Circular Orbits and Geostationary Satellites

A2 · 10 min

A satellite in a circular orbit is an object in permanent free fall: gravity pulls it towards the planet, but it moves sideways fast enough that it keeps missing. Linking Newton's law of gravitation to centripetal force gives the speed and period of any circular orbit, lets us "weigh" planets and stars from the motion of their moons, and explains why geostationary satellites must sit at one particular height above the Equator. Orbit calculations and the derivation of T2∝r3T^2 \propto r^3 appear in almost every Paper 4.

Gravity provides the centripetal force

For a satellite of mass mm in a circular orbit of radius rr around a planet of mass MM, the only force acting is the planet's gravitational pull. It points towards the centre of the planet, which is the centre of the orbit, so it is exactly the centripetal force:

Key result
GMmr2=mv2r=mrω2\frac{GMm}{r^{2}} = \frac{mv^{2}}{r} = mr\omega^{2}

Gravitational force == mass ×\times centripetal acceleration. The satellite's mass mm cancels.

Because mm cancels, every object at the same orbital radius around the same planet has the same speed and period, whether it is a space station or a spanner dropped by an astronaut.

Orbital speed

Cancelling mm and one factor of rr:

GMr=v2⇒v=GMr\frac{GM}{r} = v^{2} \quad\Rightarrow\quad v = \sqrt{\frac{GM}{r}}

Satellites in lower orbits move faster. The International Space Station, a few hundred kilometres up, moves at nearly 8 km s−18\ \text{km s}^{-1}; the Moon, far away, moves at about 1 km s−11\ \text{km s}^{-1}.

Orbital period: deriving T2∝r3T^2 \propto r^3

This derivation is a frequent "show that" question. Write it out in full.

Period of a circular orbit

The gravitational force provides the centripetal force:

GMmr2=mrω2\frac{GMm}{r^{2}} = mr\omega^{2}

Substitute ω=2πT\omega = \dfrac{2\pi}{T}:

GMmr2=mr(2πT)2=4π2mrT2\frac{GMm}{r^{2}} = mr\left(\frac{2\pi}{T}\right)^{2} = \frac{4\pi^{2}mr}{T^{2}}

Cancel mm and rearrange:

T2=4π2GM r3T^{2} = \frac{4\pi^{2}}{GM}\,r^{3}

Since 4π2/(GM)4\pi^2/(GM) is a constant for a given central mass, T2∝r3T^2 \propto r^3. This is Kepler's third law.

Key result
T2=(4π2GM)r3T^{2} = \left(\frac{4\pi^{2}}{GM}\right) r^{3}

A graph of T2T^2 against r3r^3 for all the satellites of one planet is a straight line through the origin with gradient 4π2/(GM)4\pi^2/(GM). A graph of lg⁡T\lg T against lg⁡r\lg r is a straight line of gradient 1.51.5.

The same equation is the most common way to find the mass of a central body: measure the radius and period of anything orbiting it, then

M=4π2r3GT2M = \frac{4\pi^{2}r^{3}}{GT^{2}}

Notice what you can and cannot find this way: the central mass MM, never the mass of the orbiting body.

Geostationary orbits

A geostationary satellite stays above the same point on the Earth's surface at all times. That makes it ideal for communications and broadcasting: a ground dish can point at it permanently without tracking.

Definition

A satellite in a geostationary orbit:

  • remains at the same point above the Earth's surface;
  • has an orbital period of 2424 hours, the same as the Earth's rotation;
  • orbits from west to east, in the same direction as the Earth rotates;
  • is directly above the Equator.

Why each condition is needed:

  • Period 24 hours: the satellite must turn through the same angle as the ground beneath it in the same time.
  • West to east: it must rotate in the same sense as the Earth, otherwise it would move across the sky.
  • Above the Equator: the centre of every orbit must be the centre of the Earth (gravity points there). An orbit inclined to the Equator would carry the satellite north and south of the Equator each day, so only an equatorial orbit can stay above a fixed point.

Because the period is fixed, T2∝r3T^2 \propto r^3 means the radius is fixed too: there is only one geostationary orbit radius, about 4.2×107 m4.2 \times 10^{7}\ \text{m} from the centre of the Earth (about 36 000 km36\,000\ \text{km} above the surface).

Tip

Strictly, the Earth rotates once relative to the stars every 2323 hours 5656 minutes (a sidereal day), and a geostationary satellite has that period. The syllabus and mark schemes use 2424 hours; use 2424 hours unless a question gives you something else. The difference in radius is less than 0.2%0.2\%.

Geostationary satellites are not the only useful kind. Satellites in low orbits (a few hundred kilometres up) take about 9090 minutes per orbit. They pass over different parts of the Earth on each orbit, giving detailed, close-up images and short signal delays, but a ground station sees each one for only a few minutes. Geostationary satellites are far away, so their images are less detailed and signals take about a quarter of a second for the round trip, but they provide continuous coverage of almost a third of the Earth's surface.

Weightlessness in orbit

Astronauts in an orbiting station are not beyond the reach of gravity: at 400 km400\ \text{km} up, the gravitational field strength is still about 90%90\% of its surface value. They feel weightless because they and their spacecraft are in free fall together, both accelerating towards the Earth at the same rate gg. There is no contact force between astronaut and floor, and it is the contact force that we feel as "weight".

Orbit calculations
  1. Write "gravitational force provides the centripetal force".
  2. Write GMmr2=mv2r\dfrac{GMm}{r^2} = \dfrac{mv^2}{r} or GMmr2=mrω2\dfrac{GMm}{r^2} = mr\omega^2, depending on whether speed or period is involved.
  3. Make sure rr is the distance from the centre of the planet: r=R+hr = R + h.
  4. Convert the period to seconds.
  5. Rearrange symbolically first, then substitute.
  6. For ratio problems between two satellites of the same planet, use T2∝r3T^2 \propto r^3 or v∝1/rv \propto 1/\sqrt{r} directly.

Worked examples

The International Space Station

The International Space Station orbits 400 km400\ \text{km} above the Earth's surface. The Earth has mass 5.97×1024 kg5.97 \times 10^{24}\ \text{kg} and radius 6.37×106 m6.37 \times 10^{6}\ \text{m}. Calculate the orbital speed and the period of the station.

Solution

r=6.37×106+0.40×106=6.77×106 mr = 6.37 \times 10^{6} + 0.40 \times 10^{6} = 6.77 \times 10^{6}\ \text{m}.

Gravitational force provides the centripetal force: GMmr2=mv2r\dfrac{GMm}{r^2} = \dfrac{mv^2}{r}, so

v=GMr=6.67×10−11×5.97×10246.77×106=7.67×103 m s−1v = \sqrt{\frac{GM}{r}} = \sqrt{\frac{6.67 \times 10^{-11} \times 5.97 \times 10^{24}}{6.77 \times 10^{6}}} = 7.67 \times 10^{3}\ \text{m s}^{-1}T=2πrv=2π×6.77×1067.67×103=5.55×103 s (92 minutes)T = \frac{2\pi r}{v} = \frac{2\pi \times 6.77 \times 10^{6}}{7.67 \times 10^{3}} = 5.55 \times 10^{3}\ \text{s} \ (92 \text{ minutes})
Radius of a geostationary orbit

Using the data above, show that the radius of a geostationary orbit is about 4.2×107 m4.2 \times 10^{7}\ \text{m}, and calculate the height above the Earth's surface and the orbital speed.

Solution

T=24×3600=86 400 sT = 24 \times 3600 = 86\,400\ \text{s}.

r3=GMT24π2=6.67×10−11×5.97×1024×(86 400)24π2=7.53×1022 m3r^{3} = \frac{GMT^{2}}{4\pi^{2}} = \frac{6.67 \times 10^{-11} \times 5.97 \times 10^{24} \times (86\,400)^{2}}{4\pi^{2}} = 7.53 \times 10^{22}\ \text{m}^3r=4.22×107 mr = 4.22 \times 10^{7}\ \text{m}

Height above surface: 4.22×107−6.37×106=3.59×107 m4.22 \times 10^{7} - 6.37 \times 10^{6} = 3.59 \times 10^{7}\ \text{m}.

Speed: v=2πr/T=2π×4.22×107/86 400=3.07×103 m s−1v = 2\pi r/T = 2\pi \times 4.22 \times 10^{7}/86\,400 = 3.07 \times 10^{3}\ \text{m s}^{-1}.

Mass of Mars from its moon

Phobos orbits Mars in a circle of radius 9.38×106 m9.38 \times 10^{6}\ \text{m} with a period of 7.657.65 hours. Calculate the mass of Mars.

Solution

T=7.65×3600=2.754×104 sT = 7.65 \times 3600 = 2.754 \times 10^{4}\ \text{s}.

M=4π2r3GT2=4π2×(9.38×106)36.67×10−11×(2.754×104)2=6.44×1023 kgM = \frac{4\pi^{2}r^{3}}{GT^{2}} = \frac{4\pi^{2} \times (9.38 \times 10^{6})^{3}}{6.67 \times 10^{-11} \times (2.754 \times 10^{4})^{2}} = 6.44 \times 10^{23}\ \text{kg}

The mass of Phobos is not needed and cannot be found from this data.

Ratio of periods

Two moons orbit the same planet. Moon A has orbital radius 2.0×108 m2.0 \times 10^{8}\ \text{m} and period 3.03.0 days. Moon B has orbital radius 5.0×108 m5.0 \times 10^{8}\ \text{m}. Calculate the period of moon B and the ratio of their orbital speeds vA/vBv_A / v_B.

Solution

T2∝r3T^2 \propto r^3 for the same central mass:

TB=TA(rBrA)3/2=3.0×(2.5)1.5=11.9 daysT_B = T_A\left(\frac{r_B}{r_A}\right)^{3/2} = 3.0 \times (2.5)^{1.5} = 11.9\ \text{days}

v∝1/rv \propto 1/\sqrt{r}:

vAvB=rBrA=2.5=1.58\frac{v_A}{v_B} = \sqrt{\frac{r_B}{r_A}} = \sqrt{2.5} = 1.58

The inner moon moves faster and has the shorter period.

Using surface gravity instead of G and M

A question gives only g=9.81 N kg−1g = 9.81\ \text{N kg}^{-1} at the Earth's surface and R=6.37×106 mR = 6.37 \times 10^{6}\ \text{m}. Find the period of a satellite orbiting at a radius of 2R2R.

Solution

At the surface g=GM/R2g = GM/R^2, so GM=gR2=9.81×(6.37×106)2=3.98×1014 N m2 kg−1GM = gR^2 = 9.81 \times (6.37 \times 10^{6})^2 = 3.98 \times 10^{14}\ \text{N m}^2\ \text{kg}^{-1}.

T=2πr3GM=2π(1.274×107)33.98×1014=1.43×104 s (about 4.0 hours)T = 2\pi\sqrt{\frac{r^{3}}{GM}} = 2\pi\sqrt{\frac{(1.274 \times 10^{7})^{3}}{3.98 \times 10^{14}}} = 1.43 \times 10^{4}\ \text{s} \ (\text{about } 4.0 \text{ hours})

The substitution GM=gR2GM = gR^2 is a standard trick worth remembering.

Why a geostationary satellite must be above the Equator

A student suggests placing a geostationary satellite permanently above a city at latitude 40∘N40^\circ\text{N}. Explain why this is impossible.

Solution

The only force on the satellite is gravity, which acts towards the centre of the Earth. For a circular orbit, the centripetal force must point to the centre of the orbit, so the plane of every orbit must pass through the Earth's centre. A satellite that stayed above latitude 40∘N40^\circ\text{N} would have to move in a circle centred on a point on the Earth's axis north of the Earth's centre, which gravity cannot provide. An orbit through the Earth's centre that passes over 40∘N40^\circ\text{N} must also pass equally far south of the Equator during each orbit, so the satellite would not stay above the city.

Watch out

Using height instead of radius. In every orbit equation rr is measured from the centre of the planet. Height above surface must have the planet's radius added.

Watch out

Writing "the satellite is weightless because there is no gravity". There is gravity; it provides the centripetal force. The satellite and everything in it are in free fall together.

Watch out

Including the satellite's mass in the answer. The satellite's mass cancels from GMm/r2=mv2/rGMm/r^2 = mv^2/r. If a question gives you the satellite's mass, it is for a later part (such as kinetic energy), not for the speed or period.

Exam tip
  • "Show that T2=(4π2/GM)r3T^2 = (4\pi^2/GM)r^3": start from "gravitational force provides centripetal force", write both expressions, substitute ω=2π/T\omega = 2\pi/T (or v=2πr/Tv = 2\pi r/T), and rearrange. Each step is a mark; skipping straight to the result scores nothing.
  • "State three features of a geostationary orbit": period 24 hours; west to east (same direction as the Earth's rotation); above the Equator. "Stays above the same point" is the definition, so it does not count as an extra feature.
  • Orbit answers are often required to 2 or 3 significant figures; carry at least 4 through the working, especially when cubing or taking square roots.
Summary
  • In a circular orbit, gravity provides the centripetal force: GMm/r2=mv2/r=mrω2GMm/r^2 = mv^2/r = mr\omega^2.
  • Orbital speed v=GM/rv = \sqrt{GM/r}: lower orbits are faster.
  • T2=(4π2/GM)r3T^2 = (4\pi^2/GM)r^3 (Kepler's third law): derive it from the force equation.
  • The mass of the central body is M=4π2r3/(GT2)M = 4\pi^2r^3/(GT^2); the orbiting mass cancels.
  • Geostationary: period 24 hours, west to east, above the Equator, at r≈4.2×107 mr \approx 4.2 \times 10^{7}\ \text{m}; stays above one point on the surface.
  • GM=gR2GM = gR^2 lets you work without GG and MM.
  • Astronauts in orbit are weightless because they are in free fall, not because gravity is absent.

Practice questions

Question
  1. State what provides the centripetal force on a satellite and write the equation linking orbital speed to orbital radius.
  2. Calculate the orbital speed and period of a satellite at a height of 2.0×106 m2.0 \times 10^{6}\ \text{m} above the Earth's surface. (ME=5.97×1024 kgM_E = 5.97 \times 10^{24}\ \text{kg}, RE=6.37×106 mR_E = 6.37 \times 10^{6}\ \text{m})
  3. Calculate the radius of orbit of a satellite with a period of 9090 minutes, and hence its height above the surface.
  4. Two satellites orbit the Earth, one at four times the orbital radius of the other. Find the ratio of their periods.
  5. The Earth orbits the Sun at 1.50×1011 m1.50 \times 10^{11}\ \text{m} once a year (365.25365.25 days). Calculate the mass of the Sun.
  6. Explain why astronauts on the International Space Station appear weightless even though the gravitational field strength there is about 8.7 N kg−18.7\ \text{N kg}^{-1}.
  7. A satellite of mass 500 kg500\ \text{kg} is in geostationary orbit at 4.22×107 m4.22 \times 10^{7}\ \text{m} from the Earth's centre. Calculate its kinetic energy.
  8. (a) Show that, for circular orbits around a planet of mass MM, lg⁡T=32lg⁡r+12lg⁡(4π2GM)\lg T = \tfrac{3}{2}\lg r + \tfrac{1}{2}\lg\left(\dfrac{4\pi^2}{GM}\right). (b) For the moons of a planet, a graph of lg⁡(T/s)\lg(T/\text{s}) against lg⁡(r/m)\lg(r/\text{m}) has gradient 1.501.50 and passes through the point (8.00, 5.20)(8.00,\ 5.20). Determine the mass of the planet.
Answers
  1. The gravitational force of the planet on the satellite. GMm/r2=mv2/rGMm/r^2 = mv^2/r, so v=GM/rv = \sqrt{GM/r}.
  2. r=8.37×106 mr = 8.37 \times 10^{6}\ \text{m}. v=6.67×10−11×5.97×1024/8.37×106=6.90×103 m s−1v = \sqrt{6.67 \times 10^{-11} \times 5.97 \times 10^{24}/8.37 \times 10^{6}} = 6.90 \times 10^{3}\ \text{m s}^{-1}. T=2πr/v=7.62×103 sT = 2\pi r/v = 7.62 \times 10^{3}\ \text{s} (about 127127 minutes).
  3. T=5400 sT = 5400\ \text{s}. r=(GMT2/4π2)1/3=6.65×106 mr = (GMT^2/4\pi^2)^{1/3} = 6.65 \times 10^{6}\ \text{m}; height =6.65×106−6.37×106=2.8×105 m= 6.65 \times 10^{6} - 6.37 \times 10^{6} = 2.8 \times 10^{5}\ \text{m} (about 280 km280\ \text{km}).
  4. T∝r3/2T \propto r^{3/2}: ratio =41.5=8= 4^{1.5} = 8. The outer satellite's period is 88 times longer.
  5. T=365.25×86 400=3.156×107 sT = 365.25 \times 86\,400 = 3.156 \times 10^{7}\ \text{s}. M=4π2r3/(GT2)=4π2×(1.50×1011)3/(6.67×10−11×(3.156×107)2)=2.0×1030 kgM = 4\pi^2r^3/(GT^2) = 4\pi^2 \times (1.50 \times 10^{11})^3/(6.67 \times 10^{-11} \times (3.156 \times 10^{7})^2) = 2.0 \times 10^{30}\ \text{kg}.
  6. The station and the astronauts are both in free fall, accelerating towards the Earth at the same rate (gravity provides their centripetal acceleration). There is no contact force between the astronauts and the station, so they feel weightless.
  7. v2=GM/rv^2 = GM/r, so EK=12mv2=GMm2r=6.67×10−11×5.97×1024×5002×4.22×107=2.36×109 JE_K = \tfrac{1}{2}mv^2 = \dfrac{GMm}{2r} = \dfrac{6.67 \times 10^{-11} \times 5.97 \times 10^{24} \times 500}{2 \times 4.22 \times 10^{7}} = 2.36 \times 10^{9}\ \text{J}.
  8. (a) T2=(4π2/GM)r3T^2 = (4\pi^2/GM)r^3. Take lg⁡\lg of both sides: 2lg⁡T=3lg⁡r+lg⁡(4π2/GM)2\lg T = 3\lg r + \lg(4\pi^2/GM), then divide by 22. (b) Intercept: 5.20=1.50×8.00+c5.20 = 1.50 \times 8.00 + c, so c=−6.80c = -6.80. Then 12lg⁡(4π2/GM)=−6.80\tfrac{1}{2}\lg(4\pi^2/GM) = -6.80, so 4π2/GM=10−13.6=2.51×10−144\pi^2/GM = 10^{-13.6} = 2.51 \times 10^{-14}. M=4π2/(G×2.51×10−14)=2.4×1025 kgM = 4\pi^2/(G \times 2.51 \times 10^{-14}) = 2.4 \times 10^{25}\ \text{kg}.

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