Spaceflight

The orbit that has to be paid for every year

A geostationary satellite is not in equilibrium in any direction. The Sun and Moon tilt its plane by 0.85 degrees a year, the Earth's equatorial ellipticity makes two longitudes stable and two unstable, and the end of a satellite's life is the end of its propellant.

Assumes Oblateness and Plane change.

A geostationary satellite is described as parked. It sits over a fixed longitude, a dish on the ground points at it and never moves again, and the arrangement has the look of something that has been solved.

Nothing about it is at rest. The orbit is a compromise between four perturbations that pull in different directions, none of which is negligible, and holding the satellite where the dish expects it costs propellant continuously. When the propellant runs out the spacecraft is still perfectly functional and its mission is over, which is a striking way for an engineering system to end.

Where the fuel goes, and it is not where a satellite points. Left, the orbit pole of a geostationary satellite, in degrees from the Earth's. The Sun and the Moon between them carry it round a circle of radius 7.4° in 53 years, and a satellite launched into the equatorial plane starts on the rim of that circle rather than at its centre — so its inclination climbs from zero at 0.88° a year, reaches 14.8° after 27 years, and comes back. Right, what holding it costs. A plane change of 0.88° at 3.07 km/s is 47.1 m/s a year; holding the longitude against the equatorial bulge, computed from the same resonant term that makes the longitude a pendulum, is 1.8 m/s a year. North–south is 96% of the budget, and a satellite that gives up on it does not fail — it starts tracing a figure of eight on the sky 1.8° tall in the first year, which a fixed dish cannot follow and a steerable one can. Retiring at the end of the propellant is therefore a choice about which service ends first.
Fig. 1 Left, the orbit pole of a geostationary satellite, in degrees from the Earth’s. The Sun and Moon between them carry it round a circle of radius 7.4° in 53 years, and a satellite launched into the equatorial plane starts on the rim of that circle rather than at its centre — so its inclination climbs from zero at 0.88° a year, reaches 14.8° after 27 years, and comes back. Right, what holding it costs: a plane change of 0.88° at 3.07 km/s is 47 m/s a year, against 1.8 m/s a year to hold the longitude. North–south is 96% of the budget, and it is the number that decides how long a satellite lives.

Why the plane will not stay put

The Earth’s equator is inclined 23.4° to the ecliptic, so the Sun’s pull on a satellite in the equatorial plane has a component out of that plane for most of the year. The Moon’s orbit is inclined about 5° to the ecliptic, so it does the same and with a different period.

Averaged over a year, the effect of both is a torque that carries the orbit’s angular momentum vector — its pole — around a fixed direction, in the same way that the lunisolar torque on the Earth’s own equatorial bulge carries the rotation pole around. The direction it circles is not the Earth’s pole; it is a compromise between the Earth’s pole and the ecliptic pole, lying about 7.4° from the first, and the circuit takes about 53 years.

The consequence is geometric and unavoidable. A satellite launched into the equatorial plane has its pole at the Earth’s pole, which is a point 7.4° from the centre of that circle — that is, on its rim. Carried round the rim, its inclination is the distance from the Earth’s pole, which starts at zero, rises to twice 7.4°, and returns.

An inclination of zero is not a stable state; it is the worst possible starting point on a circle it is being carried round.

What 28.5° of plane change costs, at three orbital speeds. The cost of rotating an orbital plane, 2v sin(Δi/2), against the angle turned, for the three speeds a transfer to geostationary orbit passes through: 7.669 km/s in a 400 km circular orbit, 3.075 km/s once circular at 42,164 km, and 1.618 km/s at the apogee of the ellipse between them. All three are √(μ/r) or vis-viva at μ⊕ = 398,600 km³/s². A 28.5° turn therefore costs 3.775, 1.514 or 0.797 km/s depending only on where it is done — the apogee figure is 21% of the low one, and that fraction is the speed ratio, so it is the same at every angle. Past 23.9° a turn in the low orbit costs more than the 3.176 km/s that leaves Earth from it, and a full reversal costs 2v = 15.34 km/s, 4.8 times the escape burn.
Fig. 2 Why the correction is so expensive. The Δv for a plane change is 2vsin(Δi/2)2v\sin(\Delta i/2), so the cheapest place to turn is where the speed is lowest — and a geostationary satellite is at a fixed radius and a fixed speed of 3.07 km/s, with no low-speed point available. A degree of turn costs 54 m/s at that speed. The satellite is stuck at the expensive end of this curve for its whole life, which is why the north–south budget dominates everything else by a factor of twenty-five.

The longitude is a pendulum

The east–west problem is quite different in character, and it is the more interesting one.

The Earth’s equator is not a circle. Its ellipticity is small — the equatorial radii differ by about 70 metres — but a geostationary satellite orbits at exactly the rotation rate, so the perturbation from that asymmetry is resonant: the same small force acts in the same direction on every revolution instead of averaging out. The result is a longitude acceleration

λ¨=18n2J22(Ra)2sin2(λλ22),\ddot\lambda = 18\,n^2 J_{22}\left(\frac{R_\oplus}{a}\right)^2\sin 2(\lambda - \lambda_{22}),

peaking at 1.7×1031.7\times10^{-3} degrees per day squared.

Two longitudes a satellite falls towards, and two it falls away from. Above, the longitude acceleration a geostationary satellite feels from the Earth's equatorial ellipticity, at every longitude: 18n²J₂₂(R⊕/a)² sin 2(λ − λ₂₂), peaking at 1.70e-3 degrees per day squared. It vanishes at four longitudes and only two of them are places to sit. The bulge points at 14.91°W, and that longitude and its antipode are unstable — the acceleration there points away — while 75.1°E and 104.9°W, a quarter turn from the bulge, restore. Below, a satellite abandoned at 45°E: it does not drift away, it librates, swinging past the stable point and back with a period of 2.4 years. Every dead geostationary satellite is doing this now, and the two stable longitudes are the crowded graveyards it produces. The published stable points are 75.3°E and 104.7°W; the two here come from the resonant term alone, and the tenth of a degree between them is the higher harmonics this figure leaves out.
Fig. 3 Above, that acceleration at every longitude. It vanishes at four places and only two of them are places to sit. The bulge points at 14.91°W, and that longitude and its antipode are unstable — the acceleration there points away — while 75.1°E and 104.9°W, a quarter turn from the bulge, restore. Below, a satellite abandoned at 45°E: it does not drift away, it librates, swinging past the stable point and back with a period of 2.4 years. Every dead geostationary satellite is doing this now, and the two stable longitudes are the crowded graveyards it produces.

The distinction between the two stable points and the two unstable ones is the whole of east–west station-keeping. A satellite stationed near a stable longitude is being pulled back towards it and needs very little correction; one stationed near an unstable longitude is being pushed away and needs the most. Most of the commercially desirable longitudes — over the Atlantic, over Europe, over the Americas — are neither, and the cost is somewhere between.

Node regression against inclination, at 20200 km. The rate at which an orbit's node moves under the Earth's oblateness, against the orbit's inclination, for a circular orbit at 20200 km. It is proportional to cos i, so a polar orbit does not drift at all and a retrograde one drifts the other way — and at this altitude the largest rate available anywhere on the curve is 0.067° a day, short of the 0.986 a sun-synchronous orbit needs, so no inclination gives one.
Fig. 4 The drift that does not have to be paid for, at the altitude where it is small. Node regression falls off as the inverse three-and-a-half power of the semi-major axis, so a navigation satellite at 20,200 kilometres precesses more than two orders of magnitude more slowly than one in low orbit — slowly enough that the constellation’s geometry is maintained rather than fought. Which drifts cost fuel is a question about altitude before it is a question about mission, and the same table of terms answers it everywhere.
Node regression against inclination, at 35786 km. The rate at which an orbit's node moves under the Earth's oblateness, against the orbit's inclination, for a circular orbit at 35786 km. It is proportional to cos i, so a polar orbit does not drift at all and a retrograde one drifts the other way — and at this altitude the largest rate available anywhere on the curve is 0.013° a day, short of the 0.986 a sun-synchronous orbit needs, so no inclination gives one.
Fig. 5 Node regression against inclination at geostationary altitude itself. The rate is tiny compared with a low orbit’s — the oblateness term falls as the seven-halves power of the radius — and it is not the term that matters here: at this altitude the plane is turned by the Sun and the Moon rather than by the Earth’s own bulge. Which perturbation dominates is a function of altitude alone, and the crossover is what makes a geostationary station-keeping budget look nothing like a low-orbit one.

The box, and what it is a statement about

An operator holds a satellite within a station-keeping box, quoted as ±0.05°\pm 0.05° or ±0.1°\pm 0.1° in latitude and longitude. That box is not a tolerance in the engineering sense; it is a statement about how much of each perturbation is being tolerated before a correction is made.

The latitude half-width is the inclination allowed to accumulate before a north–south manoeuvre. At 0.88° a year, holding ±0.05°\pm 0.05° means a manoeuvre roughly every three weeks; holding ±0.1°\pm 0.1° halves the manoeuvre count and doubles the excursion. The total Δv is the same either way — it is set by the drift rate, not by the box — so a wider box saves operational effort and not fuel.

The longitude half-width is the amplitude of the libration allowed before an east–west burn, and here the box does affect the cost, weakly: a satellite allowed to drift further spends more time away from its nominal longitude but is corrected less often, and since the acceleration is quadratic in the excursion the total cost falls slightly with a wider box.

Only a few tens of metres of pointing on the ground correspond to a tenth of a degree at geostationary distance, so the boxes are set by the beamwidth of the dishes on the ground rather than by anything about the spacecraft.

What was actually measured

The numbers in this essay are all operational rather than theoretical, and they are among the best-checked in astrodynamics because thousands of spacecraft have paid them.

North–south: 45 to 51 m/s per year. The variation is real and it is the Moon’s node. The lunar orbital plane precesses with an 18.6-year period, so the combined lunisolar torque varies over that cycle and the annual inclination drift runs between about 0.75 and 0.95 degrees. An operator budgeting for a fifteen-year mission has to take the high end.

East–west: 0.5 to 2 m/s per year, depending on longitude, plus a comparable amount for eccentricity control. Solar radiation pressure drives the eccentricity round an annual cycle whose amplitude depends on the area-to-mass ratio; a satellite with large solar arrays and low mass — which is every modern communications satellite — sees an eccentricity excursion of a few times 10410^{-4}, corresponding to a daily longitude oscillation of a few hundredths of a degree.

Total, over a fifteen-year life: about 750 m/s. For a spacecraft with a mass of five tonnes and an apogee engine exhaust velocity of 3 km/s, that is 1.1 tonnes of propellant carried for station-keeping alone — a fifth of the launch mass, entirely to stay still.

The end, which is a manoeuvre

A satellite that simply stops is a hazard, because it librates into one of the two stable longitudes and joins the population already there. The IADC guideline, and now the licence condition in most jurisdictions, is that a geostationary spacecraft must be raised at least 235 km + 1000CRA/m1000\,C_R A/m above the geostationary ring before it is passivated — a graveyard orbit high enough that solar radiation pressure will not bring it back down through the ring.

That manoeuvre costs about 11 m/s, or roughly three months of station-keeping propellant, and it has to be performed while enough propellant remains to perform it. Estimating the remaining propellant in a fifteen-year-old spacecraft, from tank pressures and thruster-firing histories, is one of the genuinely uncertain quantities in the business, and the usual practice is to retire with a margin — which is to say, to end a working mission early because the fuel gauge cannot be trusted.

Node regression against inclination, at 800 km. The rate at which an orbit's node moves under the Earth's oblateness, against the orbit's inclination, for a circular orbit at 800 km. It is proportional to cos i, so a polar orbit does not drift at all and a retrograde one drifts the other way — and at 98.6° the drift is exactly one turn a year, which is what makes a sun-synchronous orbit possible.
Fig. 6 And the same relation at eight hundred kilometres, where the oblateness term is at its largest. The regression rate reaches several degrees a day at low inclination and passes through zero at 90°, and the inclination where it matches the Earth’s mean motion about the Sun is the sun-synchronous one. The same curve is a nuisance at one altitude and a design tool at another, and nothing about the physics differs between the two readings.

Four perturbations, one table

Setting them beside each other is the fastest way to see why the budget is shaped as it is.

Perturbation What it does Annual cost
Lunisolar torque tilts the plane by 0.85–0.95° 45–51 m/s
Equatorial ellipticity (J22J_{22}) drives longitude towards 75°E or 105°W 0.5–2 m/s
Solar radiation pressure pumps the eccentricity annually ~1 m/s
Earth’s oblateness (J2J_2) precesses the node 0 — absorbed into the definition

The last row is the one worth explaining. J2J_2 is by far the largest perturbation on a low orbit and it costs a geostationary satellite nothing at all, because its effect at synchronous radius is a slow rotation of the node within a plane that is already being defined by the operator. The nominal radius of 42,164.17 km already includes the J2J_2 correction to the period, so the perturbation has been absorbed into what “geostationary” means rather than being fought.

A perturbation is only a cost if it moves the spacecraft relative to what the mission needs, and three of these four do.

The same reading explains why the inclination is fought and the longitude libration is merely managed. A drifting inclination breaks the geometry the ground segment was built around — a fixed dish sees the satellite move — and there is no cheap way to accommodate it. A librating longitude, by contrast, is a slow oscillation about a point, and a satellite can simply be stationed at a stable longitude and left to swing within its box, which is why the two graveyard longitudes are also the two cheapest places to operate.

The same thrust is worth 2.08 times more at perigee, and out of plane it is worth nothing at all. The rate of change of the semi-major axis under a unit acceleration in each of the three directions, against position around an orbit of eccentricity 0.35, from Gauss's variational equations. The along-track curve carries the factor p/r = 1 + e cos f and therefore peaks at perigee, where the same impulse is worth 2.08 times what it is worth at apogee — the whole of the Oberth effect, arriving as a term in a differential equation rather than as an argument about kinetic energy. The radial curve is antisymmetric about apoapsis and integrates to exactly zero over a revolution: pushing outwards for half an orbit and being pushed back for the other half changes the energy by nothing, which is checked here by quadrature and comes out at -9.0e-18. And the out-of-plane response is identically zero at every point of the orbit, because W is perpendicular to the velocity and does no work. An orbital plane can be rotated without touching the energy, and that is why a plane change is so expensive: none of what is spent goes anywhere useful.
Fig. 7 Where a given burn actually goes, which decides what is worth paying for. Gauss’s variational equations split a thrust into three directions and say what each one moves: along-track changes the energy and therefore the semi-major axis, radial mostly shifts the periapsis around, and out-of-plane changes the inclination and the node and nothing else. The same thrust is worth 2.08 times more at periapsis for raising the orbit and worth nothing at all out of plane — so station-keeping budgets are not a total but a list, one line per element, each with its own cheapest place to burn.

The ring is a scarce resource, and the scarcity is not gravitational

Everything so far treats a longitude as a place a satellite can be put. Whether it may be is a separate question, settled by treaty rather than by dynamics, and the reason is interference.

Two satellites at nearby longitudes are seen from the ground at nearby angles, and a dish has a finite beamwidth. A three-metre antenna at C band has a main lobe around two degrees across, so a satellite two degrees away is inside the beam and its transmissions arrive alongside the wanted signal. The spacing of the ring is therefore set by the size of the receiving antennas rather than by anything about orbits, and the historic figure of two degrees comes from exactly that calculation.

Two degrees of spacing gives 180 positions in a full circle, and the useful arc is much smaller than a circle for any given service area — a satellite serving Europe has to be visible from Europe at a workable elevation angle, which confines it to perhaps 70 degrees of longitude. The result is that the commercially valuable arc holds a few dozen slots, and they are allocated by the International Telecommunication Union through a filing and coordination process that has produced its own economy of speculative registrations.

The station-keeping box connects to this directly. A satellite held to ±0.05°\pm0.05° occupies a tenth of a degree; one that has stopped correcting its longitude wanders through several degrees and through its neighbours’ slots. So the box is not only about keeping a dish pointed — it is the condition on which the slot was granted, and a satellite that cannot hold it has to leave.

Where the fuel goes, and it is not where a satellite points. Left, the orbit pole of a geostationary satellite, in degrees from the Earth's. The Sun and the Moon between them carry it round a circle of radius 7.4° in 53 years, and a satellite launched into the equatorial plane starts on the rim of that circle rather than at its centre — so its inclination climbs from zero at 0.88° a year, reaches 14.8° after 27 years, and comes back. Right, what holding it costs. A plane change of 0.88° at 3.07 km/s is 47.1 m/s a year; holding the longitude against the equatorial bulge, computed from the same resonant term that makes the longitude a pendulum, is 1.8 m/s a year. North–south is 96% of the budget, and a satellite that gives up on it does not fail — it starts tracing a figure of eight on the sky 1.8° tall in the first year, which a fixed dish cannot follow and a steerable one can. Retiring at the end of the propellant is therefore a choice about which service ends first.
Fig. 8 The lunisolar torque at the semi-synchronous altitude of a navigation constellation rather than at geostationary. The inclination is driven through a long-period oscillation whose amplitude depends on the orbit’s initial orientation, and for these orbits it is large enough that the constellation is designed around it rather than corrected — the satellites are launched into an inclination chosen so that the drift carries them through the useful range rather than out of it. Station-keeping and orbit selection are the same decision made at different times.

Steering the eccentricity rather than fighting it

Solar radiation pressure entered the budget above as a one-metre-a-second annual nuisance, and the way it is handled is a good example of working with a perturbation instead of against it.

The pressure acts in the anti-solar direction, so as the Sun goes round the sky over a year, the force direction rotates with it. Its effect is to push the orbit’s eccentricity vector — the vector pointing towards perigee with length ee — around a circle, once a year, with a radius set by the spacecraft’s area-to-mass ratio. For a modern platform with large arrays that radius corresponds to e3×104e \approx 3\times10^{-4}, which is a daily east–west oscillation of a few hundredths of a degree.

Fighting that means burning to keep ee near zero, continuously, all year. The alternative — the sun-pointing perigee strategy — is to place the eccentricity vector deliberately so that the annual circle traced by the radiation pressure is centred on the origin rather than starting there. The eccentricity then goes round a closed loop of fixed radius, never growing, and the longitude oscillation it produces is a constant known amplitude that the box is sized to accommodate.

Nothing is corrected and nothing accumulates. The manoeuvres that remain are the east–west drift corrections, which are then timed so that each one also places the eccentricity vector where the coming year’s solar cycle wants it. One burn, two purposes, and a perturbation converted from a cost into a constraint on when the burn is scheduled.

One inclination per altitude, and all of them retrograde. The inclination at which a circular orbit's node keeps exact pace with the Sun, against altitude. Every point satisfies −(3/2)J₂(R/p)²n cos i = 0.9856°/day, checked at each drawn point rather than at the ends: 96.67° at 300 km rising to 100.42° at 1200. All of it is retrograde, because a prograde orbit's node moves the wrong way and no prograde inclination can be made to follow the Sun at any altitude. The curve rises because n and (R/p)² both fall with height, so a higher orbit needs more of the cosine to make up the same rate — and it runs out: past 5,974 km the fastest rate available, the one at 180° where cos i = −1, is already slower than the Sun's, and no inclination works at any price. Landsat sits at 705 km and 98.2°.
Fig. 9 The sun-synchronous condition over a narrower altitude range, marked at Landsat’s orbit alone. One inclination per altitude, and the curve is steep enough that a hundred kilometres of altitude is nearly a degree of inclination — which is why a launch that under-performs by a hundred kilometres does not simply arrive low, it arrives in the wrong plane and cannot be corrected without a plane change nobody budgets for.

Several satellites in one box

The scarcity above has an obvious response — put more than one spacecraft at the same longitude — and it creates a collision problem inside a volume a few tens of kilometres across.

Two satellites in the same box cannot simply be flown to the same nominal position, because their errors are independent and their separation would be uncontrolled. What is done instead is eccentricity and inclination vector separation: the two spacecraft are given eccentricity vectors pointing in opposite directions, or inclination vectors similarly opposed, so that whenever one is at the east side of the box the other is at the west, or one is north when the other is south.

The geometry is arranged so that the two separations are never simultaneously zero. A satellite whose radial offset vanishes has, at that moment, a maximal cross-track offset, and the minimum distance between the two over a day is a few kilometres rather than a few metres — held by the shape of the two orbits rather than by any active avoidance.

Four or five satellites have been colocated this way at a single longitude. The scheme’s cost is that it consumes part of the box: the separations use up the tolerance that would otherwise absorb station-keeping error, which means tighter control on each spacecraft and more frequent manoeuvres. It is the ring’s scarcity being paid for in propellant.

There is a limit to how far the trick scales. Each additional spacecraft needs its own pair of separations, and the available room in the box is fixed, so the practical ceiling is around four or five — beyond which the required control accuracy on each satellite costs more propellant than the shared slot is worth. The arithmetic that makes colocation attractive is the same arithmetic that stops it.

None of this applies to the constellations in low orbit, where the satellites are numerous, individually cheap and short-lived, and the separation is maintained by continuous propulsion and active avoidance rather than by orbit design. The geostationary ring is the last place in spaceflight where a single spacecraft’s position is a scarce and individually negotiated asset, and the practices in this essay are what that scarcity produced.

It is also the one regime where a satellite’s operators can say precisely what its remaining life is, because the limiting consumable is measured in metres per second and the drain is known to a few per cent a year. Everywhere else in spaceflight a mission ends when something breaks; here it ends on a schedule that was written before launch.

Two practical matters follow from all of this and are worth stating, because they are where the arithmetic meets an operator’s decisions.

The first is that the two station-keeping budgets are not comparable in size. East–west keeping, against the triaxiality that drives the longitude pendulum, costs of order two metres a second a year. North–south keeping, against the lunisolar torque on the plane, costs about fifty — twenty-five times as much, and it is the whole of the difference between a satellite’s fuelled lifetime and the fifty years its hardware might last. So a satellite near the end of its propellant is often taken out of north–south keeping and allowed to drift in inclination, reaching a degree or two over a few years. It is then still useful: a ground station with a steerable antenna can follow the resulting daily figure-of-eight, and the satellite is leased for services that can tolerate it. Inclined-orbit operation is the industry’s ordinary way of trading a ground-segment cost against an orbital one, and it exists because one of the two budgets is far larger than the other.

The second is that the disposal orbit is not a fixed altitude. The standard requires a satellite to be raised far enough above the ring that solar radiation pressure cannot bring it back, and since that pressure acts on area while gravity acts on mass, the required height depends on the vehicle’s area-to-mass ratio: a few hundred kilometres for a compact satellite, more for one with large arrays. The formula is written into the guidelines rather than a single number, and the manoeuvre costs about eleven metres a second — a few months of north–south keeping, spent at the end on the one manoeuvre that returns nothing.

Where the model stops

The account above treats the four perturbations as independent, and at the level of a budget they are. They are not independent in detail.

The north–south manoeuvre changes the plane, which changes the resonant longitude acceleration slightly; the east–west manoeuvre changes the semi-major axis, which changes the drift rate; and both are performed by thrusters mounted on a spacecraft whose attitude is itself being controlled, so every burn has a component in a direction nobody wanted. Modern operations combine the two into a single manoeuvre with the thrust vector chosen to deliver both components, which saves propellant and complicates the analysis.

The 7.4° figure for the forced plane is also not a constant. It depends on the satellite’s own semi-major axis, and for orbits away from geostationary the balance between the Sun’s and the Moon’s contributions shifts — at low altitudes the Earth’s own oblateness dominates and the whole picture is different, which is what makes a sun-synchronous orbit possible at 800 km and impossible at 36,000.

One inclination per altitude, and all of them retrograde. The inclination at which a circular orbit's node keeps exact pace with the Sun, against altitude. Every point satisfies −(3/2)J₂(R/p)²n cos i = 0.9856°/day, checked at each drawn point rather than at the ends: 96.33° at 200 km rising to 102.51° at 1600. All of it is retrograde, because a prograde orbit's node moves the wrong way and no prograde inclination can be made to follow the Sun at any altitude. The curve rises because n and (R/p)² both fall with height, so a higher orbit needs more of the cosine to make up the same rate — and it runs out: past 5,974 km the fastest rate available, the one at 180° where cos i = −1, is already slower than the Sun's, and no inclination works at any price. A sun-synchronous orbit sits at 786 km and 98.5°; Landsat sits at 705 km and 98.2°.
Fig. 10 The regime where a perturbation is used rather than fought. At low altitude the Earth’s oblateness regresses the node fast enough that an inclination can be chosen to make the regression exactly one degree a day — so the orbit plane keeps a fixed angle to the Sun for free, and every image is taken at the same local time. The same class of perturbation is a design tool at 800 km and a fuel bill at 36,000 km, and the difference is only which one happens to dominate.

One asymmetry runs under all four perturbations and is worth naming. Three of them — oblateness, triaxiality, lunisolar — are conservative: they move an element back and forth, and a satellite that could wait long enough would find its orbit returned. Solar radiation pressure is not, because the photons are absorbed and re-emitted rather than reflected elastically, and because the satellite’s own attitude changes what area it presents. So the eccentricity it drives is genuinely pumped rather than merely oscillated, which is why the strategy for it is to choose an orientation that makes the drift close on itself rather than to cancel it. The distinction between a perturbation that oscillates and one that accumulates decides whether a budget is a rate or a total, and it is the first question to ask of any term in the table above.

Where this ladder goes next

This rung is the geostationary case, which is the one with the largest fleet and the clearest economics. The rungs above it generalise in two directions.

One is other stations. A spacecraft at Sun–Earth L2L_2 is at an unstable equilibrium and drifts off exponentially with an ee-folding time of about three weeks, yet holds its position for a few metres per second a year — a thousandth of the geostationary cost, because the instability can be cancelled while it is still small rather than fought continuously. The tubes that make that point a gateway are the same structures that make it cheap to sit at, and the contrast between the two budgets is a good illustration of what an equilibrium is worth.

The other is what happens when the budget is not paid. The graveyard population, the inclined-orbit secondary market for ageing satellites, and the growing question of whether refuelling or robotic servicing changes the arithmetic — the first such docking, of MEV-1 to Intelsat 901 in 2020, added five years to a satellite that had run out of nothing but propellant.

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End of lifeGeostationary orbitGraveyard orbitInclination driftLibrationLunisolar perturbationSolar radiation pressureStation-keepingStation-keeping boxTriaxiality