7.6726
7.9168
10.8507
0.031
11,850
7.6726
7.9168
10.8507
0.031
11,850
The Re-entry Speed Calculator computes the speed of a spacecraft or meteoroid when it reaches the top of the atmosphere from orbit, and estimates the peak stagnation temperature — the heating experienced at the leading edge of the vehicle. Re-entry heating is one of the most extreme engineering environments humans have ever designed for, and calculating entry speed is the first step in designing a thermal protection system.
When a spacecraft de-orbits from circular orbit, it performs a retrograde burn to lower its perigee into the upper atmosphere. As the perigee drops to the atmospheric interface (typically 122 km for Earth, where the atmosphere becomes significant), the spacecraft is moving at a speed determined by the vis-viva equation for the transfer orbit. For LEO reentry, this speed is approximately 7.9 km/s — about 23 times the speed of sound at sea level.
The stagnation temperature at the leading edge of a blunt body is estimated using aerothermodynamic theory. All of the kinetic energy of the incoming flow is converted to thermal energy at the stagnation point. The temperature scales roughly as the square of the entry velocity: T_stagnation approximately proportional to v^2. At LEO reentry speeds of 7.9 km/s, peak stagnation temperatures reach 10,000-15,000 K (hotter than the Sun's surface!). At Mars-return entry speeds (12 km/s), temperatures approach 20,000 K or more.
These extreme temperatures require advanced thermal protection systems (TPS). The Space Shuttle used reinforced carbon-carbon tiles for the hottest areas and silica foam tiles elsewhere. SpaceX Dragon uses PICA-X (phenolic impregnated carbon ablator). Ablative TPS materials absorb heat by vaporizing, carrying heat away from the vehicle. The Apollo capsule's TPS survived reentry at 11 km/s on return from the Moon.
Orbital speed at altitude = sqrt(GM/r). Entry speed uses vis-viva for the transfer orbit connecting orbit altitude to entry interface altitude: v_entry = sqrt(GM*(2/r_entry - 2/(r_orbit+r_entry))). Escape speed = sqrt(2*GM/r_orbit). Specific kinetic energy = 0.5*v_entry^2 in MJ/kg. Stagnation temperature estimate: T ≈ 11800*(v/v_LEO)^2 K (rough empirical scaling from LEO baseline of 11800 K at 7.9 km/s).
LEO reentry (7.9 km/s): peak stagnation ~11,800 K — tiles on Shuttle reached 1500 C surface temperature. Moon return (11 km/s): ~23,000 K (Apollo ablator). Mars return (~12 km/s): ~27,000 K. Jupiter probe (47 km/s): ~300,000 K (Galileo probe, which survived only 57 minutes). Stagnation temperature is theoretical maximum; actual surface temperature depends on heat conduction, ablation, and radiation cooling.
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Dragon enters at about 7.85 km/s. The 30.8 MJ/kg of kinetic energy must be dissipated by the heat shield; the theoretical stagnation temperature reaches nearly 12,000 K.
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Returning from the Moon at 400,000 km altitude, the Apollo capsule hits the atmosphere at 11 km/s — nearly twice the kinetic energy of LEO reentry. This demanded the heavy ablative heat shield.
Atmospheric reentry is the process by which a spacecraft, meteoroid, or re-entry vehicle enters (or re-enters) a planet's atmosphere from space. The dramatic heating and deceleration occur as kinetic energy is converted to heat through compression of the atmosphere ahead of the vehicle (not primarily friction, as commonly believed). Successful reentry requires a thermal protection system to survive the heating.
A spacecraft at orbital velocity has enormous kinetic energy (about 30 MJ/kg for LEO). This must be dissipated in minutes as the spacecraft decelerates to subsonic speed. The compressed air ahead of the blunt body forms a shock wave. Air in the shock layer is heated to plasma temperatures. The vehicle radiates, ablates, or conducts away this heat through its thermal protection system.
A common misconception: reentry heat is primarily from compression of the atmosphere (a shock wave), not surface friction. The shock wave ahead of the vehicle compresses air to extremely high temperatures and pressures. Less than 1% of heating comes from actual surface friction. This is why blunt bodies (Apollo, SpaceX Dragon) are more efficient for reentry than sharp bodies — they push the shock wave away from the vehicle surface.
Ablative TPS materials protect a vehicle by pyrolysis (charring) and vaporization. As the surface heats up, the ablator material chars and vaporizes, carrying heat away from the vehicle. The char layer insulates the underlying structure. Ablative TPS was used on Mercury, Gemini, Apollo, and is used on SpaceX Dragon (PICA-X), Mars Science Laboratory, and other missions requiring deep/high-speed entry.
The Shuttle used four types: Reinforced Carbon-Carbon (RCC) for the nose and wing leading edges (hottest areas, up to 1650 C); High-temperature Reusable Surface Insulation (HRSI, black tiles) for lower surfaces; Low-temperature RSSI (white tiles) for upper surfaces; and flexible Nomex blankets for lower-heat areas. The Columbia accident (2003) was caused by foam damage to the RCC wing leading edge.
A skip reentry (bouncing reentry) occurs when a spacecraft enters the atmosphere at a shallow angle, decelerates partially in the upper atmosphere, then exits back into space briefly before final reentry. It spreads the heating over a longer period and allows precise landing site targeting. The Apollo command module used a form of skip reentry (lifting reentry) to control landing point.
The entry corridor is the range of flight path angles that leads to successful reentry. Too shallow (less negative): the vehicle bounces off the atmosphere without decelerating enough. Too steep (more negative): the vehicle experiences excessive deceleration g-loads and heating. For crewed Apollo reentries, the corridor was only about 2 degrees wide (between -5.5 and -7.5 degrees below local horizontal).
Ballistic coefficient BC = m/(C_D * A), where m is mass, C_D is drag coefficient, and A is cross-sectional area. Higher BC means the vehicle penetrates deeper into the atmosphere before decelerating significantly — it reaches lower altitudes at higher speed, experiencing more concentrated heating. A low BC (large area, low mass) decelerates high in the atmosphere, spreading heating over a longer time and lower temperatures.
Mars has a thin atmosphere (about 1% of Earth's surface pressure) but reentry still occurs because the entry speeds are high (4-7 km/s from orbit, 5.5 km/s from direct entry). The thin atmosphere makes it harder to decelerate: vehicles must use large aeroshells (high drag) and sometimes supersonic parachutes and retro rockets. The Mars Science Laboratory used a 4.5 m diameter aeroshell and a sky crane system for the 1-tonne Curiosity rover.
Peak heating rate (W/cm^2) is the maximum instantaneous heat flux at the vehicle nose. Total heat load (J/cm^2) is the total energy per unit area deposited during the entire entry. A steep, fast entry has high peak heating rate but short duration (low total load). A shallow entry has lower peak rate but longer duration. Both must be managed: peak rate determines material temperature survival, total load determines ablator thickness needed.
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