Orbital Velocity Calculator

Calculate the orbital speed for a circular orbit using v_orb = √(GM/r).

🛸 Orbit 📐 v=√(GM/r) 🌍 Circular Orbit
Central body mass (M) kg
Orbital radius (r) m

Presets:

⚠️ Enter valid positive numbers.

Understanding Orbital Velocity

Orbital velocity is the speed required for a satellite to maintain a circular orbit at a given altitude. The formula v_orb = √(GM/r) comes from setting centripetal force equal to gravitational force: mv²/r = GMm/r² → v = √(GM/r). Like escape velocity, it is independent of the satellite's mass.

At lower orbits (smaller r), orbital velocity is higher — satellites must move faster to 'fall around' a tighter curve. The ISS orbits at 400 km altitude (r ≈ 6,771 km) at about 7.66 km/s. At geostationary orbit (35,786 km), the orbital velocity drops to 3.07 km/s — exactly matching Earth's rotation, so the satellite appears stationary.

Orbital period follows from v_orb: T = 2πr/v = 2π√(r³/GM). This is Kepler's Third Law — period squared is proportional to orbit radius cubed. From LEO (T ≈ 90 min) to GEO (T = 24 hours) to Moon (T = 27.3 days), the relationship holds precisely.

Orbital velocity relates to escape velocity by v_esc = √2 × v_orb. To leave orbit and escape Earth's gravity, a spacecraft must increase its velocity by a factor of √2 ≈ 1.414. This is the 'Δv budget' for trans-lunar injection and interplanetary missions.

Formula Reference Table

Solve ForFormulaNotes
Orbital velocityv = √(GM/r)G = 6.674×10⁻¹¹ N·m²/kg²
Orbital periodT = 2πr/v = 2π√(r³/GM)Kepler's Third Law
GEO altituder_GEO = (GM·T²/4π²)^(1/3)T = 86,400 s
ISS (LEO)v ≈ 7.66 km/sT ≈ 92 min
Moon orbitv ≈ 1.02 km/sT = 27.3 days
vs escapev_esc = √2 × v_orb1.414× orbital speed

3 Worked Examples

Example 1
ISS Low Earth Orbit

Find ISS orbital velocity. r = R_Earth + 400 km = 6.371×10⁶ + 4×10⁵ = 6.771×10⁶ m.

  • v = √(6.674×10⁻¹¹ × 5.972×10²⁴ / 6.771×10⁶)
  • v = √(5.887×10⁷) = 7,673 m/s = 7.67 km/s
  • Period T = 2π × 6.771×10⁶ / 7,673 = 5,541 s = 92.4 min
✓ v = 7.67 km/s; T = 92.4 minutes
Example 2
Geostationary Orbit Altitude

Find radius of GEO orbit (T = 24 hours).

  • r = (GM × T²/(4π²))^(1/3) = (3.986×10¹⁴ × (86400)² / 39.48)^(1/3)
  • r = (7.532×10²²)^(1/3) = 4.216×10⁷ m = 42,160 km
  • Altitude = 42,160 − 6,371 = 35,789 km
✓ GEO altitude = 35,786 km
Example 3
Moon's Orbital Speed

Moon orbit: r = 3.844×10⁸ m, M_Earth = 5.972×10²⁴ kg.

  • v = √(6.674×10⁻¹¹ × 5.972×10²⁴ / 3.844×10⁸)
  • v = √(1.036×10⁶) = 1,018 m/s = 1.02 km/s
  • Period = 2π × 3.844×10⁸ / 1,018 = 2.372×10⁶ s = 27.5 days
✓ v = 1.02 km/s; T = 27.5 days

Real-World Applications

🛰️
Satellite Design
Communication satellites must hit precise orbital velocities. Too slow → fall to lower orbit; too fast → climb higher. Station-keeping thrusters correct for atmospheric drag in LEO.
🌍
GPS Satellites
GPS satellites orbit at 20,200 km altitude (MEO). v_orb ≈ 3.87 km/s, T = 11 hours 58 min. Engineers calculate orbital velocities precisely for timing synchronization required for centimeter-accuracy GPS.
🚀
Mission Planning
Δv (velocity change) budget for missions is calculated from orbital velocity differences. Going from LEO to GEO requires Δv ≈ 3.9 km/s via Hohmann transfer — a key cost driver in satellite propellant mass.
📡
Geostationary Comms
GEO satellites at 35,786 km appear stationary because their orbital period exactly matches Earth's rotation. This requires v_orb = 3.07 km/s — directly calculable from v = √(GM/r).
🌙
Lunar Missions
To enter lunar orbit, Apollo spacecraft decelerated to v_orb ≈ 1.5–1.7 km/s at their chosen lunar orbit altitude. Too fast → flyby; too slow → crash. The rocket equation determined how much fuel was needed for orbital insertion.

Common Mistakes to Avoid

⚠️
Confusing orbital and escape velocity

v_esc = √2 × v_orb. Orbital velocity keeps you in orbit; escape velocity breaks free of gravity. They differ by a factor of 1.414.

⚠️
Using altitude instead of orbital radius

r in the formula is distance from the planet's CENTER, not altitude. Always add planet radius: r = R_planet + altitude.

⚠️
Wrong G constant units

G = 6.674×10⁻¹¹ N·m²/kg². Using G = 6.674×10⁻¹¹ with M in solar masses or r in AU gives wrong answers — must use consistent SI units.

⚠️
Assuming all orbits are circular

v = √(GM/r) gives circular orbit velocity. Elliptical orbits have varying speed (faster at perigee, slower at apogee) — v = √(GM(2/r − 1/a)) where a = semi-major axis.

⚠️
Forgetting that orbital velocity decreases with altitude

Counter-intuitively, higher orbit = slower speed. This is because at higher altitude, less centripetal acceleration is needed (weaker gravity), so lower orbital speed is required.

Frequently Asked Questions

How is orbital velocity derived?
For circular orbit: gravitational force = centripetal force → GMm/r² = mv²/r → v = √(GM/r). The satellite's mass cancels, so orbital velocity is independent of satellite mass — a 1 kg cubesat and the ISS orbit at the same speed at the same altitude.
What is Kepler's Third Law?
T² ∝ r³: orbital period squared is proportional to semi-major axis cubed. Precisely: T² = 4π²r³/(GM). For solar system planets orbiting the Sun: T²/a³ = 4π²/(GM_sun) is constant. This allowed Newton to verify his inverse-square gravity law against Kepler's observations.
What is geostationary orbit?
GEO is the altitude where orbital period = Earth's rotational period (24 hours = 86,400 s). Solving T = 2π√(r³/GM): r_GEO = 42,164 km from Earth's center = 35,786 km altitude. At this altitude and 0° inclination, the satellite appears fixed in the sky — ideal for TV, weather, and communications satellites.
Why do satellites decay from orbit?
Even at LEO altitudes, trace atmosphere exerts tiny drag, slowly removing kinetic energy. The satellite spirals inward, paradoxically speeding up as it descends (lower orbit = higher speed). Eventually atmospheric heating destroys it. The ISS loses ~2 km of altitude per month and requires regular reboosts.
What is delta-v (Δv)?
Δv is the change in velocity a spacecraft must execute to change orbits. It determines propellant needed via the rocket equation: Δm/m₀ = 1 − e^(−Δv/Isp·g). LEO→GEO requires Δv ≈ 3.9 km/s; Earth escape from LEO ≈ 3.2 km/s; Mars surface launch ≈ 3.6 km/s.
What is the Lagrange point?
Lagrange points are positions in a two-body orbital system where a small object maintains a stable position relative to both large bodies, combining the gravity and orbital motion of both. There are 5 Lagrange points (L1–L5) for each two-body system. The James Webb Space Telescope orbits Earth-Sun L2 at 1.5 million km from Earth.
Can a satellite orbit at any altitude?
Practically speaking, below ~160 km atmospheric drag rapidly decays any orbit. Above this, theoretically any altitude works, but GEO is special for communications. Some satellites use sun-synchronous orbits (polar, ~600 km) to always pass over the same location at the same local time, useful for Earth observation.
What determines how long a satellite lasts in orbit?
Drag is the main decay mechanism at LEO. Drag depends on atmospheric density (varies with solar activity), satellite area-to-mass ratio, and Cd. Satellites at 800 km altitude can last decades; at 400 km (ISS altitude) only 1–2 years without reboost. GEO satellites last 15+ years with station-keeping propellant.

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