What If the Moon Was 400 km Above Earth? (I Simulated It)
Meridian Lab
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What If the Moon Was 400 km Above Earth? (I Simulated It)
1 просмотр · 4 дн. назад
Meridian Lab
1 просмотр · 4 дн. назад
Put the Moon where the space station flies and it would fill 109 degrees of sky. It would also be torn apart before it finished one orbit. I worked out where the Roche limit is, then simulated a cloud of loose rock to see how much of the Moon survives at different distances.
0:00 The question
0:26 The rules
0:47 What you would see
1:12 The tides
1:48 The tipping point (Roche limit)
2:21 The simulation
2:53 The verdict
3:16 Saturn's rings
3:30 The real Moon is drifting away
3:51 The answer
HOW THIS WAS MADE
Setup: the Moon's surface is 400 km above Earth's surface, so its centre is 8,508 km from Earth's centre. (A Moon centred 400 km up is impossible: it would sit inside the Earth.)
Sky size: angular radius = asin(Moon radius / distance from the observer) = 54.4 degrees, so about 109 degrees across and about 42% of the visible sky.
Orbit: circular, tidally locked. Period 129 minutes, speed 6.8 km/s.
Tides: stretching acceleration at the surface = 2 G M_Earth R_Moon / d^3. At 8,508 km it is 2.25 m/s2, against the Moon's own surface gravity of 1.62 m/s2. At the real distance it is about 1/66,000 of surface gravity. The ratio of tidal strength at 8,508 km versus 384,400 km is about 92,000.
Roche limit for loose rock: where stretch equals surface gravity, 9,490 km from the centre (about 3,000 km above the ground). The flowing-liquid limit is quoted at about 18,400 km (rigid and fluid Roche limits, e.g. the standard 2.44 R (rho_planet / rho_moon)^(1/3) form).
Simulation: 1,257 test particles on the Moon's disc, 2-D, tidally locked start, Earth and Moon gravity, RK4 integration for two orbits at 20,000, 15,000, 12,000 and 8,508 km. Percent shown is the share within 3 Moon radii of the Moon's centre at the end. At 8,508 km about 48% of particles dip inside Earth's radius and the rest go to wide orbits. It is a toy model: no collisions, no rock strength, no 3-D.
Recession: about 3.8 cm per year, measured by lunar laser ranging off the retroreflectors left by the Apollo missions.
Edouard Roche (1820-1883), French astronomer, worked out the limit in the 1840s-1850s.
Every visual is drawn in code. The Moon and Earth textures are generated, not photographs. No stock footage and no AI-generated video.
Narration is a synthetic voice (ElevenLabs).
Meridian Lab asks one question per video and answers it by running the numbers.