Escape Velocity Calculator

Compute the classical escape velocity using v = √(2 G M / r). Use presets for common bodies (Earth, Moon, Sun), enter a custom mass and radius, or provide altitude above a body's surface. Outputs are shown in m/s and km/s with optional step-by-step derivation.

If altitude is provided, r used = body radius + altitude (units converted).

Escape Velocity — meaning, formula and practical implications

Escape velocity is the minimum initial speed required for an object to leave the gravitational influence of a massive body without further propulsion, neglecting atmospheric drag and assuming energy-conserving motion. For a spherically symmetric mass distribution, the classical escape velocity from distance r from the center is

v = √(2 G M / r)

Where the formula comes from

The expression follows from conserving mechanical energy. The object needs initial kinetic energy equal to the change in gravitational potential energy required to move from r to infinity: (1/2) m v² = G M m / r. Cancel m and rearrange to get v = √(2GM/r). This derivation assumes Newtonian gravity and neglects other forces.

Typical values and presets

Common surface escape speeds: Earth ≈ 11.186 km/s, Moon ≈ 2.38 km/s, Sun (photosphere) ≈ 617.5 km/s. These are computed using accepted mass and radius values for the bodies. The calculator includes presets for convenience but allows custom M and r for satellites, exoplanets or hypothetical bodies.

Using altitude and surface vs center

Escape speed decreases with altitude because r increases. To compute escape speed from altitude h above the surface: use r = R_body + h. For spacecraft launches the required delta-v is higher than the surface escape speed due to atmospheric drag, gravity losses during ascent, and the need to achieve certain trajectories, so escape velocity is a theoretical baseline rather than a direct launch target.

Limits and assumptions

The formula assumes a point mass or spherically symmetric mass distribution and classical mechanics. It ignores atmospheric drag, rotational energy of the body (which can assist or hinder escape depending on launch azimuth and latitude), and relativistic effects. For relativistic or high-precision astronomical work, general relativity and detailed mass distribution models must be used.

Worked examples

Example 1 — Earth surface: Using M_earth = 5.972e24 kg and R_earth = 6.371e6 m, v = √(2 × 6.67430e-11 × 5.972e24 / 6.371e6) ≈ 11,186 m/s ≈ 11.186 km/s.

Example 2 — From altitude: At 400 km altitude (ISS orbit approximate), r ≈ 6.371e6 + 4e5 = 6.771e6 m. Escape speed ≈ √(2GM / r) ≈ 10.97 km/s (slightly lower than from surface).

Practical implications for missions

Real launch vehicles do not simply accelerate to escape speed; they follow powered trajectories that trade gravity losses and atmospheric drag. For interplanetary missions the spacecraft often first reach orbit and then apply burns (Oberth effect) to raise energy. Additionally, missions use gravity assists, which rely on relative motion rather than pure escape speed calculations.

Units and precision

Use SI for internal calculations. This tool converts common units (km, km for radius, Earth-mass, Solar-mass) into SI and provides outputs in m/s and km/s. For high-precision research, use the latest measured planetary parameters from authoritative sources.

Using this calculator

Select a preset or enter custom mass (M) and radius (r). Optionally enter an altitude to compute from above the surface. Choose precision and enable steps to show the algebraic derivation and intermediate conversions. Export results to CSV or copy them to the clipboard for reports.

Frequently Asked Questions

1. What is escape velocity?
Escape velocity is the minimum speed required to escape a body's gravity without further propulsion, ignoring drag.
2. Does rotation of a planet change escape velocity?
Rotation doesn't change the classical formula significantly, but launching eastward from a rotating planet gives an initial tangential velocity which reduces the required additional speed to reach escape from surface.
3. Why is atmosphere ignored?
Atmospheric drag converts kinetic energy into heat; incorporating it requires detailed aerodynamics and trajectory modeling beyond the simple formula.
4. Can I use Earth-masses or Solar-masses?
Yes — the calculator accepts Earth-mass and Solar-mass input units for convenience and converts them to kg internally.
5. How do I compute escape from altitude?
Provide altitude; r used in v = √(2GM/r) is radius + altitude (both in metres after conversion).
6. Is this the same as orbital velocity?
No — circular orbital velocity at radius r is v_orbit = √(GM/r), which is 1/√2 (~0.707) times the escape speed for the same r.
7. Are tidal or multi-body effects included?
No — the simple formula assumes a single central mass. Multi-body dynamics (e.g., Lagrange points) require more complex modeling.
8. Can I use this for black holes?
Not reliably — near a black hole relativistic effects dominate and the Newtonian formula is invalid.
9. Does the calculator show both m/s and km/s?
Yes — results are shown in m/s and km/s for convenience.
10. Is the tool free?
Yes — AkCalculators provides this educational tool free for students and engineers.