Sidereal Orbital Period of the Moon
| Value | 2,360,594.88 s |
| Status | Conventional / typical value |
| Source | NASA NSSDC Planetary Fact Sheet, Moon (sidereal orbit period) |
| Categories | Astronomicalsolar-systemmoon |
| Planck time | 4.3785693e+49 tP |
| attosecond | 2.3605949e+24 as |
| femtosecond | 2.3605949e+21 fs |
| picosecond | 2.3605949e+18 ps |
| nanosecond | 2.3605949e+15 ns |
| shake | 236,059,490,000,000 shake |
| microsecond | 2,360,594,900,000 μs |
| millisecond | 2,360,594,900 ms |
| second | 2,360,594.9 s |
| minute | 39,343.248 min |
| hour | 655.7208 h |
| sidereal day | 27.396504 sd |
| day | 27.3217 d |
| week | 3.9031 wk |
| fortnight | 1.95155 fn |
| month | 0.89765129 mo |
| year | 0.074802738 yr |
| decade | 0.0074802738 dec |
| century | 0.00074802738 cent |
| millennium | 0.000074802738 mil |
| megayear | 7.4802738e-08 Myr |
| eon | 7.4802738e-11 eon |
Learning zone
The Moon circles Earth in 27.32 days measured against the stars, yet the familiar cycle of phases takes 29.53 — the synodic month — because while the Moon orbits, Earth carries it a twelfth of the way around the Sun, and the Moon needs two extra days to catch up to the moving line between the two. Calendars follow the phases; dynamics follows the sidereal value, which is the number Kepler's third law wants.
The same 27.3217 days is also the Moon's rotation period, and that is no coincidence: tidal friction long ago braked the spin into synchronous lock, so one hemisphere faces Earth forever. Newton used this orbit for the first great test of universal gravitation — the Moon falls toward Earth 3600 times more weakly than an apple does, at sixty times the distance, exactly as an inverse-square law demands. And the period is slowly lengthening as the Moon spirals outward by 3.8 cm a year, angular momentum handed over from Earth's slowing spin.