Tidal Acceleration from a Distant Body

Also known as tidal acceleration · tidal force per unit mass · 2GMR/d^3 · Moon tidal pull · Sun tidal pull · tide-raising acceleration · tidal force formula · differential gravity across the Earth · why the Moon lifts the sea · tidal field of the Moon · tide generating acceleration

a=2 G M Rd3a = \frac{2\,G\,M\,R}{d^{3}}
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Worked example: Wikipedia 'Tidal force' table, the Moon: 7.34e22 kg, 6.37e6 m, 3.84e8 m → 1.1e-6 m/s2 (2 s.f.). Press Try an example to run it live, then adjust anything.

Enter your known values, leave one input blank, and solves for the missing one. Tap a variable’s symbol to see what it means, with a typical value. Change any unit and the answer follows.

See also

Gravitational Field Strength: The gravity of the same body at one distance: the tidal acceleration is its difference between the near side and the centre.Newton's Law of Universal Gravitation: The force between the two bodies that the tidal field is the small unevenness of.Tide Height Between High and Low Water (Cosine Curve): What the sea does with the pull: the height of the tide between a high water and a low water.
Learning zone

Tidal Acceleration from a Distant Body explained

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A distant body does not pull evenly on a large ball: the near side feels slightly more of its gravity than the centre does. That unevenness is the tidal acceleration, and it is what lifts the oceans on the near and far sides of the Earth at once. The formula a=2GMR/d3a = 2GMR/d^{3} is the difference between the body's gravity at the near side and at the centre, kept to first order in R/dR/d. Here MM is the mass of the body that pulls, dd its distance from the centre of the ball, RR the radius of the ball and GG the gravitational constant.

The cube of the distance is what matters. Take the Moon's mass of 7.34×10227.34\times10^{22} kg at a distance of 3.84×1083.84\times10^{8} m and the Earth's radius of 6.37×1066.37\times10^{6} m: the formula gives 1.1022×10−61.1022\times10^{-6} m/s². For the Sun, 1.99×10301.99\times10^{30} kg at 1.50×10111.50\times10^{11} m, it gives 5.014×10−75.014\times10^{-7} m/s². The Sun's tidal pull is therefore a little under half the Moon's, though it pulls far harder, because the cube of the distance shrinks it.

The page is checked against a published table of tidal accelerations for the Earth, which prints 1.1×10−61.1\times10^{-6} m/s² for the Moon and 0.5×10−60.5\times10^{-6} m/s² for the Sun. Those printed values have two significant figures for the Moon and one for the Sun, so they check the page only that closely: within 4.5 percent for the Moon and 10 percent for the Sun. That is enough to catch a missing 2 or a wrong power of the distance, but not a small error. Treat it as a first-order approximation to a difference in gravity, not a precision tool.

The formula keeps only the first term. The exact difference, GM/(d−R)2−GM/d2GM/(d-R)^{2} - GM/d^{2}, is larger by about 1.5 R/d1.5\,R/d, which is 2.4 percent for the Moon and nothing noticeable for the Sun. It gives the pull along the line to the body; across that line the tide squeezes, with half the size. The sea's real tide follows the shape of the basins and the water's own response, so this is the sky's share of it, not a tide height. As a round-number check, M=1022M = 10^{22} kg, R=106R = 10^{6} m and d=108d = 10^{8} m give 1.33486×10−61.33486\times10^{-6} m/s², and read backwards give d=108d = 10^{8} m again.

Tidal Acceleration from a Distant Body formula

a=2 G M Rd3a = \frac{2\,G\,M\,R}{d^{3}}
Where
  • aa= Tidal acceleration (m/s²)
  • MM= Mass of the body that pulls (kg)
  • RR= Radius of the body being stretched (km)
  • dd= Distance between the centres (km)
Revised 31 October 2026
Cite this page

formula.expert. (2026, October 31). Tidal Acceleration from a Distant Body Formula & Calculator. https://formula.expert/solvers/tidal-acceleration-distant-body