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Alfvén wave

Low-frequency plasma wave

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  • 8 chapters

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Through Magnetic field, Solar wind and Oscillation

Discovered theoretically by Alfvén in 1942—work that contributed to his 1970 Nobel Prize in Physics—these waves play a fundamental role in numerous astrophysical and laboratory plasma phenomena. Alfvén waves are observed in the solar corona, solar wind, Earth's magnetosphere, fusion plasmas, and various astrophysical settings. They are particularly significant for their role in the coronal heating problem, energy transport in the solar atmosphere, particle acceleration, and plasma heating.

Unlike some other plasma waves, Alfvén waves are typically non-compressive and dispersionless in the simplest MHD description, though more complex variants such as kinetic and inertial Alfvén waves emerge in certain plasma regimes. The characteristic speed of these waves—the Alfvén velocity—depends on the magnetic field strength and the plasma density, making these waves an important diagnostic tool for magnetized plasma environments.

Definition

An Alfvén wave is a low-frequency (compared to the ion gyrofrequency) travelling oscillation of the ions and magnetic field in a plasma. The ion mass density provides the inertia and the magnetic field line tension provides the restoring force. Alfvén waves propagate in the direction of the magnetic field, and the motion of the ions and the perturbation of the magnetic field are transverse to the direction of propagation. However, Alfvén waves existing at oblique incidences will smoothly change into magnetosonic waves when the propagation is perpendicular to the magnetic field.

Alfvén waves are dispersionless.

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