What is a geosynchronous transfer orbit (GTO)?

A GTO is a long, stretched orbit with its low point a few hundred kilometres up and its high point near geostationary height, used to carry satellites towards GEO.

Rockets usually do not carry a satellite all the way to geostationary orbit. Instead they release it on a stretched ellipse: the low point is a few hundred kilometres up, and the high point is near 35,786 km. This is a geosynchronous transfer orbit.

The satellite then fires its own engine near the high point to round the orbit out. That job is called orbit-raising.

The transfer orbit is usually tilted, too. ESA notes that a launch from Kourou, about 500 km north of the equator, leaves a slightly tilted transfer orbit, and the burn at the high point removes that tilt as well. Launches from Cape Canaveral can instead aim the high point above geostationary height — a "supersynchronous" transfer — to save fuel.

Earth transfer orbit perigee 170 km apogee 36,568 km burn at apogee rounds out the orbit GEO circle 35,786 km not to scale
GSLV-F12 left NVS-01 on a 170 × 36,568 km transfer orbit; the satellite's own burns at the high point then rounded the orbit out near geostationary height. Not to scale.

An Indian example: GSLV-F12 and NVS-01

On 29 May 2023 a GSLV launched the 2,232 kg navigation satellite NVS-01 from Sriharikota. ISRO's target orbit was 170 km at the low point and 36,568 km at the high point, tilted 19.36° to the equator.

Today the catalogue shows NVS-01 at 35,751 × 35,820 km with an inclination of 1.84°. The satellite's own burns lifted its low point by about 35,600 km and took out most of the tilt.

When the second step fails

In January 2025 a GSLV placed NVS-02 into its transfer orbit correctly. But when the satellite tried its first orbit-raising burn, the valves that let oxidiser into its thrusters did not open. Without that burn the satellite stayed on its stretched orbit.

Its catalogue orbit is still 214 × 37,251 km, with a period of 660 minutes — 11 hours, not one day.

Rockets are rated by what they can lift to GTO

Because GTO is the usual drop-off point for geostationary satellites, launch vehicles quote their capacity to it. ISRO's GSLV Mk II can carry 2,250 kg to GTO. The PSLV can carry 1,425 kg to a sub-GTO, a transfer orbit with a lower high point.

See it live

NVS-02's estimated height swings between about 214 km and about 37,251 km every 11 hours — a transfer orbit it never left. Track NVS-02 on its transfer orbit

Key facts

  • GSLV-F12 target GTO: 170 ± 3 km × 36,568 km, inclination 19.36°.
  • NVS-01 lift-off mass: about 2,232 kg.
  • GSLV Mk II capacity: 2,250 kg to GTO; PSLV: 1,425 kg to sub-GTO.
  • NVS-02 remains in a 214 × 37,251 km orbit with a 660-minute period.

Go deeper

The vis-viva equation gives the speed anywhere on an orbit: v² = GM (2/r − 1/a), where a is the semi-major axis.

Worked numbers for the GSLV-F12 target orbit (R = 6,378 km, GM = 398,600 km³/s²):

  • r_p = 6,548 km, r_a = 42,946 km, so a = 24,747 km and e = (r_a − r_p)/(r_a + r_p) = 0.735.
  • Period T = 2π√(a³/GM) = 10.8 h.
  • Speed at perigee: v_p = 10.28 km/s. Speed at apogee: v_a = 1.57 km/s.
  • A circular orbit at the apogee radius needs v_c = √(GM/r_a) = 3.05 km/s.

If the orbit were already in the equator's plane, one burn at apogee would need Δv = 3.05 − 1.57 = 1.48 km/s. But the GTO is tilted 19.36°. A plane change is cheapest where the satellite moves slowest, so it is folded into the apogee burn. By the law of cosines:

Δv = √(v_a² + v_c² − 2·v_a·v_c·cos 19.36°) = 1.68 km/s.

The tilt removal adds only about 0.2 km/s because it is done at apogee. Braeunig notes this is standard practice: a small plane change at perigee, most of it at apogee.

For NVS-02 the same arithmetic gives a = 25,111 km and T = 2π√(a³/GM) = 660 min — exactly the catalogue's period, confirming the satellite is still on its transfer ellipse.

Check yourself

Why do rockets usually release geostationary satellites into a transfer orbit instead of GEO itself?

The rocket reaches the high point only on a stretched ellipse. The satellite's own engine then makes the final burns at apogee to make the orbit circular, which is the standard way to reach GEO.

What went wrong with NVS-02 after launch?

The valves that admit oxidiser to its thrusters did not open, so the planned orbit-raising burn could not be done. The satellite stayed in an elliptical transfer orbit.

Why is the plane change from a tilted GTO to GEO done at apogee?

The satellite moves slowest at apogee, so turning its direction there costs the least change in velocity, and it can be combined with the circularising burn.

Sources

  1. Orbital Mechanics (Rocket and Space Technology) — Robert A. Braeunig
  2. Types of orbits — European Space Agency
  3. GSLV-F12/NVS-01 mission brochure — ISRO
  4. Geosynchronous Satellite Launch Vehicle Mk II — ISRO
  5. Polar Satellite Launch Vehicle — ISRO
  6. SATCAT record: NVS-01 (IRNSS-1J) — CelesTrak
  7. SATCAT record: NVS-02 (IRNSS-1K) — CelesTrak
  8. Earth Fact Sheet — NASA NSSDCA