Earth’s inner core may have stopped spinning – but what does that mean?

With thousands of miles of rock in the way, it’s hard to get a good look at exactly what’s going on in the center of the Earth. Scientists have to study it indirectly by measuring magnetic field changes, ancient crystals, or how seismic waves from earthquakes propagate through different layers. This has helped geologists learn new details, including that the core could be made of a superionic iron alloy.

Now a new study has reached a surprising conclusion – that relative to Earth’s surface, the inner core stopped spinning around 2009. This could be possible because the inner core is a more or less solid ball of iron floating in a liquid outer core, so its rotation is not necessarily tied to that of the rest of the planet.

The researchers, from Peking University, analyzed the seismic waves from earthquakes passing through the inner core since the 1960s, investigating the differences in how those waves looked and how long it took them to propagate. Intriguingly, they found that for decades the travel times of these waves would vary in specific ways – but after about 2009, that variation all but vanished. Travel times have remained steady, which the team says is an indication that the core’s rotation has “paused.”

That doesn’t mean that it’s not spinning at all – it means that the core’s rotation is now essentially in lockstep with the rotation at the surface. At different times the core can race around or lag behind the surface, but even then the difference is tiny. It can, however, add up over time, so that the core is drifting by dozens of kilometers per year.

The team goes a step further and says that the study could indicate that the core may now be rotating in the opposite direction. But again, that doesn’t quite mean what it sounds like – instead, the core’s slowing rotation makes it appear to be drifting backwards relative to the surface.

The cause of this cycle could be several major competing forces. The magnetic field generated by the outer core could be speeding up the inner core’s spin, while the huge gravitational influence of the mantle could drag on it and slow its spin.

Of course, in the murky world of inner Earth geology, nothing is set in stone (pun intended), and other scientists disagree with the findings of the new study.

“These mathematical models are most likely all incorrect because they explain the observed data but are not required by the data,” Hrvoje Tkalcic, a geophysicist at the Australian National University, told AFP. “Therefore, the geophysical community will be divided about this finding and the topic will remain controversial.”

The new study was published in the journal Nature Geoscience.

Source: Nature
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