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Science Astronomy Atmosphere

Vol. Science · Astronomy · The orbit

Satellites
around Earth

Pick an altitude. A circular orbit around Earth then has one period, one speed, and one ground track. The period is P = 2π √(a³ / μ). The speed is v = √(μ / r). μ is the Earth Fact Sheet GM, 0.39860 × 106 km3/s2. The altitude is height above that sheet’s equatorial radius, 6,378.137 km. Geostationary is the circle whose period equals the same sheet’s sidereal rotation, 23.9345 hours, not the 24.0000-hour mean solar day. That circle sits at 35,786.05 km. The slider runs from 160 km to 410,000 km, far enough to reach the Moon Fact Sheet distances. An ellipse is optional: perigee and apogee, and vis-viva speeds at each end. The year of a solar circle is the Kepler desk. Leaving the circle is the escape desk. The half-ellipse up to the geosynchronous radius is the Hohmann desk. The sidereal day itself is the sidereal desk.

Educational calculator. Simplified two-body model. Circular unless an ellipse is set. No drag, no oblateness, and no third body in the arithmetic. Not for mission planning. The drawing is top-down from the north, in the equatorial plane. Cited inclinations are not drawn. The horizon ignores refraction. A radio horizon sits farther out than this geometric one. The 160 km end of the slider is a classroom floor, not a cited boundary.

Interactive · One altitude

True scale · Earth and the orbit in one ruler · north up

  • Earth
  • Orbit
  • Geostationary
  • Satellite

True scale. The frame fits the current orbit, so a low orbit is a thin ring on a large Earth.

Altitude above the equatorial radius. The slider is logarithmic.

km

What this means

A lower orbit is faster, and it finishes sooner. Gravity is stronger closer in, so the sideways speed that keeps missing the Earth is higher: v = √(μ / r). The path is also shorter. The period grows as a to the power 3/2, so the time drops faster than the radius. At the cited ISS altitude of about 420 km the circle takes 92.97 minutes and moves at 7.657 km/s. At geostationary altitude the same formulas give 23 h 56.07 min and 3.075 km/s. Nothing in the arithmetic pushes the low satellite. It is falling the whole way, and the ground curves away as fast as it falls.

Geostationary sits where one orbit lasts one sidereal day. The ground’s turn against the stars is the fact sheet’s 23.9345 hours, not the 24.0000-hour mean solar day. Set P equal to that sidereal period and solve r³ = μ P² / (4π²). Subtract the equatorial radius and the altitude is 35,786.05 km. A circle timed to 24.0000 hours would sit 76.89 km higher, and it would drift. Geostationary also means a circle in the equatorial plane. This page matches the period. It does not draw the inclination. The Hohmann desk uses this same GM and the same 23.9345 hours, then subtracts the volumetric mean radius, 6,371.000 km. The circle in space is the same. The printed altitude differs by those two radii, 7.137 km.

Low orbits decay. This page does not time the decay. NASA’s Earth-observing notes say the station’s altitude drops from atmospheric drag, and that reboosts raise it. The same notes say each orbit takes 90–93 minutes depending on the exact altitude, and that the ground track steps west by about 22.9°. Hubble’s public pages say the telescope still meets enough air to descend, which is why shuttle crews boosted it. Those are qualitative facts. A lifetime in days is not printed here, because it depends on solar activity and on the satellite, and this model has no atmosphere in the formula.

Literacy · one radius, several readings

Circular orbit
One radius, one speed, √(μ / r). The period is 2π √(r³ / μ). Around the Sun, in years and AU, that period is the P² = a³ of the Kepler desk. Here μ is Earth’s, and the radius is kilometers.
Geostationary
The circular period equals Earth’s sidereal rotation, so the satellite and the ground turn together. On these constants that altitude is 35,786.05 km. A real geostationary satellite is also equatorial. Geosynchronous is the wider word: the period matches, and the inclination may not be zero. This button is the period.
Ground track
During one orbit the Earth turns east by 360° × P / 23.9345 h. The next equatorial crossing is that far west of the previous one. At geostationary altitude the turn is exactly one rotation, so the crossing does not step. No J2, so no extra nodal drift. A cited inclination changes which latitudes the track reaches. It is not in this angle.
Horizon
From a sphere, the limb is the tangent. The line-of-sight distance is √(r² − R²). The distance along the ground is R × arccos(R / r). The visible cap is (1 − R / r) / 2 of the surface. It never reaches a half. Refraction is left out.
Light time
Straight down and straight back: 2 × altitude / c, with c = 299,792.458 km/s. A station off to the side is a longer slant. The readout is the nadir round trip. The one-way time is half of it.
Ellipse
Perigee and apogee set a = (rp + ra) / 2 and e = (ra − rp) / (ra + rp). The period still comes from a alone. The speeds are vis-viva, v = √[μ (2/r − 1/a)], faster at perigee. The vis-viva desk is that formula for the planets. The Moon button uses the fact-sheet perigee and apogee. Earth’s GM alone does not reproduce the sheet’s 27.3217-day month or its 1.082 and 0.970 km/s. The sheet’s Moon GM is not added.

Sources · public pages

Cited, not invented

Classroom picture of one Earth orbit. GM, equatorial radius, and the sidereal day are the Earth Fact Sheet. Preset sizes are the cited altitudes or radii. Periods, speeds, the ground track, the horizon, and the light time are computed. Simplified two-body model. Circular unless an ellipse is set. Not for mission planning. Earthrise preview: NASA / Bill Anders (public domain).

Keep going

The ellipse

Vis-viva

v = √[μ (2/r − 1/a)] anywhere on one ellipse. Earth’s perihelion rounds to 30.29 km/s. The speeds at perigee and apogee here are that formula.

The coast

Hohmann

Half an ellipse from a low circle up to the geosynchronous radius. Same GM and the same sidereal day. Not a mission.

The speed

Escape

Circular orbit and escape at one altitude. √2 apart. A cannon diagram, not this coast.

The year

Kepler

P² = a³ in years and AU, for a circular orbit around the Sun. The same period law, another μ.

The bulges

Tides

The Moon’s distance, held fixed, and what it does to the oceans. Not this orbital period.

The spin

Sidereal

Why 23.9345 hours, not 24.0000, is the turn that sets geostationary altitude.

The shape

Eccentricity

How e sets periapsis and apoapsis. The ellipse switch on this page is that stretch, around Earth.

Neighborhood

Solar map

Where Earth sits. Day and local time, still a schematic.