Philippines · Science & Engineering
Potential Energy Calculator
Choose which quantity to solve for and enter the other three. The calculator rearranges U = mgh and shows the substitution, with units stated on every input.
How do you calculate gravitational potential energy?
Gravitational potential energy is U = mgh — mass in kilograms, times gravitational field strength in metres per second squared, times height in metres, giving joules. A 2 kg object raised 5 metres on Earth has 2 × 9.81 × 5 = 98.1 joules of potential energy relative to its starting point.
How to use this calculator
- Choose the unknownThe calculator rearranges the formula for you. Solving for height or mass is just as common in problem sets as solving for energy, and the rearrangement is where marks are lost.
- Use SI units throughoutKilograms, metres and metres per second squared. Grams and centimetres are the most common source of a wrong answer, and the working shows the units so a mistake is visible.
- Set g for the body you are on9.81 on Earth. The Moon is 1.62 and Mars 3.72, and problem sets use them precisely to check whether you understood that g is not a universal constant.
- Decide your reference levelHeight is measured from a zero point you choose. Only changes in height are physically meaningful, so pick a convenient reference and stay consistent.
How the calculation works
Gravitational potential energy is the work done against gravity to lift an object. Work is force times distance; the force needed is the object's weight, mg; the distance is the height h. Multiply them and you have mgh.
That derivation matters because it shows what the formula assumes. It treats g as constant over the height involved, which is an excellent approximation near a planetary surface and a poor one over orbital distances. For a satellite you need the full inverse-square expression, U = −GMm/r, and the two only agree for small height changes.
The reference level is arbitrary, and this is the conceptual point students most often miss. There is no absolute potential energy — only differences. Putting the zero at the floor, at the bench, or at sea level changes every value you compute and changes none of the physics, because every problem depends on ΔU rather than U.
Rearranging is straightforward algebra, but it is worth noting that solving for height is the same operation as asking how far something falls to release a given energy, which is why the calculator also shows the free-fall speed and time.
U = mgh · m = U ÷ gh · h = U ÷ mg · g = U ÷ mhWorked example: a book on a shelf
A 2 kg book is lifted onto a shelf 5 metres above the floor, on Earth.
U = mgh = 2 × 9.81 × 5 = 98.1 joules. That is the work done against gravity in lifting it, and the energy that would be released if it fell back.
If it does fall, all of that converts to kinetic energy at the moment before impact. Setting ½mv² equal to 98.1 and solving gives v = √(2gh) = √(2 × 9.81 × 5) = 9.9 m/s. The mass cancels entirely — which is why a 2 kg book and a 20 kg one hit the ground at the same speed from the same height, ignoring air resistance.
The fall takes √(2h/g) = √(10/9.81) = 1.01 seconds. Both figures appear in the breakdown, because energy questions and kinematics questions are usually two halves of the same problem.
Gravitational field strength elsewhere
| Body | g (m/s²) | Energy to lift 1 kg by 1 m |
|---|---|---|
| Earth | 9.81 | 9.81 J |
| Moon | 1.62 | 1.62 J |
| Mars | 3.72 | 3.72 J |
| Jupiter (cloud tops) | 24.79 | 24.79 J |
| Venus | 8.87 | 8.87 J |
| Mercury | 3.70 | 3.70 J |
Earth's own value varies slightly with latitude and altitude — roughly 9.78 at the equator and 9.83 at the poles. Problem sets almost always use 9.81, and some textbooks use 9.8 or even 10 for mental arithmetic. Use whichever your course specifies, because the difference will show in a marked answer.
Where the simple formula stops working
U = mgh holds where g can be treated as constant. Near Earth's surface that is true to well within measurement error for any height you are likely to encounter in a problem set — even a kilometre changes g by about 0.03%.
Over larger distances it fails. Gravitational field strength falls with the square of the distance from the centre of mass, so lifting something to orbital altitude requires the full expression U = −GMm/r. The negative sign there is not an error: potential energy is conventionally defined as zero at infinite separation, which makes every bound state negative.
The formula also covers only gravitational potential energy. Elastic potential energy in a spring is ½kx², and chemical, electrical and nuclear potential energy are governed by entirely different relationships. A question asking for potential energy without qualification almost always means the gravitational kind, but it is worth checking.
One final subtlety: mgh gives the work done against gravity, which equals the energy stored only if the object is raised without gaining speed. Lift it and let it arrive moving and some of the work went into kinetic energy instead.
Air resistance is ignored throughout. For a dense compact object over a few metres that is a good approximation. For anything light or with a large surface area — a sheet of paper, a parachute — the energy released on falling is dissipated rather than converted to speed, and the free-fall figures here do not apply.
Assumptions and limitations
- Assumes g is constant over the height involved — valid near a planetary surface, not over orbital distances
- Covers gravitational potential energy only, not elastic, chemical or electrical
- Height is measured from a reference level you choose; only differences are physically meaningful
- Free-fall speed and time assume no air resistance
- Requires SI units throughout — kilograms, metres and metres per second squared
- The formula gives work done against gravity, which equals stored energy only if the object arrives at rest
Questions people ask about this in Philippines
How do you calculate gravitational potential energy?
Multiply mass by gravitational field strength by height: U = mgh. With mass in kilograms, g in metres per second squared and height in metres, the answer is in joules.
A 2 kg object raised 5 metres on Earth has 2 × 9.81 × 5 = 98.1 joules relative to its starting point.
What is g and does it change?
Gravitational field strength, about 9.81 m/s² on Earth. It differs on other bodies — 1.62 on the Moon, 3.72 on Mars — and varies slightly across Earth's surface, from roughly 9.78 at the equator to 9.83 at the poles.
Where do I measure height from?
Anywhere convenient, as long as you are consistent. Potential energy has no absolute value — only differences matter — so the zero point is a choice. The floor, the bench or sea level are all valid references and will give different numbers for the same physical situation.
Does mass affect how fast something falls?
No, ignoring air resistance. Setting mgh equal to ½mv² cancels the mass entirely, giving v = √(2gh). A heavy object and a light one released from the same height hit the ground at the same speed, which is exactly the point of the classic demonstration.
Why is potential energy sometimes negative?
In the full gravitational expression U = −GMm/r, potential energy is defined as zero at infinite separation, which makes every bound state negative. The simple mgh version measures from a local reference instead, so it can be positive or negative depending on where you put the zero.
Can I use mgh for satellites?
No. mgh assumes g is constant, and gravitational field strength falls with the square of distance. Over orbital altitudes that assumption breaks down badly and you need U = −GMm/r. The two only agree for height changes small compared with the planet's radius.
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Method, source and review date
- How it is worked out
- Gravitational potential energy near a planetary surface, rearranged for any variable
- Formula used
U = mgh, where m is mass in kg, g is field strength in m/s², h is height in m- Basis
- Standard mechanics, E = mgh
- Last reviewed
- Confidence
- High
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Disclaimer
Grade and score calculations follow the published rules as we understand them, but institutions apply their own variations and change them between intakes. Confirm anything that affects an application with the school, university or examination body itself.