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Geodetic Precession (Gravity Probe B)

Also known as: de Sitter precession · Geodetic effect

Carry a spinning gyroscope around a massive body and its axis slowly tips — not from any torque, but because the space it moves through is curved. After one orbit the gyroscope points in a slightly new direction. Gravity Probe B measured Earth's geodetic precession at 6.6 arcseconds per year, exactly as general relativity predicts.

Ωgeo=32 GMc2r3 (r⃗×v⃗)\Omega_{\text{geo}} = \frac{3}{2}\,\frac{GM}{c^2 r^3}\,(\vec{r}\times\vec{v})
Live simulation
warming up the physics…

A gyroscope orbits Earth; its spin-axis arrow rotates slightly each lap from parallel transport through curved space, accumulating a visible geodetic precession that grows as the orbit tightens.

Equivalent forms

magnitude
∣Ωgeo∣=32GMc2r ωorb|\Omega_{\text{geo}}| = \frac{3}{2}\frac{GM}{c^2 r}\,\omega_{orb}
gpb value
Ωgeo≈6.6 arcsec/yr (GP-B)\Omega_{\text{geo}} \approx 6.6\ \text{arcsec/yr (GP-B)}
A free gyroscope, touched by nothing, quietly rotates because the geometry it threads is not flat.