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Physics · Ch 7 — Gravitation

Geostationary Satellite

7.13

Geostationary Satellite

A geostationary satellite is an Earth satellite that appears completely stationary in the sky when viewed from any fixed point on the ground -- an enormously useful property for communication and weather-monitoring satellites, since a ground antenna aimed at it never needs to be re-pointed to keep tracking it. This appearance of standing still requires three conditions to hold simultaneously:

  1. The orbit must lie exactly in the equatorial plane of the Earth (an orbit tilted at any angle to the equator would still carry the satellite visibly north and south across the sky over the course of each day, even if its period matched the Earth's rotation).
  2. The satellite must orbit in the same sense as the Earth's own rotation -- eastward.
  3. Its orbital period must exactly equal the Earth's own rotation period (very close to 24 h24\ \text{h}; more precisely, one sidereal day, about 23 h 56 min23\ \text{h}\ 56\ \text{min}, though 24 h24\ \text{h} is used as the standard approximation in problems).

With all three conditions met, the satellite completes exactly one orbit in exactly the time the Earth itself takes to complete one rotation, so it stays permanently above the same fixed point on the equator, appearing motionless from the ground (see the accompanying figure).

Finding the orbital radius. Since a geostationary orbit is circular, the period relation derived in Section 7.11, T=2πr3/GMT = 2\pi\sqrt{r^3/GM}, applies directly. Squaring and solving for rr,

r=(GMT24π2)1/3r = \left(\frac{GMT^2}{4\pi^2}\right)^{1/3}

Taking M=6×1024 kgM = 6 \times 10^{24}\ \text{kg}, G=6.674×10−11 N m2/kg2G = 6.674 \times 10^{-11}\ \text{N}\,\text{m}^2/\text{kg}^2 (so GM≈4.00×1014 m3/s2GM \approx 4.00 \times 10^{14}\ \text{m}^3/\text{s}^2) and T=24 h=86400 sT = 24\ \text{h} = 86400\ \text{s},

r=((4.00×1014)(86400)24π2)1/3≈4.2×107 m=4.2×104 kmr = \left(\frac{(4.00\times 10^{14})(86400)^2}{4\pi^2}\right)^{1/3} \approx 4.2 \times 10^{7}\ \text{m} = 4.2 \times 10^{4}\ \text{km}

Subtracting the Earth's own radius, R≈6400 kmR \approx 6400\ \text{km}, gives the satellite's height above the surface,

h=r−R≈42,000 km−6400 km≈3.6×104 kmh = r - R \approx 42{,}000\ \text{km} - 6400\ \text{km} \approx 3.6\times 10^{4}\ \text{km} …

Figure 1Geometry of a geostationary satellite's orbit

What this figure shows. A cross-sectional view of the Earth viewed from above its North Pole, with the equatorial plane drawn as a circle and a small arrow on the Earth's outline showing its direction of spin, eastward (anticlockwise as drawn). A second, larger concentric dashed circle, well outside the Earth's own outline and lying exactly in the same equatorial plane, represents the satellite's orbit, drawn to scale roughly 6.66.6 times the Earth's own radius (the real ratio, since the orbit's radius from the Earth's centre is about 42,000 km42{,}000\ \text{km} against the Earth's own radius of about 6400 km6400\ \text{km}). A small satellite icon sits on this outer circle, with an arrow showing it moving in the SAME sense (eastward) as the Earth's own spin, and a dashed radial line drawn from the Earth's centre out to the satellite is labelled rr. A short caption notes that because the satellite's orbital period exactly equals the Earth's own rotation period, and both turn the same way i …