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Orbital Period

Quick answer

Orbital period is the time a satellite takes to complete one revolution — about 90 minutes in low Earth orbit, 12 hours for navigation constellations, and 23 h 56 m at geostationary altitude. Period depends only on the orbit's size, not the satellite's mass.

📘 Full definition✓ Reviewed 2026-09-07
The orbital period is the duration of one full revolution around a body. Kepler's third law fixes it by orbit size alone: period squared is proportional to the semi-major axis cubed, so every orbit of a given size has the same period whether it carries a CubeSat or a space station, and regardless of eccentricity. The practical ladder runs from about 88 minutes at the lowest sustainable altitudes, through ~92–95 minutes for the busy 400–600 km band, two hours near 1,700 km, 12 hours (sidereal) for GNSS constellations near 20,000 km, to 23 hours 56 minutes — one sidereal day — at the 35,786 km geostationary altitude, where the period matches Earth's rotation and the satellite hangs stationary in the sky. Period drives everything an observer experiences: how many passes a day a satellite makes, how long each lasts, and how quickly a constellation's coverage pattern repeats.
LEO (400 km)
92 min
GPS (20,200 km)
12 hours
GEO (35,786 km)
24 hours
Moon
27.3 days

Understanding Orbital Period

The period ladder

Reading altitude from period becomes second nature: ISS-class orbits tick just over 90 minutes and deliver ~15.5 orbits a day; Sun-synchronous imagers near 700 km run ~99 minutes; GPS-class semi-synchronous orbits complete two revolutions per sidereal day; and the one-sidereal-day geostationary period closes the ladder. Special rungs exist — the 12-hour Molniya orbit shares GNSS's period but spends it utterly differently, dwelling over one hemisphere.

Resonance and repeat cycles

When a period divides evenly into Earth's rotation, the ground track repeats: a satellite at exactly 15 orbits per day retraces its path daily. Designers tune periods a shade off resonance to make tracks march steadily in longitude, building repeat cycles of N days that guarantee a sensor revisits every point on a fixed schedule — the backbone of systematic Earth observation.

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Frequently Asked Questions

Both gravitational pull and the inertia to be moved scale identically with the satellite's mass, so it cancels: a bolt and a 400-tonne station in the same orbit circle Earth in exactly the same time. Only the central body's mass and the orbit's size matter.
A satellite must match Earth's rotation relative to the stars — the sidereal day of 23 h 56 m 4 s. The familiar 24-hour solar day is slightly longer because Earth must turn a little extra each day to face the Sun again as it moves along its orbit.
It doesn't change it — a stretched orbit and a circle with the same semi-major axis share one period. Eccentricity redistributes the time: the satellite lingers near apogee and sprints through perigee, but the lap time stays fixed.

Sources & References

Definitions are reviewed against primary sources. Last reviewed: 2026-09-07.