Dynamorörelse
Dynamorörelse refers to the complex process within the Earth's core that is believed to be responsible for generating its magnetic field. This process involves the convection of molten iron and nickel in the outer core. As this electrically conductive fluid moves, it creates electrical currents, which in turn generate a magnetic field.
The dynamo effect is thought to be self-sustaining. The Earth's rotation plays a crucial role, influencing the
Scientists study the geodynamo through theoretical modeling, computer simulations, and analysis of paleomagnetic data, which records
The Earth's magnetic field is vital for life on the planet, as it deflects harmful charged particles