An expanding weak spot in Earth’s magnetic field has been growing steadily for over a decade above the South Atlantic Ocean, alarming scientists. This region, known as the South Atlantic Anomaly, is caused by unusual magnetic behaviors called reverse flux patches.
Reverse flux patches are areas where magnetic field lines behave unexpectedly by diving back into Earth’s core instead of extending outward. This reversal is uncommon and is thought to arise from turbulent flows in Earth’s molten outer core, which is responsible for generating the planet’s magnetic field.
Normally, field lines in the southern hemisphere emerge from the core and arc outward. But in the anomaly zone, this flow is disrupted, weakening the magnetic field irregularly and complicating modeling efforts.
The anomaly’s changes are not isolated to the southern hemisphere. In the north, magnetic field trends differ:
These dynamic magnetic shifts highlight the complexity of Earth’s inner structures and their influence on our planet’s protective shield.
Author’s summary: A growing weak spot in Earth’s magnetic field above the South Atlantic reveals complex core dynamics and shifts, with contrasting changes occurring simultaneously in the northern hemisphere.