Acceleration Converter
Converters · Added 15 August 2026
Convert acceleration between metres per second squared, g-force, imperial units and the rate-of-speed-change forms used for vehicles. One g is standard gravity, exactly 9.80665 m/s², which is the yardstick most acceleration figures are quoted against.
Result
1 m/s² in standard gravity
0.101971621 g
1 m/s² = 0.101971621 g
The same value in every unit
- Metre per second squared (m/s²)
- 1
- Centimetre per second squared (gal) (cm/s²)
- 100
- Millimetre per second squared (mm/s²)
- 1,000
- Kilometre per second squared (km/s²)
- 0.001
- Kilometre per hour per second (km/h/s)
- 3.6
- Mile per hour per second (mph/s)
- 2.23693629
- Foot per second squared (ft/s²)
- 3.2808399
- Inch per second squared (in/s²)
- 39.3700787
- Standard gravity (g)
- 0.101971621
One g is standard gravity, defined as exactly 9.80665 m/s². It is an agreed yardstick rather than a measurement of the local gravitational field, which varies slightly with latitude and altitude.
How to use the acceleration converter
- 1Enter the acceleration value you have.
- 2Pick its unit and the one you want.
- 3The table shows the same acceleration in every unit at once.
- 4For vehicle figures, km/h per second and mph per second are usually the most intuitive.
- 5Swap the units to reverse the conversion.
Examples
Gravity
- Input
- 1 g
- Result
- 9.80665 m/s² · 32.174 ft/s²
Standard gravity is defined exactly rather than measured, so this conversion is exact.
A brisk car
- Input
- 26.82 km/h/s
- Result
- 7.45 m/s² · 0.76 g
This is 0–100 km/h in about 3.7 seconds, sustained.
Seismology
- Input
- 100 cm/s² (gal)
- Result
- 1 m/s² · 0.102 g
The gal, named after Galileo, is the standard unit for ground acceleration in earthquake measurement.
About the acceleration converter
Acceleration is a change in velocity, not a speed
Acceleration measures how quickly velocity changes, which is why its units carry a squared time: metres per second, per second. A car going from rest to 27 metres per second in ten seconds averaged 2.7 m/s². The unit looks strange until you read it aloud as a rate of a rate.
Because velocity is a vector, changing direction is acceleration even at constant speed. A car cornering at a steady 60 km/h is accelerating, which is exactly what the passengers feel pushing them sideways. This is also why an object in circular orbit is permanently accelerating despite never speeding up.
The rate-of-speed-change units in this converter — km/h per second, mph per second — are dimensionally the same thing expressed more legibly for vehicles. Saying a car gains 27 km/h every second is easier to picture than saying it accelerates at 7.5 m/s², even though they are identical.
Why standard gravity is a definition
Actual gravitational acceleration varies across the Earth's surface. It is weakest at the equator, where distance from the centre is greatest and centrifugal effect largest, and strongest near the poles — roughly 9.78 to 9.83 m/s². Altitude reduces it further, and dense rock beneath your feet increases it slightly.
That variation is a problem for any unit defined in terms of gravity, which includes kilogram-force and pound-force as well as the g used here. So standard gravity was fixed by agreement at exactly 9.80665 m/s², a value close to the average at mid-latitudes at sea level. It is a convention, not a measurement, which is why it never needs revising.
The variation is small but genuinely measurable, and gravity surveying makes a science of it. Mapping tiny local differences in gravitational acceleration — measured in milligals — reveals density variations underground, which is how oil, mineral and groundwater deposits are located from the surface without drilling.