A white dwarf star with a significant magnetic field, affecting its evolution and observable properties.A magnetic white dwarf is a stellar remnant—the dense core left after a Sun-like star exhausts its nuclear fuel—that possesses an exceptionally strong magnetic field, often thousands to millions of times stronger than that of the Sun. These fields profoundly affect the star's structure, cooling rate, and the appearance of its spectrum, as the magnetic field splits spectral lines (Zeeman effect) and can even distort the star's shape.
The first magnetic white dwarf was discovered in 1970 by James Kemp and collaborators, who observed circular polarization in the star Grw+70°8247. Since then, surveys have found hundreds, with the recent discovery of 32 new ones (as referenced in the title) expanding the known population.
The magnetic field is thought to be a fossil remnant from earlier evolutionary stages, possibly amplified by differential rotation or convection during the star's collapse. The field interacts with the charged particles in the star's atmosphere, altering energy transport and creating distinct polarization patterns in the emitted light. In some cases, the field can also influence the accretion of matter from a companion star, funneling it toward the magnetic poles.
Magnetic white dwarfs serve as natural laboratories for studying extreme matter under intense magnetic fields, and they are important for understanding stellar evolution and the physics of accretion in binary systems.
Some magnetic white dwarfs have fields so strong that they can slow down the infalling matter from a companion star, creating a 'propeller' effect that ejects material instead of letting it accumulate.










