The North Magnetic Pole has been shifting towards Russia.
Charting a Course: Magnetic North
A compass always points towards the North Magnetic Pole. Maritime and airplane navigation systems, defense systems, and even smartphones depend on accurate magnetic readings.
This magnetism has been long known, but the true origins of this force were poorly understood. In one of the first maps of the Arctic by Gerardus Mercator, the centerpiece of it was massive rock located exactly at the pole, Rupus Nigra et Altissima, or “Black, Very High Cliff.”
Most people thought that this rock formation was magnetic, which provided an easy explanation for why compasses point north. This did not convince Mercator, so he included a different rock, which he labeled the “Magnetic Pole.”
Mercator was right about the general location of Magnetic North, but he did not have the tools we have today to understand how the anomaly moves. The North Magnetic Pole is a spot on the top of the planet where the Earth’s magnetic ﬁeld lines converge and drive straight into its core.
As it turns out, the Earth’s physical structure is behind all this magnetic shifting. The planet’s inner core is made of solid iron, while surrounding that is a molten metallic outer core. It’s from here that heat escapes, creating electric currents in the conductive iron alloys in the core.
In other words, the processes that create the magnetic effect are far more complex — and occur way deeper in the planet — than Mercator could have ever imagined.
The Dynamo Effect
The Earth itself spins on its axis. The inner core spins as well, and it spins at a different rate than the outer core. This creates a dynamo effect that enables the Earth’s magnetic field.
Satellite data tracking the Earth’s magnetic field indicate that the pole is moving faster across the Arctic than previously recorded. While it’s hard to estimate an exact date by which the North Pole will lie in Russia (due to contested geographic claims in the Arctic), it will eventually get there.
What surprises scientists is the rate at which the movement has increased in recent history:
This is happening because of a push and pull between two unusually strong magnetic patches in the Earth’s outer core. One patch is under Canada while the other is beneath Siberia.
The North Magnetic Pole has historically lain within Canadian borders because of stronger pull of the Canadian magnetic patch, but that is changing rapidly.
The Evidence: How Do We Know What We Know?
Scientists can study the phenomenon of moving poles by examining the rocks lying on the ocean floor that captured magnetic traces of previous orientations of the Earth’s magnetic field.
According to the geological record, the last time the poles switched was ~780,000 years ago, and it has happened about 400 times in 330 million years. Each reversal takes roughly a thousand years to complete. The field has weakened about 10% in the last 150 years. Some scientists think this is a sign of a flip in progress.
Technology is advancing and providing new tools for scientists to study this phenomenon. In 2013, the European Space Agency (ESA) launched the SWARM mission to study the Earth’s magnetic field using satellites. This will provide data for modeling the geomagnetic field and its interaction with other physical aspects of Earth, offering a look inside the Earth from space.