Rendezvous and Intercept Targeting
Δv as a function of departure time and flight time, safety constraints, phasing, and correcting Lambert for real dynamics
Gemini 4, June 1965
Jim McDivitt has the spent upper stage of his own Titan rocket a few hundred metres ahead, and the flight plan says to fly formation with it. He does what every pilot's instinct says: points the nose at the target and thrusts towards it.
The target drifts away — upward and ahead. He thrusts again, harder. It recedes further. After using a large share of his manoeuvring propellant the attempt is abandoned.
Nothing was broken. Thrusting forward raised his orbit, and a higher orbit is slower, so he fell behind. Two years earlier an Air Force pilot named Buzz Aldrin had written an MIT doctoral thesis on exactly this — line-of-sight rendezvous guidance — and six months after McDivitt's attempt Gemini 6A and Gemini 7 met in orbit using the method. Orbital rendezvous is not flying towards something. It is solving Lambert's problem.
Watch first · presented by Shoaib Aziz
Intercept versus rendezvous. An intercept only has to arrive at the target's position: one burn, . A rendezvous must also match velocity: a second burn at arrival. Two free choices drive the cost:
- the wait time before the first burn (it sets where both spacecraft are when the transfer starts), and
- the flight time (it sets where the target will be at arrival).
For each pair, propagate both spacecraft, solve Lambert from the chaser's position at to the target's position at , and price the burns. The result is a two-dimensional cost map.
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💡Reading the map
Valleys run diagonally: leaving later and flying shorter can reach the same arrival geometry. They repeat with the synodic period of the two orbits, , because that is how long the relative geometry takes to come back.
Cliffs appear where the transfer angle passes 180° (the plane flips and the cost spikes) and where short flights would need to cut through the planet.
The floor of the best valley sits at the Hohmann transfer when the orbits are circular and coplanar: wait until the target leads by , then fly half the transfer ellipse. Lambert does not know about Hohmann — it simply finds it.
⚠Valid is not the same as flyable
A fast transfer between two nearby points is nearly a straight line, and a straight chord between two points in low orbit passes through the Earth. Every Lambert answer must be checked for perigee on the arc: perigee is passed between departure and arrival exactly when and . If so, require . In the first lab, 12 of 23 intercept times between 300 km and 600 km orbits fail this test — all the fastest ones.
📐Worked Example: 300 km to 600 km
Chaser at 300 km, target at 600 km, coplanar circular orbits, target 30° ahead.
Hohmann. km, m/s, flight time 46.8 min. The target moves during the transfer, so it must lead by at departure. It starts 30° ahead and the chaser gains on it at , so the right moment comes after 95.5 min. The synodic period is 23.7 h: miss it and you wait a day.
Lambert map. A 15 min × 5 min grid finds 181.9 m/s at (wait 90 min, fly 50 min) — a grid point near the floor. Solving Lambert at exactly the Hohmann timing (0.999 of the transfer time, to stay off 180°) returns 167.9 m/s.
Intercept only. The cheapest safe intercept from the starting geometry is 452 m/s with a 70-minute flight; every faster option dives into the atmosphere.
Lambert is a first guess, not an answer. Lambert assumes a point-mass Earth. Fly its velocity with included and the arrival misses — by 64 km after 70 minutes in the third lab. Operational targeting therefore wraps Lambert in a differential corrector: propagate in the full force model, measure the miss , estimate the sensitivity matrix (by finite differences or the state transition matrix), and update .
Newton shooting. Because Lambert's answer is already close, convergence is quadratic: 64 km → 229 m → 3 cm in two corrections, for a velocity change of 4.6 m/s.
🛰How a crew vehicle reaches the ISS
A crew or cargo vehicle is launched into a lower orbit so that it gains on the station from behind. Over the following hours it performs a sequence of phasing and height-adjust burns, each targeted with a Lambert-type solution to an aim point behind or below the station, re-solved after every burn with fresh tracking. For the last few kilometres the dynamics are linearised about the station's orbit — the Clohessy–Wiltshire equations — and the approach is flown along a corridor. Russian vehicles that once took two days now regularly reach the station about three hours after launch, by fitting the whole phasing sequence into two orbits.
💡McDivitt explained
Thrusting toward a target ahead raises your orbit; the higher orbit has a longer period, so you fall behind. To catch something ahead, drop to a lower, faster orbit and let geometry close the gap — or, equivalently, solve Lambert for the arrival point and fly the velocity it gives you, which will usually point somewhere a pilot's instinct would not.
↓But there is a problem
Two free dates, one Lambert solve per pair, a cost at every point. In Earth orbit the map repeats every synodic period of a few hours or a day.
Now change the attracting body to the Sun and the two orbits to Earth's and Mars's. The synodic period becomes 26 months. The map is the same kind of object — but it is the most important chart in planetary exploration, and missions live or die by which part of it their launch date falls in.