Sidereal Rotation Period of Uranus
| Value | 62,064 s |
| Status | Conventional / typical value |
| Source | NASA NSSDC Planetary Fact Sheet, Uranus (sidereal rotation period, −17.24 h; magnetic field, Voyager 2) |
| Categories | Astronomicalsolar-systemplanets |
| Planck time | 1.1511993e+48 tP |
| attosecond | 6.2064000e+22 as |
| femtosecond | 6.2064000e+19 fs |
| picosecond | 6.2064000e+16 ps |
| nanosecond | 62,064,000,000,000 ns |
| shake | 6,206,400,000,000 shake |
| microsecond | 62,064,000,000 μs |
| millisecond | 62,064,000 ms |
| second | 62,064 s |
| minute | 1,034.4 min |
| hour | 17.24 h |
| sidereal day | 0.72030007 sd |
| day | 0.71833333 d |
| week | 0.10261905 wk |
| fortnight | 0.051309524 fn |
| month | 0.023600758 mo |
| year | 0.0019666895 yr |
| decade | 0.00019666895 dec |
| century | 0.000019666895 cent |
| millennium | 0.0000019666895 mil |
| megayear | 1.9666895e-09 Myr |
| eon | 1.9666895e-12 eon |
Learning zone
Uranus's clouds are so bland that no telescope could ever clock the rotation; the 17.24-hour figure comes from Voyager 2's nine days of listening to radio bursts tied to the magnetic field, and it has never been checked by a second spacecraft. Formally the NSSDC lists it as −17.24 h: with the spin axis tipped 98°, past the perpendicular, the rotation is technically retrograde — a bookkeeping consequence of the tilt rather than a separate oddity.
The field doing the broadcasting turned out to be its own surprise: offset from the planet's centre by a third of the radius and inclined 59° to the spin axis, a lopsided magnet whose origin is still debated — possibly generated in a thin shell of ionic water rather than a deep core. Because the field is the only handle on the interior's rotation, the 17.24-hour day inherits every uncertainty about the field itself; models of the interior treat its last digits gently.