SSA-01 Module 2 gave orbital mechanics and the space environment a first pass — enough to place LEO, MEO, and GEO on a map and know why "zero gravity" is a myth. This module goes further: the actual laws governing orbits, how you move between them, and how the environment forces specific engineering decisions rather than just being hostile in general.
Johannes Kepler worked these out from planetary observation data decades before Newton explained why they're true. They apply just as well to a satellite orbiting Earth as to a planet orbiting the Sun.
Not circles. Every orbit is an ellipse with the central body (Earth, the Sun) at one focus, not the center. A circular orbit is just the special case where both foci coincide.
A line from the central body to the orbiting object sweeps out equal areas in equal time — which means an object moves fastest at its closest approach and slowest at its farthest point.
The square of an orbital period is proportional to the cube of the orbit's size (T² ∝ a³). This is exactly why GEO sits at one specific altitude — it's the only altitude where the math works out to a 24-hour period.
Real orbital mechanics uses six elements. These three carry most of the practical meaning.
Half the "long axis" of the orbital ellipse — effectively the orbit's overall size. Per Kepler's third law, this single number determines the orbital period.
How stretched the ellipse is, from 0 (a perfect circle) toward 1 (increasingly elongated). Most operational satellites use low-eccentricity, near-circular orbits; some science and communications missions deliberately use highly eccentric ones.
The tilt of the orbital plane relative to Earth's equator. A 0° orbit stays directly over the equator; a 90° polar orbit crosses over both poles on every revolution.
Moving from one circular orbit to another isn't a straight shot — it's the most fuel-efficient two-burn maneuver between them, named for Walter Hohmann, who worked it out mathematically in 1925.
Illustrative — not to scale. Real burn sizes and transfer times depend on the specific altitudes involved.
SSA-01 Module 2 named vacuum, radiation, and thermal extremes as threats. Here's specifically what engineers do about each one.
Ordinary materials outgas — slowly releasing trapped gases and vapors — in vacuum, which can fog optics and contaminate sensitive surfaces. Spacecraft use low-outgassing, vacuum-rated materials specifically to avoid this.
Radiation can flip bits in electronics or degrade solar cells over time. Spacecraft use radiation-hardened components, shielding around the most sensitive electronics, and redundant systems that can outvote a single corrupted result.
Multi-layer insulation (MLI) blankets — the gold or silver foil visible on most spacecraft — passively reflect radiant heat, while radiators and heaters actively manage the swing between sunlit and shadowed sides.
Tiny natural particles and human-made debris both travel fast enough to punch through a thin hull. Whipple shielding — a sacrificial outer layer set slightly away from the main hull — breaks up an impactor before it can reach anything critical.
NASA Glenn Research Center orbital mechanics and Hohmann transfer primers, NASA/ESA spacecraft materials and outgassing guidelines, and NASA orbital debris and micrometeoroid shielding technical documentation.
Module 4 covers applied satellite systems — navigation, meteorology, and telecommunications, end to end.