Page 3: Research news on magnetic field (earth)

Earth’s magnetic field is the vector field generated primarily by dynamo action in the liquid outer core, where convective motion of electrically conducting iron alloys induces and sustains a predominantly dipolar geomagnetic field. It extends from the core through the mantle and crust into space, forming the magnetosphere via interaction with the solar wind. The field is characterized by its intensity, inclination, and declination, and exhibits secular variation, westward drift, and polarity reversals on geological timescales. It governs charged particle dynamics in near-Earth space, shapes radiation belts, and constrains models of core dynamics and planetary evolution.

How our planet's history was shaped when the Earth moved

The history of Earth is written on the great tablets of tectonic plates. The motions of plates shaped land masses, formed oceans, and created the varied climates and habitats that set the stage for evolution and the diversity ...

Ice satellite detects powerful geomagnetic storm with precision

It seems improbable that a satellite designed to monitor polar ice sheets and floating sea ice could accurately measure a disturbance in Earth's magnetic field. But that is just what ESA's CryoSat mission did earlier this ...

Missing geomagnetic reversals: Earth's past may be incomplete

Several studies have predicted that not all geomagnetic reversals have been discovered, but it was unknown in which periods they might be hidden. Researchers led by the National Institute of Polar Research used a statistical ...

When Earth's magnetic field took its time flipping

Earth's magnetic field is generated by the churn of its liquid nickel-iron outer core, but it is not a constant feature. Every so often, the magnetic north and south poles swap places in what are called geomagnetic reversals, ...

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