The magnetic field extending from the Sun into the solar system, shaped by solar activity.The interplanetary magnetic field (IMF) is the extension of the Sun's magnetic field carried outward by the solar wind, filling the entire solar system. It is not a static structure but a dynamic, spiral-shaped web of magnetic field lines that constantly changes in response to solar activity. The IMF plays a crucial role in governing space weather, as it interacts with planetary magnetic fields, cosmic rays, and charged particles throughout the heliosphere.
The concept was established in the 1950s by Eugene Parker, who predicted the spiral structure of the solar wind and its embedded magnetic field. The IMF was first directly measured by the Mariner 2 spacecraft in 1962.
The Sun's rotating magnetic field is dragged outward by the supersonic solar wind, a stream of charged particles. Because the Sun rotates, the field lines become twisted into a spiral pattern known as the Parker spiral. The IMF is not uniform; it is divided into sectors where the field points either toward or away from the Sun, and its strength and orientation fluctuate with solar activity, such as coronal mass ejections and solar flares.
The IMF is used to forecast space weather, particularly in predicting geomagnetic storms that can disrupt satellites, power grids, and communication systems on Earth.
The IMF is so weak at Earth's distance that a typical refrigerator magnet is thousands of times stronger, yet it still manages to deflect many cosmic rays and shape the heliosphere's boundary.
| F | variable | frequency of magnetic oscillation — frequency hertz |
| A | variable | extremal cross-sectional area of Fermi surface — area square metre |
| h | constant | planck constant = 6.62607015e-34 joule second |
| e | constant | elementary charge = 1.602176634e-19 coulomb |
| g_N | variable | Newtonian gravitational acceleration — acceleration metre per second squared |
| ν | variable | MOND interpolation function |
| a_0 | constant | Characteristic acceleration scale of Modified Newtonian Dynamics, below which deviations from Newtonian gravity appear. — mond acceleration scale = 1.2e-10 metre per second squared |
| H | variable | Hamiltonian (total energy operator) — hamiltonian joule |
| J | variable | Exchange coupling constant between neighboring spins — exchange coupling joule |
| \mathbf{S}_i | variable | Spin operator at site i — spin operator |
| \mathbf{S}_j | variable | Spin operator at site j — spin operator |
| \sum_{\langle i,j \r | operator | Summation over all pairs of adjacent lattice sites — sum over nearest neighbors |











