Satellite constellations — where it appears
Named by 2 essays across one field — each of them below, with the objects they name alongside it.
The shadow that also switches off the satellites
After sunset the sky overhead darkens as the Earth's shadow climbs through the air, and the same shadow, climbing on past the top of the atmosphere, decides which satellites still catch sunlight. For a satellite five hundred and fifty kilometres up the zenith stays lit until the Sun is twenty-three degrees down — five degrees past the end of astronomical twilight — and at the latitudes of most large observatories' summers there is no hour of the night when it is not.
The sunlit area in orbit is almost all in things already tracked
The diffuse glow that objects in orbit add to the night sky depends only on how much sunlit reflecting area there is, and the debris too small to track was thought to be where most of that area might hide. It is not. Whether the smallest pieces hold the area depends on one number — whether the size distribution's slope is steeper or shallower than two — and for the fragments of break-ups it is shallower. The pieces below ten centimetres hold less than one per cent of the cross-section in orbit; the satellites and spent stages, every one of them catalogued, hold the rest.
Named alongside it
The objects these essays reach for when they reach for this one.
Sky brightnessAstronomical twilightAtmospheric dragBreakup modelCross-sectionEarths shadowLatitudeLow earth orbitObserving conditionsOrbital debrisSize distributionSolar depression