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Found primary source plus pages of other space agencies for max apogee of Geotail (previous edit relied on Wikipedia.) The Japanese JAXA/ISAS page actually seemed to contradict itself as to whether 210 or 220 Re was the maximum; edited to reflect that. (nb I think 220 is more likely but am not sure)

I found the following "far out" spacecraft:

  • TESS (Transiting Exoplanet Survey Satellite) recently launched, not in final orbit yet
  • Spektr-R
  • IBEX or Interstellar Boundary Explorer
  • Geotail

Here are their IDs:

TESS       43435    2018-038A
Spektr-R   37755    2011-037A
IBEX       33401    2008-051A
Geotail    22049    1992-044A

I downloaded both TLEs and orbit data from JPL Horizons in order to piece together this qualitative data.

The problem is that for such high orbits, the gravity of the Sun and the Moon can push them around significantly so their orbits change over time, sometimes by quite a bit!

The all-time winner (of the four that I found) seems to be Geotail. Using historical TLEs shows Geotail's maximum semi-major axis of about 280,000 km or about 44 Earth radii, and a maximum apoapsis of over 500,000 km or about 81 Earth radii. However, according to the Japanese space agency's website (see also Wikipedia), the orbit is designed to cover the magnetotail over a wide range of distances: 8 Re to 210 Re from the earth. This is over 1,300,000 km from the Earth! In fact, some sections of that site and those of NASA/ESA suggest the maximum apogee may have been an even higher 220 Re, over 1,400,000 km distant!

This would not likely have been long term stable, and so after sampling the tail of the magnetosphere out there it was ramped down closer to Earth.

I have two plots for TESS, both current data from TLEs and future data (the big DOT) after it will use a close swing-by maneuver with the Moon and then another propulsive maneuver in order to reach its half lunar month orbit. Once that happens, TESS will be the longest period artificial satellite around the Earth, at least one with a fairly stable orbit and whose information is available publicly.

TESS has this orbit in order to spend most of its time staring at nearby stars looking for exoplanets, then it makes a close pass by Earth to download data, once every two weeks.

You can read more about how TESS' orbit works in this answer to the question TESS orbit and moon resonance.

I've put a plot of TESS' calculated orbit from Horizons below. The green, tightly repeating orbit is the Moon's. The red orbit, inclined, evolving, changing orbit is for TESS only for a few years currently in the Horizon's simulation. It's almost a miracle that it can remain so close to its orbit. Well, it's "just F=ma" (roughly), but it's still beautiful!

TESS might represent the highest non-Lagrangian Geocentric orbit that is stable over decades. It was carefully designed to have half the period of the Moon in order to cancel out perturbing effects. It is called a 2:1 resonant orbit. For orbits higher than that, lunar perturbations may become problematic.

Earth-Moon Lagrange orbits are Geocentric orbits that are in 1:1 resonance with the Moon (they are not lunar orbits). They will have their own stability issues and require station keeping. A particularly stable Geocentric orbit which is associated with the Earth-Moon Lagrange points is the Near Rectilinear Halo Orbit. Read more about it in the questions and their answers:

The Halo orbit associated with the Earth-Moon Lagrange L1 and L2 points are probably the highest Geocentric orbits that are also usefully stable. Instead of being perturbed by the Moon's gravity, they remain in resonance with it and use it to provide additional stability. However, they still require station keeping.

enter image description here

below: I've put a plot of TESS' calculated orbit from Horizons below. The green, tightly repeating orbit is the Moon's. The red orbit, inclined, evolving, changing orbit is for TESS only for a few years currently in the Horizon's simulation.

TESS' orbit from Horizons

uhoh
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