Solar Physics
The Zeeman Effect in Sunspots
How split spectral lines revealed the first magnetic field ever measured beyond Earth
The Zeeman effect in sunspots is the splitting of a single spectral line into two or more polarized components caused by the intense magnetic field inside the spot. Because the wavelength split grows in proportion to the field strength B, it acts as a built-in magnetometer written into starlight. George Ellery Hale exploited it at Mount Wilson in 1908, measuring sunspot fields of roughly 2600–2900 gauss (about 0.26–0.29 tesla) — the first detection of a magnetic field anywhere beyond Earth. The same signal, scanned across the disk, produces the magnetograms that map the Sun's field today, and it remains the primary way we measure magnetic fields on other stars.
- Effect discoveredPieter Zeeman, 1896 (Nobel Prize 1902)
- First measured in sunspotsGeorge Ellery Hale, 1908 (Mount Wilson)
- Umbral field strength~2000–4000 G (0.2–0.4 T)
- Splitting lawΔλ = 4.67×10⁻¹³ · g · λ² · B
- Umbra temperature~3500–4000 K (vs ~5800 K photosphere)
- Workhorse lineFe I 630.25 nm, g = 2.5
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Why the Zeeman effect matters
Magnetism runs the Sun's weather. Sunspots, flares, prominences, coronal loops, the 11-year activity cycle, and the coronal mass ejections that batter Earth's magnetosphere are all magnetic phenomena. But magnetic fields emit no light of their own — they are invisible. The Zeeman effect is the workaround: it imprints the field onto ordinary spectral lines that atoms are already emitting, converting an invisible vector field into a measurable wavelength split and a polarization signature. It is, quite literally, how we read the Sun's magnetism.
- First magnetism beyond Earth. Hale's 1908 measurement made the Sun the first astronomical body with a directly measured magnetic field.
- The engine of space weather. The fields Zeeman diagnostics reveal store the energy that erupts as flares and CMEs, so magnetograms underpin space-weather forecasting.
- A remote magnetometer. No probe need touch the plasma; the field strength arrives encoded in the starlight itself.
- The bridge to stellar physics. The identical signal measures magnetic fields on stars light-years away, from active M dwarfs to megagauss white dwarfs.
- A test of atomic and plasma physics. The line splitting depends on quantum mechanics (Landé factors) and the polarization on radiative transfer in a magnetized atmosphere.
How it works, step by step
The Zeeman effect is fundamentally a quantum-mechanical splitting of atomic energy levels by a magnetic field. Here is the chain from atom to magnetogram.
- Degenerate levels split. An atomic level with total angular momentum J normally has 2J+1 magnetic sublevels (mJ = −J … +J) at the same energy. A magnetic field B breaks this degeneracy: each sublevel shifts by ΔE = g mJ μB B, where μB is the Bohr magneton and g is the Landé g-factor.
- One line becomes several. A transition between two split levels no longer occurs at a single wavelength. Selection rules (ΔmJ = 0, ±1) sort the components into an unshifted π component (Δm = 0) and two shifted σ components (Δm = ±1) — the classic normal Zeeman triplet.
- The split scales with B. The σ components sit symmetrically about line center by Δλ = 4.67×10⁻¹³ · g · λ² · B (λ in ångströms, B in gauss). Measure Δλ, and you have B.
- The components are polarized. Viewed along the field (longitudinal), the two σ components are oppositely circularly polarized and the π component vanishes. Viewed across the field (transverse), all three are linearly polarized. Polarization therefore encodes field direction, not just strength.
- Sunspots supply the strong field. A sunspot umbra carries a near-vertical field of thousands of gauss — strong enough to split iron lines such as Fe I 630.25 nm by tens of milliångströms, comfortably resolvable with a good spectrograph.
- Scan to build a magnetogram. Sweep the spectrograph slit (or use a filtergraph) across the disk, measuring the circular-polarization split at every pixel. The result is a longitudinal magnetogram — a black-and-white map where brightness encodes the strength and sign of the line-of-sight field.
Key numbers: fields, splits, and temperatures
| Quantity | Value | Note |
|---|---|---|
| Earth's surface field | ~0.25–0.65 G | Reference for scale |
| Quiet-Sun general field | ~1–10 G | Large-scale poloidal field |
| Sunspot penumbra | ~700–1500 G | Inclined, more horizontal field |
| Sunspot umbra | ~2000–3500 G | Strong, near-vertical field |
| Strongest spots measured | ~4000–6000 G | Rare, largest active regions |
| Umbra temperature | ~3500–4000 K | vs ~5800 K photosphere |
| Zeeman split, Fe I 630.25 nm at 3000 G | ~0.14 Å per σ (~0.28 Å full) | g = 2.5, easily resolved |
The governing equation
For the normal Zeeman triplet, the wavelength separation between line center and each shifted σ component is:
Δλ = 4.67 × 10⁻¹³ · g · λ² · B
- Δλ — wavelength shift of a σ component from line center, in ångströms (Å).
- g — effective Landé g-factor of the transition (dimensionless), a quantum-mechanical number that sets the line's magnetic sensitivity. Fe I 630.25 nm has g = 2.5; a line with g = 0 does not split at all.
- λ — the rest wavelength of the line, in ångströms.
- B — the magnetic field strength, in gauss (1 G = 10⁻⁴ tesla).
- 4.67 × 10⁻¹³ — the constant e/(4πmec²) expressed for these units; it bundles the electron charge, mass, and the speed of light.
Worked example. For Fe I 630.25 nm (λ = 6302.5 Å, g = 2.5) in a 3000 G umbra, Δλ = 4.67×10⁻¹³ × 2.5 × (6302.5)² × 3000 ≈ 0.14 Å for each σ component from line center, so the two σ lines sit ≈0.28 Å apart. Note the crucial λ² scaling: an infrared line at 1.565 µm splits about six times more than a green line for the same field, which is exactly why weak-field work migrated to the near-infrared. Hale worked at Mount Wilson in 1908, saw both the split and its circular polarization, and read off ~2600–2900 G — the first magnetic field measured beyond Earth.
A note on Hale, 1908
Pieter Zeeman had split a sodium line in the lab in 1896, and Hendrik Lorentz's electron theory explained it — work that earned the pair the 1902 Nobel Prize. George Ellery Hale then asked whether the same signature might appear in sunspot spectra. Using the Snow telescope and later the 60-foot tower at Mount Wilson, he found that lines in sunspots were both split and circularly polarized, and that the polarity of the split flipped between spot pairs. His 1908 papers established that sunspots are seats of intense magnetism, and by 1919 Hale, Ellerman, Nicholson, and Joy had formulated Hale's polarity laws — the observation that a solar hemisphere's leading spots share one polarity, trailing spots the opposite, and the whole pattern reverses each ~11-year cycle (a 22-year magnetic cycle). All of it flows from reading the Zeeman effect.
Common misconceptions
- "Sunspots are dark because they are cold holes." They are cooler (~3500–4000 K) but still incandescent; they look dark only against the hotter surroundings. And they are cool because the strong field throttles convection, not the other way around.
- "The Zeeman effect changes the atom's chemistry." It only shifts and splits energy sublevels; the element and its transitions are unchanged. A line with Landé g = 0 shows no split at all.
- "A magnetogram is a photograph of magnetic field lines." It is a map of one field component (usually line-of-sight) inferred from polarization; the field lines themselves are reconstructed, not seen.
- "Bigger splitting always means a bigger field." Only for a given line — splitting also scales with g and with λ², so comparisons must hold the line fixed.
- "You need to resolve the star to measure its field." No — for distant stars the disk-integrated line still broadens and polarizes in proportion to the field, which is how stellar magnetism is measured.
- "Zeeman splitting and Doppler broadening are the same." Doppler broadening smears a line symmetrically with no polarization; Zeeman splitting produces polarized components whose separation tracks B.
Frequently asked questions
What is the Zeeman effect?
The Zeeman effect is the splitting of a single spectral line into several polarized components when the emitting or absorbing atoms sit in a magnetic field. The field lifts the energy degeneracy of atomic sublevels (different m_J values), so one transition becomes several at slightly different wavelengths. Pieter Zeeman discovered it in 1896; he and Hendrik Lorentz shared the 1902 Nobel Prize in Physics for it.
How did Hale measure the magnetic field of sunspots?
In 1908 George Ellery Hale, using the tower telescope and spectrograph at Mount Wilson, photographed spectral lines from sunspots and saw them split — the Zeeman effect. The components were also circularly polarized, the signature of a line-of-sight field. From the size of the splitting he inferred field strengths of about 2600–2900 gauss. This was the first detection of a magnetic field anywhere beyond Earth and proved sunspots are intensely magnetic.
How strong is the magnetic field in a sunspot?
In the dark central umbra of a large sunspot the field is typically 2000–3500 gauss (0.2–0.35 tesla), with the strongest spots reaching about 4000 gauss. It weakens toward the lighter penumbra and to a few hundred gauss at the outer edge. For comparison, Earth's surface field is about 0.5 gauss and the quiet Sun's general field is only a few gauss, so a sunspot is thousands of times stronger.
Why does the magnetic field make sunspots dark and cool?
The strong vertical field in a sunspot suppresses the convection that normally carries heat up to the surface — the magnetic pressure and tension inhibit the rising hot gas. Starved of that convective heat flux, the umbra cools to about 3500–4000 K versus roughly 5800 K for the surrounding photosphere. It still glows, but against the brighter background it looks dark. So the same field the Zeeman effect reveals is what causes the spot.
What is a magnetogram?
A magnetogram is a map of the Sun's magnetic field made by measuring the Zeeman splitting and polarization of a spectral line at every point on the disk. The circular polarization gives the line-of-sight field (a longitudinal magnetogram, shown as black-and-white for opposite polarities); the linear polarization gives the transverse field. Instruments like SDO's HMI produce full-disk magnetograms every minute or so, tracking the field that drives flares and coronal mass ejections.
How is the Zeeman splitting related to field strength?
The wavelength shift of the split components is directly proportional to the magnetic field strength B. For the normal Zeeman triplet the shift is Δλ = 4.67 × 10⁻¹³ · g · λ² · B, with λ in ångströms and B in gauss. The factor g is the Landé g-factor of the line and sets its magnetic sensitivity. Because Δλ scales with λ², astronomers deliberately use long-wavelength lines (red or infrared) to make weak fields easier to detect.
Can the Zeeman effect measure magnetic fields on other stars?
Yes — it is the foundation of stellar magnetism. A distant star is a point of light, so you cannot resolve its spots, but the disk-integrated line still broadens and becomes polarized in proportion to the surface field. Zeeman broadening measures the average field strength even without polarization; spectropolarimetry with Zeeman-Doppler imaging reconstructs the large-scale field geometry. Fields from a few gauss on Sun-like stars up to tens of kilogauss on some M dwarfs and megagauss on magnetic white dwarfs are measured this way.