Earth’s magnetic field is acting up and geologists don’t know why
Something
strange is going on at the top of the world. Earth’s north magnetic
pole has been skittering away from Canada and towards Siberia, driven by
liquid iron sloshing within the planet’s core. The magnetic pole is
moving so quickly that it has forced the world’s geomagnetism experts
into a rare move. On 15 January, they are set to update the World Magnetic Model, which describes the planet’s magnetic field and underlies all modern navigation, from the systems that steer ships at sea to Google Maps on smartphones. The
most recent version of the model came out in 2015 and was supposed to
last until 2020 — but the magnetic field is changing so rapidly that
researchers have to fix the model now. “The error is increasing all the
time,” says Arnaud Chulliat, a geomagnetist at the University of
Colorado Boulder and the National Oceanic and Atmospheric
Administration’s (NOAA’s) National Centers for Environmental
Information. The problem lies partly with the moving pole and
partly with other shifts deep within the planet. Liquid churning in
Earth’s core generates most of the magnetic field, which varies over
time as the deep flows change. In 2016, for instance, part of the
magnetic field temporarily accelerated deep under northern South America
and the eastern Pacific Ocean. Satellites such as the European Space
Agency’s Swarm mission tracked the shift. By early 2018, the World
Magnetic Model was in trouble. Researchers from NOAA and the British
Geological Survey in Edinburgh had been doing their annual check of how
well the model was capturing all the variations in Earth’s magnetic
field. They realized that it was so inaccurate that it was about to
exceed the acceptable limit for navigational errors.
Wandering pole
“That
was an interesting situation we found ourselves in,” says Chulliat.
“What’s happening?” The answer is twofold, he reported last month at a
meeting of the American Geophysical Union in Washington DC. First,
that 2016 geomagnetic pulse beneath South America came at the worst
possible time, just after the 2015 update to the World Magnetic Model.
This meant that the magnetic field had lurched just after the latest
update, in ways that planners had not anticipated.
Source: World Data Center for Geomagnetism/Kyoto Univ.
Second, the motion of the north magnetic pole made the
problem worse. The pole wanders in unpredictable ways that have
fascinated explorers and scientists since James Clark Ross first
measured it in 1831 in the Canadian Arctic. In the mid-1990s it picked
up speed, from around 15 kilometres per year to around 55 kilometres per
year. By 2001, it had entered the Arctic Ocean — where, in 2007, a team
including Chulliat landed an aeroplane on the sea ice in an attempt to
locate the pole. In 2018, the pole crossed the International Date Line into the Eastern Hemisphere. It is currently making a beeline for Siberia. The
geometry of Earth’s magnetic field magnifies the model’s errors in
places where the field is changing quickly, such as the North Pole. “The
fact that the pole is going fast makes this region more prone to large
errors,” says Chulliat. To fix the World Magnetic Model, he and
his colleagues fed it three years of recent data, which included the
2016 geomagnetic pulse. The new version should remain accurate, he says,
until the next regularly scheduled update in 2020.
Core questions
In
the meantime, scientists are working to understand why the magnetic
field is changing so dramatically. Geomagnetic pulses, like the one that
happened in 2016, might be traced back to ‘hydromagnetic’ waves arising
from deep in the core1. And the fast motion of the north magnetic pole could be linked to a high-speed jet of liquid iron beneath Canada2. The
jet seems to be smearing out and weakening the magnetic field beneath
Canada, Phil Livermore, a geomagnetist at the University of Leeds, UK,
said at the American Geophysical Union meeting. And that means that
Canada is essentially losing a magnetic tug-of-war with Siberia. “The
location of the north magnetic pole appears to be governed by two
large-scale patches of magnetic field, one beneath Canada and one
beneath Siberia,” Livermore says. “The Siberian patch is winning the
competition.” Which means that the world’s geomagnetists will have a lot to keep them busy for the foreseeable future.
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