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Jupiter is more than 11 times wider and 318 times more massive than Earth, yet it takes only 9 hours and 55 minutes to complete one full rotation. At its equator, the cloud layer moves at a velocity of approximately 45,000 km/h—about 27 times faster than Earth's equatorial rotational speed. No other planet in the Solar System rotates faster.
Three combined factors result in this figure.
Conservation of angular momentum
Jupiter formed earliest and swept up the majority of the remaining gas and dust in the Solar disk, accumulating 2.5 times more mass than all other planets combined. The material fell in from a vast area of the disk, carrying with it the angular momentum of that entire region.
As this mass of material contracted into a sphere many times smaller, angular momentum had to be conserved, causing the rotational speed to skyrocket—much like an ice skater pulling their arms in close to their body to spin faster.
Runaway accretion
According to the model by Pollack et al. (1996), when the gas mass in the envelope catches up to the solid core mass, the planet enters a phase of runaway gas accretion: the hydrogen and helium surrounding it no longer fall in gradually but pour down rapidly. This mass of gas originates from the disk orbiting Jupiter, so it carries the disk's angular momentum in addition to its own mass.
No solid surface to provide braking
Earth is slowing down. Tides generated by the Moon drag against the ocean floor and the solid crust; measured from eclipse records over 2,700 years, the day length increases by an average of about 1.8 milliseconds per century.
On Jupiter, this mechanism is almost non-existent. It lacks a solid surface and no water oceans press against a rocky bottom. Tidal braking caused by satellites does occur—tidal dissipation in Jupiter has been measured—but the amount of angular momentum removed is negligible compared to the planet's massive rotational angular momentum.
The consequence is immediately visible in photographs: it rotates so fast that centrifugal force causes Jupiter to bulge at the equator and flatten at the poles. The equatorial radius is about 4,600 km larger than the polar radius—an oblateness of about 6.5%.
The invisible brake
If the accretion process only injected angular momentum without any removal mechanism, the rotational speed would increase until the equatorial centrifugal force exceeded gravity, and the planet could no longer hold itself together. The mechanism believed to have reined in this rotation is called magnetic braking—the same mechanism astronomers use to explain why young stars do not rotate infinitely fast.
It operates in three steps:
The ionized gas disk. The young planet radiates heat intensely, sufficient to warm the inner parts of the surrounding gas disk until elements that easily lose electrons begin to ionize. The disk transitions into a plasma state—consisting of ions and free electrons, making it electrically conductive.
Magnetic fields grip the plasma. This same heat source fuels a dynamo within the young planet, generating a strong magnetic field—the predecessor of today's Jovian magnetic field, maintained by liquid metallic hydrogen currents and the strongest among the planets of the Solar System. The magnetic field lines reach out into space, and because conductive plasma cannot freely cut across field lines, they grip the surrounding gas disk like invisible spokes.
Angular momentum is pulled outward. The magnetic field lines rotate with the planet, while the distant plasma rotates more slowly. This velocity differential bends the field lines and generates a drag force against the rotation: the movement of charged plasma through the magnetic field generates induced currents, and these induced currents produce a force that opposes the very motion that created them. The result is that angular momentum is transferred from the planet to the outer gas disk, then escapes the planet's sphere of influence with the gas flow, causing the planet to slow down—much like dropping a spinning magnet into a conductive fluid.
It should be made clear: the detailed sequence of this process in Jupiter remains a theoretical model, reconstructed from observations of young stars and accretion disks. No one witnessed that stage, and the specific figures are still being debated.
References
- [1]On the Terminal Rotation Rates of Giant Planets — The Astronomical Journal (2018)
- [2]Age of Jupiter inferred from the distinct genetics and formation times of meteorites — Proceedings of the National Academy of Sciences (2017)
- [3]Measurement of the Earth's rotation: 720 BC to AD 2015 — Proceedings of the Royal Society A (2016)
- [4]Strong tidal dissipation in Io and Jupiter from astrometric observations — Nature (2009)
- [5]Formation of the Giant Planets by Concurrent Accretion of Solids and Gas — Icarus (1996)
- [6]Juno Mission — NASA (2024)
- [7]Jupiter Fact Sheet — NASA NSSDC (2024)
Image: NASA/JPL-Caltech/SwRI/MSSS/Betsy Asher Hall/Gervasio Robles — Wikimedia Commons, xem trang gốc.
