Whether you’re heading out for a day of fishing, coastal cruising, or just anchored at a sandbar, the tide will have an impact. Ignoring it can lead to more than just a ruined afternoon. It can lead to running aground or being unable to clear a bridge.
Find out how to read a tide table and be prepared for fluctuating water levels and currents on coastal U.S. waters.
Tides are the rise and fall of sea levels caused by the gravitational pull of the moon and the sun, combined with the rotation of the Earth.
You’ve probably heard of high and low tides, but may not know exactly how they come into play when boating.
This is when the water is at its deepest, offering the most cushion over sandbars, rocks, and shallow inlets. While it’s the safest time to avoid running aground, it also reduces so-called “air draft”, meaning there is less clearance for your boat to pass under bridges.
At this stage, the water is at its shallowest, which can expose hidden hazards or leave you “high and dry” if you are anchored in a spot that was deep a few hours earlier.
As the water moves between these two states, it creates horizontal currents. An incoming (flood) tide pushes water toward the shore, while an outgoing (ebb) tide pulls it away, often creating strong flows in narrow channels that can significantly affect your boat’s speed and steering.
Most places in the U.S. experience two high tides and two low tides every lunar day (about 24 hours and 50 minutes). But tides don’t follow the same rhythm everywhere. Knowing your local pattern helps you avoid getting caught by a ‘low’ high tide.
A tide table from the NOAA shows three main types of information: Time, Tide and Height.
To use a tide table, you cross-reference the date of your trip with the times and heights listed to determine how much water you’ll have under your hull.
Source: NOAA
Tides are hyper-local. You’ll need a Tide Table specifically for the harbor or inlet you are navigating, not just the general region.
Check NOAA Tides and Currents for the most accurate, station-specific data in U.S. waters.
High and low times are indicated in separate columns.
If you notice a ‘missing’ high or low tide on your chart, don’t worry—it’s not a mistake! Because the tidal cycle lasts about 24 hours and 50 minutes (slightly longer than a standard day), the tide time occasionally ‘rolls over’ into the next calendar day. This is much like how the moon rises at a different time every night.
Most tables use a 24-hour (military) clock. For example, 14:30 is 2:30 PM.
The number next to the time (usually in feet) tells you how much the water level will rise above the “zero” depth shown on your GPS or paper chart.
In the U.S., tide heights are measured relative to MLLW (Mean Lower Low Water). If the table says the tide is -0.5 ft, it means the water is half a foot lower than the average low tide.
Example: If your boat has a 3-foot draft and the chart shows 2 feet of water at MLLW, you must wait for a tide height of at least +2 feet to pass safely.
Remember, tides don’t rise at a constant speed. They start slowly, pick up speed in the middle, and slow down again as they reach high or low water. Boaters use the Rule of Twelfths to estimate how much the water level changes each hour, based on the high and low tide information included in a Tide Table:
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Tide tables are astronomical predictions—they calculate the effects of the moon and sun, but they cannot account for the weather. Wind and barometric pressure (especially low-pressure systems, which can lead to storm surges) impact the ocean surface.
Tide times shift because they follow a Lunar Day, not a 24-hour Solar Day. It takes the Earth 24 hours to rotate once, but because the moon is also moving in its orbit, it takes an extra 50 minutes for the same spot on Earth to “catch up” and align with the moon again. This is why high tide is roughly 50 minutes later each day.
Scientists use Harmonic Analysis to predict the tides. By studying years of water-level data at a specific station, they identify “harmonic constituents”—mathematical patterns caused by the rotation of the Earth and the varying positions of the moon and sun. Computers combine these overlapping patterns into a single formula to predict future water levels.
Yes. While many boaters use digital apps, printing a hard copy from the NOAA is a smart safety backup. Many local bait shops and marinas still provide or sell printed annual tide booklets for their specific local waters.
The Great Lakes (and other large lakes in the U.S.) do experience true astronomical tides caused by the moon and sun, but they are so small that they are almost impossible to detect without scientific instruments.