
A pair of equal and opposite magnetic poles separated by a distance, describing the simplest field configuration.A dipole is the simplest configuration of a magnetic field, consisting of two opposite poles—north and south—separated by a distance. It serves as the fundamental building block for understanding more complex magnetic phenomena, from bar magnets to planetary magnetospheres. In physics, the dipole approximation is often used to describe the field at large distances from any localized current distribution, making it a universal tool in electromagnetism.
The concept of magnetic dipoles dates back to the 13th century with Petrus Peregrinus's experiments on lodestones, but the mathematical description was formalized by William Gilbert in his 1600 work 'De Magnete.'
The dipole field arises from a separation of magnetic charges (or, more accurately, from a loop of electric current). The field lines emerge from the north pole, curve through space, and re-enter at the south pole, with the strength decreasing as the cube of the distance. In quantum systems, dipoles can also refer to electric charge separation, which plays a role in molecular interactions and light-matter coupling.
Dipole antennas are ubiquitous in radio and telecommunications, and magnetic dipoles are central to MRI machines and data storage technologies.
The Earth's magnetic field is approximately a dipole, but its poles wander and have reversed many times in geological history.





