Solar Physics

Solar Butterfly Diagram

Plot every sunspot's latitude against the calendar and the activity belts trace two mirror-image wings, sweeping from mid-latitudes to the equator every eleven years — the solar dynamo, drawn

The solar butterfly diagram plots sunspot latitude against time. Each 11-year cycle, spots first appear near ±30–35° latitude and the active bands drift toward the equator (Spörer's law), tracing two wings that meet at the equator. Discovered by Edward Maunder in 1904, it is the clearest fingerprint of the solar dynamo.

  • DiscoveredE. W. Maunder, 1904
  • Starting latitude±30–35°
  • Ending latitude±5–8°
  • Cycle length≈ 11 years
  • Empirical ruleSpörer's law

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The plot that reveals a hidden clock

Take a century and a half of sunspot observations. For every spot group, record two numbers: the day it was seen and the heliographic latitude where it sat on the solar disk. Now make a scatter plot — date on the horizontal axis, latitude on the vertical. You do not get noise. You get one of the most elegant patterns in all of astronomy: two roughly triangular bands of points, one above the equator and one below, each starting fat and high and tapering down toward the equator, repeating every eleven years like clockwork. The shape is so evocative that it earned its own name almost immediately — the butterfly diagram, after the wings the two bands form.

The diagram does something a plain sunspot count cannot. A count tells you how many spots there are; the butterfly diagram tells you where they are. And the "where" turns out to march in a strict, predictable choreography. New cycles always begin with spots at high latitude. As a cycle ages, the belt of fresh spots slides equatorward. By the time the cycle dies, spots are erupting almost on the equator itself — just as the next cycle's first high-latitude spots are appearing 25 degrees away. This systematic latitude drift is invisible in the raw spot number and is the single most important constraint on theories of the solar magnetic dynamo.

Spörer's law: the equatorward march

The empirical regularity behind the wings is called Spörer's law, after the German astronomer Gustav Spörer, who quantified it in the 1860s–1880s from his own and Richard Carrington's position measurements. The law states that the mean latitude of sunspot activity decreases monotonically through a cycle:

Cycle phase          Typical spot latitude
─────────────────────────────────────────
Start (minimum)      ±25° to ±35°
Early rise           ±20° to ±25°
Maximum              ±12° to ±18°
Late decline         ±8° to ±12°
End (next minimum)   ±3° to ±8°

A useful empirical fit to the centroid latitude as a function of phase φ (from 0 at the start to 1 at the end of a cycle) is roughly

⟨|λ|⟩(φ) ≈ 28° − 23° × φ        (mean unsigned latitude, degrees)

so activity slides from about 28° to about 5° over a single cycle. Crucially, Spörer's law is a statement about the belt of emergence, not about any individual spot. A spot born at 22° latitude stays near 22° for its whole short life; it is the next batch of spots that emerges a little closer to the equator. The wing is the moving envelope of many short-lived groups.

How the diagram is actually built

Constructing a butterfly diagram requires positional data, not just spot counts, and that is a more demanding observation. The canonical modern compilation rests on the Royal Greenwich Observatory (RGO) photoheliographic results, a daily program of full-disk solar photography begun in 1874 that measured the area and heliographic coordinates of every sunspot group. After RGO ceased solar work in 1976, the US Air Force / NOAA SOON network and (more recently) space-based imagers such as SOHO/MDI and SDO/HMI continued the positional record. NASA Marshall's David Hathaway assembled these into the continuous 1874–present butterfly diagram that nearly every textbook reproduces.

The construction is conceptually simple. The solar surface is divided into latitude strips, typically 1° wide. For each strip and each rotation of the Sun (~27 days), the total sunspot area within that strip is summed and normalized to the visible-hemisphere area. The result is colour-coded — black or red for the strips with the most spot coverage, white for empty strips — and stacked vertically, with time running left to right. The areas matter because they weight the plot by magnetic flux: a single huge spot group carries far more flux than a dozen tiny pores, and the butterfly diagram should reflect where the flux is, not merely where the countable specks are.

Two subtleties make the diagram honest. First, foreshortening: a spot near the limb is seen at a grazing angle, so its area must be corrected by dividing by cos(heliocentric angle). Second, hemispheric asymmetry: the northern and southern wings are not perfect mirror images. One hemisphere usually leads the other by months to a couple of years, and the two can differ in total spot area by tens of percent. The 2008–2019 cycle (Cycle 24), for instance, showed the southern hemisphere lagging and then dominating — asymmetries that any complete dynamo model must explain.

Why the wings drift: the dynamo wave

The butterfly diagram is the visible trace of the solar dynamo — the self-sustaining magnetohydrodynamic process that converts the Sun's rotational and convective energy into a cyclic magnetic field. Sunspots are places where a strong, ~3000-gauss toroidal (east–west) magnetic field has become buoyant, risen through the convection zone, and pierced the photosphere. So the question "why do the spots drift equatorward?" is really "why does the strong toroidal field appear at progressively lower latitudes as the cycle ages?"

Two complementary pictures answer this. In Eugene Parker's classical dynamo-wave description (1955), the coupled growth of toroidal and poloidal field behaves as a travelling wave whose propagation direction is set by the Parker–Yoshimura sign rule:

Propagation along iso-rotation surfaces in the direction of
        s = α × (∂Ω/∂r)

α > 0 (northern hemisphere), ∂Ω/∂r < 0 near the base of the
convection zone  ⟹  s points toward the equator.

Here α is the helicity-driven regeneration term and ∂Ω/∂r is the radial gradient of angular velocity. Where ∂Ω/∂r < 0 — as in the high-latitude tachocline — the rule gives equatorward propagation. At the low latitudes where spots actually appear, however, helioseismology measures ∂Ω/∂r > 0 (angular velocity increasing outward through the tachocline), which would drive the wave poleward. This mismatch is the well-known "solar dynamo dilemma," and it is one of the main reasons the flux-transport picture below was developed.

In the more modern Babcock–Leighton flux-transport dynamo, the equatorward drift is instead set by the deep return flow of the Sun's meridional circulation. Plasma flows poleward at the surface (~10–20 m/s, the flow that also carries decaying spots' flux to the poles to reverse the polar field) and must return equatorward at the base of the convection zone at perhaps 1–2 m/s. That deep equatorward conveyor belt advects the toroidal flux toward lower latitudes, and spots erupt where the field is strongest. In this picture the cycle period is essentially set by the conveyor's turnover time. Both descriptions reproduce the butterfly; distinguishing them is an active research frontier, with helioseismic measurements of the deep meridional flow as the key evidence.

Real numbers: the figures behind the wings

QuantityValueNote
Cycle length (min→min)≈ 11.0 yr (range 9–14)Schwabe cycle
Magnetic (Hale) cycle≈ 22 yearsTwo wings + polarity flip
First-spot latitude±25° to ±35°Per Spörer's law
Last-spot latitude±3° to ±8°Spots rarely cross equator
Equatorward drift rate≈ 2°–3° per yearBelt centroid, not spots
Toroidal field in spots≈ 2,000–3,500 gaussZeeman-measured umbral field
Surface meridional flow≈ 10–20 m/s polewardCarries flux to poles
Deep return flow≈ 1–2 m/s equatorwardInferred, sets the drift
Cycle overlap window≈ 1–2 yearsTwo wing pairs coexist
Positional record begins1874 (RGO)Continuous to present

A few of these numbers are worth dwelling on. The 22-year magnetic cycle, not the 11-year spot cycle, is the fundamental period of the dynamo: it takes two successive wings for the leading-spot magnetic polarity (which flips each cycle by Hale's law) and the polar field to return to their original sign. And the equatorward drift rate of 2–3° per year, multiplied by an ~11-year span, neatly carries the belt from ~30° down to a few degrees — the dimensional sanity check on the whole picture.

Hale's law and the hidden second pattern

The butterfly diagram conceals a second, magnetic regularity discovered by George Ellery Hale and collaborators (1919). Each sunspot group is bipolar — a leading and a following spot of opposite magnetic polarity. Hale's polarity law says that within a given cycle, all leading spots in the northern hemisphere share one polarity and all leading spots in the southern hemisphere share the opposite polarity; and that at the next cycle, both hemispheres' leading polarities flip. This is why the true period is 22 years.

Hale's law gives the cleanest way to assign an overlapping spot to "old cycle" or "new cycle." During the 1–2 year window when both ±5° and ±30° belts are active, the high-latitude spots carry the leading polarity of the coming cycle, the low-latitude spots the polarity of the departing one. Without the polarity tag they would be indistinguishable; with it, the overlapping wings cleanly separate. A related rule, Joy's law, says that bipolar groups are tilted with respect to the equator by an angle that grows with latitude (roughly tilt ∝ sin(latitude)), and this systematic tilt is precisely what lets decaying-spot flux migrate poleward and reverse the polar field — the poloidal-field regeneration step at the heart of the Babcock–Leighton dynamo.

Famous wings: the Maunder Minimum and beyond

The butterfly diagram is not eternal — it can break down. The most famous failure is the Maunder Minimum (roughly 1645–1715), a ~70-year stretch when sunspots almost completely vanished; some decades recorded fewer total spots than a single ordinary year. Strikingly, the handful of spots that did appear clustered almost entirely in the southern hemisphere and stayed at low latitudes — a butterfly with one withered wing. The episode coincided with the coldest part of the "Little Ice Age," and reconstructing it from contemporaneous drawings (the Sun was watched closely after the telescope's 1610 debut, so the absence is real, not a gap in observation) is a cornerstone of solar-terrestrial climate studies.

Other landmark wings include the Dalton Minimum (~1790–1830), a weaker depression; Cycle 19 (peaking 1957–58), the strongest cycle of the space age; and the unusually feeble Cycle 24 (2008–2019), whose late and weak rise — together with a deep, extended preceding minimum — prompted speculation about an approaching grand minimum. The behaviour at the start of Cycle 25 (begun December 2019), which has run somewhat stronger than forecast, is being read directly off the butterfly diagram in near-real time as new high-latitude spots appear.

The extended cycle: wings that start above 30°

A subtler feature emerges when you add tracers other than spots. The torsional oscillation (a pattern of slightly faster- and slower-rotating latitude bands measured by helioseismology), the emergence of ephemeral magnetic regions, and the migration of coronal green-line emission all show the activity band beginning at latitudes as high as 50–60°, well before the first true sunspots appear near 35°. The band then drifts equatorward for far longer than the nominal 11 years — sometimes 17–18 years from highest latitude to the equator. This is the so-called extended solar cycle: the dynamo wave seems to switch on at high latitude years before it is strong enough to make spots, and successive extended branches overlap heavily. The clean two-wing butterfly is thus a low-latitude slice of a longer, fainter migration that the spot data alone cannot show.

Common misconceptions and edge cases

  • "Spots migrate toward the equator." No — the belt of emergence migrates. Individual spots are nearly fixed in latitude over their days-to-weeks lifetimes. Confusing the two is the most frequent error; the wing is a statistical envelope.
  • "The diagram tracks spot motion in time." It tracks where new spots appear, snapshot by snapshot. It is a plot of emergence latitude versus date, not the trajectory of any object.
  • "Spots routinely cross the equator." They almost never do. Activity dies out at ±3–8°; the equator itself is a near-dead zone, and the two wings approach but rarely touch. This near-symmetry across the equator is itself a strong dynamo constraint.
  • "Each wing is one cycle, cleanly separated." Successive cycles overlap for 1–2 years around minimum, so you can see two pairs of wings at once. Hale's polarity law is what distinguishes them.
  • "The northern and southern wings are identical." They are mirror-symmetric only on average. Real cycles show hemispheric asymmetry in timing (months to years) and in total area (tens of percent), and explaining that asymmetry is an unsolved problem.
  • "The butterfly always looks the same." During grand minima like the Maunder Minimum the pattern collapses — few spots, often one-hemisphere-dominated, no proper wings. The butterfly is a property of the active dynamo, not a fixed law of the Sun.

Frequently asked questions

Why is it called a butterfly diagram?

When you plot the latitude of every sunspot group against the date it was observed, the data points fill two roughly triangular bands — one in the northern hemisphere, one in the southern — that mirror each other across the equator. Each band starts wide and high (near ±30–35° latitude at the start of a cycle) and narrows toward the equator as the cycle ages. Side by side the two bands look like the wings of a butterfly, which is the name Edward Maunder and others gave the plot after he first published it in 1904.

What is Spörer's law?

Spörer's law is the empirical rule, named for Gustav Spörer, that the mean latitude of sunspots decreases as the cycle progresses. The first spots of a new cycle appear at high latitudes, typically ±25–35°, and over the following years successive groups emerge progressively closer to the equator, reaching about ±5–8° by the end of the cycle. The butterfly diagram is the graphical statement of Spörer's law: it shows the activity belts sweeping equatorward, not the individual spots themselves migrating.

Do individual sunspots migrate toward the equator?

No — and this is the most common misconception. A single sunspot group lives only days to a couple of months and stays at roughly fixed latitude during its life. What drifts equatorward is the latitude band where new spots are emerging. Early in the cycle that band sits near ±30°; a few years later the band has shifted so that new spots emerge near ±15°; near solar minimum new spots appear at ±5°. The butterfly wing is the envelope of many short-lived groups, not the path of one spot.

Why do the activity belts drift toward the equator?

The drift reflects the propagation of the solar dynamo wave. In the Babcock-Leighton flux-transport picture, the deep equatorward branch of the meridional circulation — flowing at roughly 1–2 m/s near the base of the convection zone — advects the toroidal magnetic field toward the equator, and sunspots erupt where that field is strongest. In the classical Parker dynamo wave picture, the direction of propagation is set by the sign of the product of differential rotation shear and the kinetic helicity (the Parker-Yoshimura sign rule), which points equatorward in the Sun. Both pictures reproduce the observed butterfly wings.

Why do new-cycle and old-cycle spots overlap on the diagram?

Because a new cycle's high-latitude spots begin erupting before the previous cycle's low-latitude spots have finished. For a year or two around solar minimum you can see two pairs of wings active at once: old-cycle spots near ±5–10° and new-cycle spots near ±25–30°. You can tell them apart because Hale's polarity law flips the leading-spot magnetic polarity between successive cycles, so the new high-latitude groups have the opposite leading polarity from the old equatorial ones. This overlap is why a sunspot 'cycle' is closer to 13 years long from first to last spot even though minimum-to-minimum is about 11 years.

How far back does the butterfly diagram extend?

Reliable position records of sunspots begin with the Royal Greenwich Observatory photoheliographic programme in 1874, which underpins the canonical butterfly diagram maintained today by NASA Marshall (David Hathaway's compilation). Earlier sketches by Richard Carrington (1853–1861) and Gustav Spörer extend the latitude record into the mid-19th century, and the telescopic sunspot-number series of Wolf reaches back to 1700. The Maunder Minimum of roughly 1645–1715, when sunspots nearly vanished and the few that appeared clustered in the southern hemisphere, predates positional data and is reconstructed from contemporaneous drawings.