Jupiter cut open: The magnetic field lines illustrate the high complexity of the magnetic field inside the planet, which, however, quickly decreases beyond the metallic layer (black line).
On the surface, a dipolar part that is inclined by ten degrees with respect to the axis of rotation dominates.
The thickness of the field lines is a measure of the local magnetic field strength.
In the equatorial region, a jet produces bundles of field lines with a pronounced east-west orientation at the transition to the metallic layer.
The coloured contours represent the radial surface field. Red indicates field lines directed outwards, blue inwards; green denotes a weak field.
The colour coding of the sections represents the field in the east-west direction – red indicates eastwards, blue westwards.
Credit: J. Wicht, MPS
Superlatives are the trademark of the
planet Jupiter.
The magnetic field at the top edge of the cloud surrounding the largest member of the solar system is around ten times stronger than Earth's, and is by far the largest magnetosphere around a planet.
Just why this field has a similar structure to that of our own planet although the interiors of the two celestial objects have a completely different structure, has mystified researchers for a long time.
With the aid of the most detailed computer simulations to date, a team headed by the
Max Planck Institute for Solar System Research in Göttingen has now succeeded in explaining the origin of the magnetic field deep inside the gaseous giant.
Magnetic fields are always generated when electric currents flow. The Earth is surrounded by a magnetic field because, deep in its interior, there is a circulating molten mass of iron and nickel.
This motion gives rise to electric currents that generate Earth's familiar
dipolar magnetic field, in much the same way as a bicycle dynamo operates. Physicists call it the geo-dynamo, but how does the dynamo inside of Jupiter work?
Jupiter consists predominantly of hydrogen and helium.
Photos of the planet show coloured bands of cloud and gigantic tornados such as the
Great Red Spot.
The temperature at the upper cloud boundary is minus 100 degrees Celsius, but temperature, pressure and electrical conductivity increase enormously with increasing depth.
At a depth of just under 10,000 kilometres and a pressure of several million atmospheres, the hydrogen even becomes conductive like a metal, an exotic state of matter which does not exist on Earth.
It is still unclear whether there is a rocky core at the centre of the planet; it could possibly amount to around 20 percent of the Jupiter radius, corresponding to 14,000 kilometres.
Previous computer simulations on the formation of the magnetic field had to greatly simplify this complex structure.
The upper gaseous region and the lower metallic region were treated separately, for example.
Thus, no computation correctly reproduced the strength and the form of the magnetic field as determined by space probes.
"Several colleagues assumed that certain physical quantities changed suddenly at the transition to the region of the metal-like conducting hydrogen," says project leader
Johannes Wicht from the
Max Planck Institute for Solar System Research in Göttingen, but new models from colleagues at the
University of Rostock seem to prove that this is probably not the case.
The properties change gradually over the whole gas layer so that the separate treatment of the outer and inner region is hardly justified.
The important step forward here was the fact that, for the first time, the Göttingen-based physicists dealt with all regions of the planet in the same simulation.
To this effect, the
Max Planck Society's huge Hydra supercomputer in Garching had to spend around six months on the computation.
The result was impressive: it portrayed Jupiter's magnetic field more or less as space probes had determined it in nature.
"The main part of the magnetic field, which looks so similar to Earth's magnetic field, is generated deep inside the planet, where the properties no longer change so strongly," says Wicht.
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