The Earth’s magnetic field is created by the movement of molten iron in the Earth’s core. This movement of molten iron creates a magnetic field which then interacts with the flowing charges to generate an electric field.
On some freezing nights, nature paints the dark canvas above the Arctic circle with light strokes of yellow and green. The wavering, fluorescent hues are recognized to be one of the most beautiful and cherished of nature’s innumerable works of art. This exhibition of rippling lights is commonly referred to as the northern lights.
The splendid display is actually a result of extremely harmful cosmic rays blurted out by the Sun interacting with the Earth’s magnetic field. If this field did not exist, the ozone layer would have been burnt to shreds and we would have been mercilessly fried. This is what happened with Mars when its magnetic field gradually dwindled and expired. So, what causes this magnetic field?
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The Basics: Ampere’s and Faraday’s Law
The magnetic field does not protect the Earth like the thick walls of a fort, it rather resembles a thin curtain or a blanket shrouding the blue dome. It is often hard to believe that it is around 40,000 times weaker than a mere fridge magnet!
The Earth’s magnetic field behaves as if a vertical column between the poles was hollowed out and a standard bar magnet was planted in the cavity. However, the magnet is not aligned perfectly with the poles, it is marginally inclined. What’s more, we found that the magnetic lines run from the south pole towards the north pole. This implies that the magnetic north is situated beside the geographical south, while the magnetic south resides along the geographical north.
Now, because opposite sides of a magnet attract, when the red needle or north magnetic pole of a compass deflects and points towards the geographical north, it is actually being attracted by the south magnetic pole of the Earth’s imaginary bar magnet.
What physicist Ampere discovered was that such a deflection can also be observed around a current carrying wire. By placing the compass at different locations in a wire’s vicinity, he discerned the direction of the magnetic field. He found that the lines run around the wire in concentric circles. The major implication is that electricity or moving charges generate a magnetic field.
People believed the relationship was unidirectional until Faraday showed that electricity and magnetism are two sides of the same coin. Faraday observed that current is induced in a wire when a magnet is moved around it. Movement is the stressed word. It is not the presence of a stationary magnet, but a moving magnet, a changing magnetic field that induces the electric field.
But according to Ampere, an electric field generates a magnetic field, which, as we learned, generates an electric field, which then generates a magnetic field and so on. What is created is a self-sustained cycle of electric and magnetic fields. This is how a dynamo light mounted on a bicycle works: when we pedal, essentially, either a wire is rotated around a fixed magnet or a magnet is rotated around a fixed coil of wire – no matter what configuration you use, the dynamo or generator relies on a symbiotic relationship between moving charges and magnetism. Earth’s magnetic field is also generated by the same principle.
The Dynamo Theory
If you were to open the lid on Earth like a Kinder Joy, you’d find inside a solid core dipped in a viscous liquid. Together they constitute the Earth’s core: the hellish molten liquid is known as the outer core while the solid core which is two-thirds the size of the moon sunk in it is called the inner core.
The inner core burns at 6,000 C, which is almost equal to the temperature on the Sun’s surface, however, the core is counterintuitively solid and not liquid due to Earth’s stark gravitational pressure. It is mostly solid iron and, as newer studies are finding out, possibly oxygen and sulfur as well. Whereas, the outer core, which boasts a temperature of 2200 C, is primarily sweltering, molten iron blended with a tinge of nickel. We believe it is this molten iron that generates Earth’s magnetic field.
Now, because we cannot peek inside the core, we can only infer the causes of its magnetic properties based on theoretical physics and studying igneous rocks. The most plausible theory is analogous to, as mentioned, a dynamo. According to it, it is the motion of molten iron — an excellent conductor for it is an ocean of electrically charged particles – that gives form to a magnetic field. The resulting magnetic field interacts with the flowing charges to generate an electric field and the cycle goes on to sustain a perpetual magnetic field. This is known as a geomagnetic dynamo.
However, the dynamo mounted on a cycle requires the energy of the cyclist to rotate the pedal. Similarly, the movement of molten fluid can only be achieved at the expense of energy, but what is the source of this energy? We currently believe that the energy arises from the convection or heat currents in the outer core when lighter iron sinks towards the inner core and eventually condenses into the solid. Condensation is essentially a loss of heat, and it is this heat that fuels the waves of molten iron. The magnitude of Earth’s magnetic field is so small because 99% of it is confined to the core. Only a meager portion escapes it to form the outer veil.
The disturbances in the outer core spread like the disturbances in weather. Their trajectories curve, curl and spiral as they spread outwards like whirlpools, thereby distorting the generated magnetic field. However, Earth’s rotation instills symmetry in their patterns. The rotation aligns the haphazard magnetic fields as it causes the current to be somewhat symmetrical around the axis. This force is called the Coriolis force. The alignment combines the plethora of minute fields to form one giant magnetic field, a semi-uniform magnetic field that is reminiscent of the field emanating from a bar magnet.
So, Earth’s magnetic field is produced by the combinatorial effects of convection currents and Earth’s rotation. Despite rotating at almost the same speed as Earth, Mars isn’t shielded by a field because it doesn’t foster a dynamo like Earth does. The non-linear differential math involved in understanding the disturbances, like the math involved in making weather predictions, is tremendously difficult and has therefore limited our understanding of the Earth’s magnetic field. Still, supercomputers have allowed us to simulate the probable mechanisms and behavior of turbulences that not only synthesize it but once in a blue moon, flip or reverse the poles!
The Story of More (Adapted for Young Adults): How We Got to Climate Change and Where to Go from Here The Two-Mile Time Machine: Ice Cores, Abrupt Climate Change, and Our Future – Updated Edition (Princeton Science Library, 31)