Page 2: 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.

Volunteers discover rare space weather events using their ears

Our planet rests inside a magnetic cocoon filled with plasma—but it's not always peaceful and quiet. Activity from the sun can send waves through this space, and some of those disturbances can even reach Earth, affecting ...

Navigating the past with ancient stone compass needles

Magnetic rocks with iron oxide concentrations act as natural chroniclers of Earth's past continental movements. Using small samples of rocks, scientists can isolate magnetic grains that were frozen in orientation as the rock ...

The northern lights' dark twin is a wild card for the power grid

Scientists are working to understand how magnetic currents from the sun spread beneath Earth's crust when the northern lights dance across the sky. Their goal is to tame its "dark twin" and prevent damage to our power grid.

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