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Update to essential scientific reference maps reveals new movement of the Earth’s magnetic field

The international science community has released an update to the International Geomagnetic Reference Field, a model created for the public good and used by scientists around the world.

01/01/2025 By BGS Press
Map of the intensity of the Earth’s magnetic field at the surface in January 2025 in units of magnetic field strength called nanoTesla. A new weak point is emerging in the south Atlantic offshore South Africa. BGS © UKRI.
Map of the intensity of the Earth’s magnetic field at the surface in January 2025 in units of magnetic field strength called nanoTesla. A new weak point is emerging in the south Atlantic offshore South Africa. BGS © UKRI.

Every five years since 1990, the international science community teams up to update the International Geomagnetic Reference Field (IGRF), a standard reference set of maps of the Earth’s magnetic field created for the public good. This year, BGS led the coordination and evaluation for the IGRF’s fourteenth update.

True north and magnetic north

Unlike ‘true north’, which is the fixed point around which the rotation axis of the Earth spins, ‘magnetic north’ is constantly moving due to the motion of liquid iron in the Earth’s outer core. As the liquid iron is conductive, the entire magnetic field moves slowly with it, dragged along in an unpredictable way. Compass needles point towards the magnetic pole in the northern hemisphere, so forecasting its movement is crucial for accurate navigation and for other applications. Due to the unpredictability of the flow of the outer core, the maps are updated every five years to remain accurate.

This is where the IGRF comes in. The IGRF can be used for many purposes, particularly those requiring very accurate magnetic field values, including:

• aeromagnetic studies
• mining
• oil and gas exploration
• ionospheric modelling
• space weather forecasting
• spacecraft orientation
• magnetic correction for compass users

Tracking the movement of magnetic north

Magnetic north is estimated to have moved at about 10 km a year from 1600 to 1990. In the 2000s, it accelerated at a record speed up to 55 km a year. The 2019 IGRF update showed magnetic north was moving by around 50 km per year, continuing on its path towards Russia, having been in Canada for the last 400 years.

Newly released maps have shown that the movement of magnetic north has slowed down over the past five years to about 35 km a year, a deceleration that has not been seen before. In comparison, the magnetic south pole has moved very little in the past decade.

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The current behaviour of magnetic north is something that we have never observed before.

With the release of the fourteenth update to the International Geomagnetic Reference Field, we have captured this unprecedented change, ensuring that scientists across the world can continue with their forecasts and explorations.

Ciarán Beggan, BGS Geophysicist.

Magnetic north dip pole locations (red) and ideal geomagnetic poles (blue) from 1900 to 2030. From the International Geomagnetic Reference Field (14th release). BGS © UKRI.
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Magnetic north dip pole locations (red) and ideal geomagnetic poles (blue) from 1900 to 2030. From the International Geomagnetic Reference Field (14th release). BGS © UKRI.

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Measurements of the magnetic field are made at geomagnetic observatories on the ground and by dedicated satellites that orbit around 500 km above the planet’s surface. Data from hundreds of absolute magnetic observatories were used, including nine operated by BGS. To make the maps, tens of millions of measurements are collected and checked for errors, before sophisticated computer programs crunch through the data to extract the core field signals.

As part of the measurements, the geomagnetic community also estimates how the magnetic field will change between 2025 and 2030.

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We predict that the magnetic north pole will continue to slow down its movement over the next five years, although still travelling towards Siberia. Interestingly, in early 2026, both the north and south pole will have the same longitude (135°W), which has not happened in many centuries.

We also noticed there is a new weak region of the field developing offshore South Africa along with the existing weak area known as the South Atlantic Anomaly, which is currently passing over Argentina.

Ciarán Beggan, BGS Geophysicist.

IGRF-14 was created in collaboration with 18 other institutes from four continents and represents the global consensus from international scientists about the Earth’s magnetic field. In 2030, this process will be repeated, in order to update the maps to 2035.

The IGRF-14 is now available for download.

The World Magnetic Model

In conjunction with the US National Oceanic and Atmospheric Administration, BGS has also updated the World Magnetic Model (WMM). The WMM is a series of magnetic field maps that help underpin commercial navigation systems in aircraft and electronic devices including mobile phones, which is also updated every five years.

The WMMHR2025 and the WMM2025 are available for download.

Contact

For more information, please contact BGS press (bgspress@bgs.ac.uk) or call 07790 607 010.

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