phenomenon

interplanetary magnetic field

The magnetic field extending from the Sun into the solar system, shaped by solar activity.
16 related articles · 3 formulas

Description

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.

History

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.

How it works

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.

In practice

The IMF is used to forecast space weather, particularly in predicting geomagnetic storms that can disrupt satellites, power grids, and communication systems on Earth.

Fun fact

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.

Concept graph →

Formulas

$$F = \frac{h}{2\pi e} A$$
Relates magnetic oscillation frequency to Fermi surface cross-sectional area.
What is in the formula
Fvariablefrequency of magnetic oscillation — frequency hertz
Avariableextremal cross-sectional area of Fermi surface — area square metre
hconstantplanck constant = 6.62607015e-34 joule second
econstantelementary charge = 1.602176634e-19 coulomb
f=\frac{ħ}{2πe}a_{{f}} · 2606.28904
$$\nu(g_N) = \frac{1}{2} + \sqrt{\frac{1}{4} + \frac{a_0}{g_N}}$$
MOND function interpolating between Newtonian and deep-MOND regimes.
What is in the formula
g_NvariableNewtonian gravitational acceleration — acceleration metre per second squared
νvariableMOND interpolation function
a_0constantCharacteristic acceleration scale of Modified Newtonian Dynamics, below which deviations from Newtonian gravity appear. — mond acceleration scale = 1.2e-10 metre per second squared
ν(g_n)=\frac{1}{2}+\sqrt{\frac{1}{4}+\frac{a_0}{g_n}} · 2607.05502v1
$$H = -J \sum_{\langle i,j \rangle} \mathbf{S}_i \cdot \mathbf{S}_j$$
Describes magnetic interactions between neighboring spins.
What is in the formula
HvariableHamiltonian (total energy operator) — hamiltonian joule
JvariableExchange coupling constant between neighboring spins — exchange coupling joule
\mathbf{S}_ivariableSpin operator at site i — spin operator
\mathbf{S}_jvariableSpin operator at site j — spin operator
\sum_{\langle i,j \roperatorSummation over all pairs of adjacent lattice sites — sum over nearest neighbors
h=-j\sum_{\langlei,j\rangle}{s}_i*{s}_j, · 2606.29140
h=-j\sum_{\langlei,j\rangle}{s}_i*{s}_j · 2607.02114

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