Michelson–Morley
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θ = 0°
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Round-trip timesAether mode
magnified view Fringe shift ΔN vs θ
Parallel arm (along the wind)
Perpendicular arm
General arm at angle φ to the wind
Path difference (wavelengths)
Angular dependence (leading order)
Actual experiment (observed)

β ≡ v/c. Earth's orbital β ≈ 9.93×10⁻⁵. ΔN varies as cos 2θ under the classical aether prediction; Actual mode enforces c constant → Δ = 0.