Planet Gravity Calculator
Embed This Widget
Add the script tag and a data attribute to embed this widget.
Embed via iframe for maximum compatibility.
<iframe src="https://starfyi.com/iframe/entity//" width="420" height="400" frameborder="0" style="border:0;border-radius:10px;max-width:100%" loading="lazy"></iframe>
Paste this URL in WordPress, Medium, or any oEmbed-compatible platform.
https://starfyi.com/entity//
Add a dynamic SVG badge to your README or docs.
[](https://starfyi.com/entity//)
Use the native HTML custom element.
Calculate your weight on other worlds
How to Use
-
1
Enter your weight on Earth
Input your body weight in kilograms or pounds. The calculator uses this value as a reference, dividing it by Earth's standard surface gravitational acceleration (9.807 m/s²) to derive your mass, which remains constant regardless of location.
-
2
Select the bodies to compare
Choose from the eight solar system planets, major moons including the Moon, Titan, Ganymede, Europa, and Io, dwarf planets like Pluto and Eris, and notable confirmed exoplanets with published radius and mass data. Multiple selections display in a ranked comparison table.
-
3
Interpret the weight and gravity values
The table shows your equivalent weight on each body alongside the surface gravitational acceleration in m/s² and as a fraction of Earth's g. Additional context explains how lower gravity affects physical activities, bone density loss rates, and atmospheric escape velocity for each world.
About
Surface gravity is a fundamental planetary characteristic that shapes atmospheric retention, geological activity, tidal forces, and the biological requirements for any life that might inhabit a world. Newton's law of universal gravitation, combined with precise measurements of planetary masses and radii, allows calculation of surface gravity for every solid body and defined pressure level in the solar system. The formula g = GM/r² distills these properties to a single comparative number.
The diversity of surface gravities across solar system bodies spans more than five orders of magnitude, from the Moon at 1.62 m/s² to Jupiter at 24.79 m/s², with tiny asteroids measuring millimeters per second squared or less. This variation profoundly affects planetary atmospheres: a body must have surface gravity sufficient to prevent light atoms like hydrogen and helium from escaping at thermal velocities over geological time. Mars lost much of its early atmosphere partly because its lower gravity allowed atmospheric escape, a process also influenced by the loss of its global magnetic field.
For human space exploration, understanding the gravitational environment of destination worlds is critical to mission design and crew health planning. The Moon's one-sixth gravity enabled Apollo astronauts to carry heavy spacesuits and samples without exhaustion, but prolonged exposure to any sub-g environment causes physiological deconditioning. Research on the ISS at near-zero gravity provides data for modeling the intermediate Martian case, guiding habitat design, exercise countermeasures, and medical protocols for long-duration surface missions.