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The science
Single-body entry equations
For a meteoroid of mass m and cross-section A in an exponential atmosphere ρ(h) = ρ0 e-h/H (H = 7.16 km), along a straight path at angle γ: dv/dt = -Cd ρ A v² / (2m) (plus gravity), dm/dt = -Λ ρ A v³ / (2Q), dh/dt = -v sin γ. Light output is taken as 1 % of the kinetic power carried by the ablated mass, ½ v² |dm/dt|.
Closed forms used for the checks
Without ablation, v = v∞ exp(-β e-h/H) with β = Cd ρ0 H A / (2 m sin γ), and the deceleration peaks at v∞ / √e with value v∞² sin γ / (2 e H) at h = H ln(2β). With ablation, dividing the two rate equations gives m = m0 exp(-σ(v∞² - v²)/2) with σ = Λ / (Cd Q).
Honest simplifications: one non-rotating, non-fragmenting body, a flat exponential atmosphere, constant Cd, Λ and 1 % luminous efficiency, no Earth curvature, no shock-heated wake chemistry. Real meteoroids often fragment, so real light curves are more jagged.
What to try
- Sand grain: it burns up high; compare with Large stony, 2 m, which reaches the lower atmosphere.
- Steep and slow vs a shallow angle: where does the deceleration peak move?
- Raise the density: the meteoroid penetrates deeper before it flares.
- Use the slow-motion slider to watch the wake develop.