposite. NOAA publishes observed levels alongside its predictions for exactly this reason. The numbers here are also the station's water, not the water two miles up a tidal creek, where the same tide arrives later and smaller. On rivers a spring freshet outweighs the tide outright.

Tide is the hour; it does not tell you which hour is worth taking. The reasoning behind the solunar windows — and what they are worth on a coast where moving water already sets the hour — is in best fishing times. The rest of the grid is catalogued on the fishing forecast hub. A printed page is also poor company in a creek at first light, and which fishing apps actually carry tide tables is a separate comparison.

The nearest stations this site carries are Cedar Key, FL (2.83 ft), St. Petersburg, FL (1.59 ft), Fernandina Beach, FL (6.02 ft) and Galveston, TX (1.46 ft), and the full list with the station behind each one is on the tide charts hub.