Climate change shifting poles of the planet
Earth’s spin axis changing due to melting glaciers
Sophisticated new gravity research suggests that changes in Earth’s climate may actually be having a stunning geophysical effect: slightly moving the location of the planet’s spin axis, or axis of daily rotation. In other words, even as the Earth spins on its axis in a west to east direction, completing a full rotation every 24 hours, that axis itself is also moving. This, in turn, means that the physical North and South poles are actually shifting, with the North Pole now drifting towards England.
And given that much of this is related to the loss of polar ice, a changing climate would appear to be at least partly — although perhaps not wholly — responsible. “If we lose mass from the Greenland ice sheet, we are essentially putting mass elsewhere. And as we redistribute the mass, the spin axis tends to find a new direction. And that’s what we mean by polar motion,” said Surendra Adhikari, a researcher with Caltech and NASA’s Jet Propulsion Laboratory who conducted the work with his colleague Erik Ivins. The new research appeared Friday in Science Advances.
Ivins emphasizes that the study doesn’t explicitly attribute the motion of the pole to human caused climate change — noting that “the word human is not in this paper.” The study wasn’t aimed at attribution of the causes of mass loss — it merely observed them using NASA’s twin GRACE satellites, which measure gravitational changes at the Earth’s surface, and tied that to polar motion.
At the same time, however, much research has suggested that the warming of the Earth is behind considerable polar ice mass, not only in Greenland and Antarc- tica, but also smaller glaciers around the world. NASA research, for instance, finds that Greenland is losing 287 billion tons of ice per year, while Antarctica is losing 134 billion tons.
The Earth’s spin axis or axis of rotation — which is simultaneously imaginary, and yet nonetheless key to understanding and visualizing the nature of the planet’s rotation — has never stayed precisely in place. Movement of material within the planet’s insides, for instance, causes it to shift subtly. So does mass change at the Earth’s surface, which can come from shifts in ice sheets, or even possibly in major atmospheric wind currents. Scientists have tracked such movements for 115 years, and up until the year 2000, the North Pole was moving slowly toward Canada (with corresponding motion of the South Pole).
Since then, however, the new study finds that the motion shifted sharply and now the North Pole is moving toward the U.K. and Europe. The motion has also sped up, though it still isn’t very large. The movement toward Canada was at around 7 to 8 centimetres per year, Adhikari said, and the movement toward the U.K. is now about 16 to 18 centimetres per year.
Why does the pole move? The answer is that if you redistribute mass on a rotating body like the Earth, you also subtly change how it spins. This is called the conservation of angular momentum, and is often illustrated with the analogy of a twirling figure skater whose rate of spin changes when he or she extends or retracts arms or a leg.
“Imagine we have a perfect sphere that is rotating about some spin axis,” says Adhikari. “And if you remove some material from any location ... the pole must be heading toward the direction where you lose the mass. For example, just imagine that Greenland is the only region where we lose mass. Then in principal, the pole must be moving toward Greenland. That’s the kind of law of nature in a way.”
Indeed, previously scientists thought that the loss of ice mass from Greenland and Antarctica were driving a polar shift. The new study says that’s still correct, but there’s a third factor as well, one that this study is new in identifying — the continents, and how much water they contain. “In some locations we are storing more water, maybe through extra precipitation, and in some regions, we are losing more water,” Adhikari said. “And this pattern is contributing substantially to this shift in the general direction of the polar motion.”
Other recent research has also tied the loss of polar ice to subtle changes in the Earth’s rotation, suggesting that these losses can slow the planet’s rotation, in addition to shifting the pole itself.
IF WE LOSE MASS FROM THE GREENLAND ICE SHEET, WE ARE ESSENTIALLY PUTTING MASS ELSEWHERE. AND AS WE REDISTRIBUTE THE MASS, THE SPIN AXIS TENDS TO FIND A NEW DIRECTION. — SURENDRA ADHIKARI, RESEARCHER WITH CALTECH AND NASA