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Tidal acceleration calculator

Compute the tidal acceleration a body exerts across a planet, compare it with the Moon's effect on Earth, and see why spring and neap tides happen.

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Results

Tidal acceleration at the surface

0.0000011 m/s²

Compared with the Moon's tide on Earth

1 ×

As a fraction of Earth's gravity
1.122 × 10⁻⁷
Compared with the Sun's tide on Earth
2.177 ×

What tides are

Gravity weakens with distance. A moon pulls the near side of a planet more strongly than its center, and the center more strongly than the far side. That difference stretches the planet along the line to the moon, raising two bulges: one facing the moon and one opposite. That is why most coasts see two high tides a day.

The formula

For a body of mass M at distance d, the tidal acceleration across a planet of radius r is approximately:

a_tidal ≈ 2 × G × M × r ÷ d³

Tidal effects fall with the cube of distance, much faster than gravity itself, which falls with the square.

Moon versus Sun

  • Moon: about 1.1 × 10⁻⁶ m/s² at Earth’s surface.
  • Sun: about 0.5 × 10⁻⁶ m/s², roughly 46% of the Moon’s effect.

The Sun’s gravity on Earth is about 180 times stronger than the Moon’s, yet its tidal effect is weaker because it is about 390 times farther away and the cube of distance wins.

Spring and neap tides

  • Spring tides: at new and full moon, the Sun and Moon line up and their effects add, about 1.46 times the lunar tide alone.
  • Neap tides: at first and last quarter, they act at right angles and partly cancel, about 0.54 times the lunar tide.

Local geography amplifies these forces enormously: tides range from a few inches in the Mediterranean to over 50 ft (16 m) in Canada’s Bay of Fundy.

Example

With the Moon’s mass (0.0123 Earth masses) at 384,400 km and Earth’s radius (6,371 km), the calculator gives about 1.10 × 10⁻⁶ m/s², about one ten-millionth of Earth’s gravity. Small as it is, acting on whole oceans it moves enormous volumes of water.

Other tidal effects

  • Tidal locking: the Moon always shows the same face because Earth’s tides on it slowed its rotation.
  • Tidal heating: Jupiter’s moon Io is the most volcanic body in the solar system because Jupiter’s tides flex it constantly.
  • Roche limit: close enough to a planet, tides can tear a moon apart, one origin proposed for planetary rings.
  • Earth’s day is lengthening: tidal friction slows Earth’s rotation by about 2 milliseconds per century and pushes the Moon about 3.8 cm (1.5 in) farther away each year.

Frequently asked questions

What is a tidal acceleration?

It is the difference in a body's pull between the near and far sides of another body. It falls with the cube of distance, approximately 2GMr/d³.

Why does the Moon cause bigger tides than the Sun?

The Sun pulls harder overall, but it is so far away that the difference across Earth is smaller. The Moon's tidal effect is about 2.2 times the Sun's.

What are spring and neap tides?

When the Sun and Moon line up, their tidal effects add and tides are large (spring tides). At quarter moons they partly cancel and tides are small (neap tides).

Can tides tear objects apart?

Yes, inside the Roche limit tidal stretching exceeds self-gravity. That is how comets such as Shoemaker-Levy 9 broke up near Jupiter.

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Results are estimates provided for information purposes. They do not replace professional advice.