☄️Reentry Simulator - Ballistic & Lifting Entry, g-Load, Heat Flux, Corridor
Pick a preset (Apollo lunar return, Soyuz, Space Shuttle, Dragon, Starship, a meteoroid or Curiosity's Mars entry) or set the entry speed, entry angle, ballistic coefficient, lift-to-drag ratio and bank angle yourself. The tool integrates the planar entry equations through a standard atmosphere and plots altitude, speed, deceleration and stagnation heat flux against time. In the animation the path is coloured by heat flux, the vehicle glows with shock-layer plasma and parachutes appear when they open. The corridor tab scans entry angles to find the window between skipping out and exceeding the g-limit, and the heat shield tab sketches how ablation works and roughly sizes the ablator.
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How to use Atmospheric Reentry Simulator
- 1Choose a preset, or adjust entry speed, entry angle, ballistic coefficient, L/D, bank angle and nose radius
- 2Play the animation on Entry trajectory and read the live state, the four time charts and the altitude–speed plot
- 3Check peak deceleration, peak heat flux, total heat load, the blackout window and touchdown speed
- 4Set a g-limit on Entry corridor to see the corridor width, and estimate ablator thickness on Heat shield
FAQ
- What is the entry corridor, and why was Apollo's so tight?
- Enter too shallow and the capsule does not slow enough in the thin upper air; with lift it bounces back into space (skip-out). Enter too steep and it decelerates violently in thick air, exceeding g and heating limits. The range of allowed entry angles between the two is the entry corridor. Returning from the Moon at about 11 km/s, 40% faster than from low orbit, Apollo's corridor was only about 2° wide and needed precise mid-course corrections. The tool runs a full simulation for each entry angle to draw the window.
- What do the ballistic coefficient and L/D do?
- The ballistic coefficient β = m/(C_D·A) is mass per unit of frontal drag area. A low β slows down earlier, higher up in thinner air, so heating and g-loads are lower. Lift (L/D) lets the vehicle hold altitude and stretch out the deceleration: Soyuz pulls about 4 g on a normal entry but 8–9 g when it falls back to a ballistic entry. The bank angle tilts the lift sideways to tune its vertical component, which is the main way to control the landing point and the g-load.
- Why does heat flux go with the cube of speed?
- The Sutton–Graves formula q = k√(ρ/r_n)·V³ describes convective heating at the stagnation point of a blunt body: the kinetic energy flux of the oncoming air scales as ρV³ and part of it reaches the surface through the boundary layer. Heat flux also falls with the square root of the nose radius r_n, which is why capsules are big and blunt: the shock stands farther off and spreads the heating. Going from 7.8 to 11 km/s nearly triples the heat flux.
- How does a heat shield work?
- Most capsules use an ablator. As the surface heats it pyrolyses, chars and is carried away by the flow; the decomposition absorbs heat, the gases injected into the boundary layer block more, and the hot char radiates a lot away. The tool divides the total heat load by an effective heat of ablation to get the ablator mass needed, a rough upper bound that ignores re-radiation; real shields also allow for heat soak and margins. The Space Shuttle used reusable ceramic tiles instead, which insulate and radiate rather than ablate.
- How is Mars entry different?
- Mars' atmosphere is only about 1% as dense as Earth's, so deceleration happens very low, the parachute must open at supersonic speed and the vehicle is still falling at close to 100 m/s under it. That is why Curiosity also needed retro-rockets and a sky crane. Entry speed is about 5.8 km/s, so heating is lower than an Earth return, but the timeline is tight. The Mars atmosphere here is an exponential model with an 11 km scale height, an approximation.
Features
- RK4 integration of the planar point-mass entry equations, ballistic or lifting (L/D plus bank angle)
- 1976 standard atmosphere for Earth (tabulated above 86 km) and an exponential atmosphere for Mars
- Sutton–Graves stagnation heat flux, total heat load and radiative-equilibrium wall temperature
- Multi-stage parachutes (drogue then main, with inflation) and meteoroid ablation mass loss
- Entry corridor scan with skip-out boundary, g-limit boundary and corridor width
- Heat-coloured trajectory animation with plasma glow and a heat shield cross-section sketch