The North Pole Is Moving And We Don’t Know Why

Sabine Hossenfelder
Sabine HossenfelderMar 19, 2026

Why It Matters

Accurate magnetic field data underpins global navigation, drilling, and satellite operations, while a potential reversal threatens increased radiation exposure, making the pole’s drift a critical concern for both industry and public safety.

Key Takeaways

  • Magnetic North Pole now moves up to 50 km/year.
  • Rapid drift forces frequent updates to navigation models worldwide.
  • Declining field strength and Siberian surge reshape Earth's magnetic geometry.
  • Oil, aviation, and military rely on accurate magnetic data.
  • Potential geomagnetic reversal could expose Earth to increased radiation.

Summary

The video explains that Earth’s magnetic north pole, distinct from the geographic pole, has begun moving dramatically, now traveling as fast as 50 kilometres per year toward Siberia, and scientists lack a definitive explanation.

For four centuries the pole drifted slowly (5‑10 km/yr) across northern Canada, but since the late 1990s its speed surged. Simultaneously, the planet’s overall magnetic field has weakened by roughly ten percent, while a strong “bundle” under Siberia has grown as the Canadian bundle fades, shifting the pole’s location.

The rapid shift forces frequent revisions of the World Magnetic Model maintained by NOAA and the British Geological Survey; an out‑of‑cycle update was issued in 2019 and a higher‑resolution version arrived this year. Industries from aviation and shipping to oil‑field drilling depend on these models to maintain precise headings, and even a fraction‑degree error can translate into costly offsets.

Continued acceleration could complicate navigation, demand costly model upgrades, and, if a geomagnetic reversal were to occur, temporarily diminish Earth’s shield against solar and cosmic radiation, exposing satellites and power grids to heightened risk.

Original Description

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Earth’s magnetic north pole is changing rapidly. First, it’s moving around quickly (for a geological feature, at least). Second, it seems to be slowly weakening over time, and also a growing number of anomalies have been detected in the Earth’s magnetic field. Let’s take a look.
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