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Standard gravity, g₀

A fixed, conventional value for the acceleration due to gravity, used for the kilogram-force, g-force ratings and standard weights. It is a convention rather than a measurement, and not the value anywhere in particular.

g₀ = 9.80665 m/s²

Exact by definition, so it has no uncertainty at all.

In other units

Values marked … are exact, but their decimals run on, so they stop at ten significant figures instead of being rounded.

Measured values are in CODATA’s concise form: the digits in brackets are the standard uncertainty in the last two places, so 6.67430(15) means 6.67430 ± 0.00015.

Standard gravity in SI units and in other units
Quantity Value
g₀ 9.80665 m/s²
g₀ 32.17404855… ft/s²
g₀ 980.665 cm/s²
1 kgf 9.80665 N

g₀ in ft/s²

  1. 9.80665 m/s² ÷ 0.3048 m/ft
  2. = 32.17404855… ft/s²

g₀ in cm/s²

  1. 9.80665 m/s² × 100 cm/m
  2. = 980.665 cm/s²

A centimetre per second squared is also called a gal, the unit geophysicists measure gravity in.

1 kgf in N

  1. 1 kg × 9.80665 m/s²
  2. = 9.80665 N

The kilogram-force is the weight of one kilogram under standard gravity.

Where the value comes from

The 3rd General Conference on Weights and Measures adopted it in 1901, declaring 980.665 cm/s² the standard acceleration due to gravity, a figure already written into the laws of some countries. The same declaration settled the difference between mass and weight: a body’s standard weight is its mass times this acceleration.

The number came from a measurement made at the International Bureau of Weights and Measures, near Paris, in 1888, divided by a theoretical factor meant to convert it to sea level at a latitude of 45°. Nothing has redefined it since, so it is a fixed convention rather than the gravity at any real place. CODATA lists it as exact, under the symbol gₙ.

Which form to use

Use 9.80665 m/s² wherever a standard or a unit calls for it: the kilogram-force, g-force ratings, standard weights. In a school problem 9.81 m/s² is the usual figure; it differs from g₀ by 0.034 percent, far less than real gravity varies over the Earth.

At sea level, gravity runs from about 9.78 m/s² at the equator to about 9.83 m/s² at the poles, roughly half a percent. Two effects add together: the Earth’s rotation throws the surface outward most strongly at the equator, and the equatorial bulge puts the surface there further from the centre.

Gravity also falls with height, by about 3 × 10⁻⁶ m/s² for every metre climbed, roughly 0.003 m/s² per kilometre. On a mountain that shows in the fourth significant figure; across the globe the change with latitude is larger.

Common mistakes

Tools that use it

Related constants

See also

Source: BIPM, 3rd General Conference on Weights and Measures (1901), Declaration 2. The same value in NIST’s CODATA listing.

The values are facts and free to use; this page’s selection and presentation are © 2026 ScienceQuest.