Science
- Earth's magnetic north pole keeps moving.
- In the last few years, it has moved so much that the National Oceanic and Atmospheric Administration issued an early update to its World Magnetic Model (WMM), which informs everything from GPS apps to the US Department of Defense's navigation systems.
- Scientists aren't certain why the planet's magnetic field - which protects us from deadly solar winds - keeps shifting, but one theory is that geomagnetic pulses in the planet's core throw the field into whack.
- In a new study, researchers modeled the source and timing of those sudden geomagnetic jerks.
- Visit Business Insider's homepage for more stories.
In the Hollywood blockbuster "The Core," the planet's core suddenly stops rotating, which causes Earth's magnetic field to collapse. Then bursts of deadly microwaves cook the Colosseum and melt the Golden Gate Bridge.
While "nearly everything in the movie is wrong," according to seismologist Justin Revenaugh from the University of Minnesota, it is true that Earth's magnetic field shields the planet from deadly and destructive solar radiation. Without it, solar winds could strip Earth of its oceans and atmosphere.
But the planet's magnetic field isn't static.
The Earth's north magnetic pole (which is not the same as geographic north) has led scientists on something of a goose chase over the last century. Each year, it moves north by an average of about 30 miles.
Wikimedia Commons The Magnetic North Pole has shifted north since the 1900s.
That movement made the World Magnetic Model (WMM) - which tracks the field and informs compasses, GPS on smartphones, and navigation systems on planes and ships - inaccurate. Since the next planned update of the WMM wasn't slated to happen until 2020, the US military requested an unprecedented early update to account for magnetic north's accelerated gambol.
Now authors of a new study have gained insight into why magnetic north might be moving, and learning how to predict these shifts.
Tracking movement in the Earth's core
Earth's magnetic field exists thanks to swirling liquid nickel and iron in the planet's outer core some 1,800 miles beneath the surface. Anchored by the north and south magnetic poles (which tend to shift around and even reverse every million years or so), the field waxes and wanes in strength, undulating based on what's going on in the core.
Periodic and sometimes random changes in the distribution of that turbulent liquid metal can cause idiosyncrasies in the magnetic field. If you imagine the magnetic field as a series of rubber bands that thread through the magnetic poles and the Earth's core, then changes in the core essentially tug on different rubber bands in various places.
Those geomagnetic tugs then influence the north magnetic pole's migration and can even cause it to veer wildly from its current position.
Read More: Earth's north magnetic pole has moved - here's what that means for our navigation systems
Aubert et al./IPGP/CNRS Photo library
A visualization of the interior of the Earth's core, as represented by a computer simulation.
So far, predicting these magnetic-field shifts has been a challenge. But in the new study, geophysicists Julien Aubert and Christopher Finlay attempted to simulate the physical conditions of Earth's core by having supercomputers crunch 4 million hours' worth of calculations.
The researchers knew that the movement of heat from the planet's interior outward can influence the magnetic field. In general, this happens at speed of 6 miles per year. But their results revealed that sometimes, there are pockets of liquid iron in the core that happen to be much warmer and lighter than the surrounding fluid. If the difference between these hot, less dense bits of fluid and their colder, denser counterparts is great enough, the warm liquid can rise very quickly.
That rapid motion then triggers magnetic waves that careen towards the core's surface, causing geomagnetic jerks.
"Think about these waves like vibrating strings of a musical instrument," Aubert told Business Insider.
Magnetic north is important for navigational models
Keeping tabs on magnetic north is imperative for European and American militaries because their navigation systems rely the WMM. Commercial airlines and smartphone GPS apps also rely on the model to help pilots and users pinpoint their locations and navigate accordingly.
That's why the British Geological Survey and the National Oceanic and Atmospheric Administration (NOAA) update the WMM every five years. The early update requested by the US military was completed February 4.
But even with these periodic updates, geomagnetic jerks make it tough to keep the model accurate, Aubert said.
Justin Sullivan/Getty Images Magnetic north is important for smartphone GPS apps.
His group's new model could address that problem by helping to predict how Earth's magnetic field might evolve.
"Within the next few years, we envision that it should indeed be possible for our groups [...] to capture past jerks and predict the future ones with improved accuracy," Aubert said.
Could the magnetic field ever collapse?
Earth's magnetic field shields its atmosphere, which does "a bulk of the work" of keeping out solar radiation, as Revenaugh put it. If we lost our magnetic field, we'd eventually lose our atmosphere.
But according to Revenaugh, that's extremely unlikely to happen, since the Earth's core would never stop rotating.
Even if the field did collapse, the devastating effects depicted in "The Core" (people with pacemakers dropping dead, out-of-control lightning storms, eviscerated national landmarks) wouldn't follow.
NASA
Without its atmosphere and magnetic field, Earth would constantly be bombarded by cosmic radiation.
A far more likely scenario, Revenaugh suggested, would involve the magnetic poles reversing like they did 780,000 years ago. When such reversals happen (there have been several in Earth's history), the magnetic field drops to about 30% of its full strength, he said.
Though that's a far-away scenario, Revenaugh added that it's still important to improve scientists' understanding of the magnetic field today.
"The better we can model it, the better we can understand what's it's up to," he said.