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.

Space waves reveal where Earth's magnetic shield is under pressure

A new study led by researchers at the University of Oulu in Finland sheds light on a poorly understood part of space weather: where powerful waves form at the edge of Earth's magnetic shield and where the solar wind can find ...

Turtles may migrate using Earth's magnetic field

New research indicates that sea turtles seem to navigate across hundreds of miles of open ocean using Earth's magnetic field. Previous experimental studies suggested that sea turtles use geomagnetism to navigate, but this ...

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