Solar Physics

Coronal Holes

Open-field windows in the Sun's corona that launch the fast solar wind

A coronal hole is a region of the Sun's corona where the magnetic field is open — instead of arching back to the surface in closed loops, the field lines stretch out into interplanetary space. That open geometry lets hot plasma escape freely, so the region drains to become cooler (~1 million K versus ~1.5–3 million K in the quiet corona) and thinner (roughly one-third the ambient density). Starved of hot, dense plasma, it emits little soft X-ray or extreme-ultraviolet light and shows up as a conspicuous dark patch in images from Skylab, Yohkoh, SOHO and SDO. Coronal holes are the wellspring of the fast solar wind (~700–800 km/s), they persist for many 27-day solar rotations, they grow largest and cap the poles at solar minimum, and their high-speed streams drive recurrent geomagnetic storms and auroras at Earth.

  • Magnetic topologyOpen field lines (extend to interplanetary space)
  • AppearanceDark in EUV / soft X-ray (cool, low-density)
  • Temperature~1 MK (vs ~1.5–3 MK quiet corona)
  • Fast solar wind~700–800 km/s (~0.25% of c)
  • Recurrence~27 days (one solar rotation)
  • Peak size / locationPoles, at solar minimum
  • First imagedSkylab soft X-rays, 1973–74

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Why coronal holes matter

  • Source of the fast solar wind. They resolved a decades-old question — where the steady ~800 km/s wind comes from. The answer is open-field coronal holes.
  • Space-weather forecasting. Because they recur on a ~27-day clock, coronal-hole storms are the most predictable component of space weather.
  • The coronal heating puzzle. Even the "cool" 1 MK hole is still hundreds of times hotter than the photosphere below — a clue in the corona-heating problem.
  • The heliosphere's shape. Fast and slow wind streams set up the Parker spiral and the heliospheric current sheet that structure the entire heliosphere.
  • Satellite drag and GPS. High-speed streams heat and expand the upper atmosphere and disturb the ionosphere, degrading orbits and navigation signals.
  • Aurora chasing. Recurrent coronal-hole streams are behind many of the reliable, non-CME auroral displays at high latitudes.

How a coronal hole works — step by step

The whole phenomenon flows from one fact: magnetic topology decides everything. In the corona, plasma is frozen to the field, so open versus closed field lines produce radically different behaviour.

  1. Open field forms. Where the Sun's global field (a dipole at minimum, tangled at maximum) fails to loop back, field lines run radially outward into space. The photosphere below looks ordinary; the difference is in the corona.
  2. Plasma escapes. Along open lines there is nothing to trap the hot gas. It streams away as solar wind rather than piling up in bright closed loops.
  3. The region cools and thins. Losing its hottest, densest plasma, the hole drops to ~1 MK and to roughly a third of the ambient density.
  4. It goes dark. Coronal EUV/X-ray brightness scales steeply with density (emission ∝ n²) and temperature, so a thinner, cooler region emits far less — a black hole-shaped patch in a 193 Å or soft X-ray image.
  5. The fast wind accelerates. With open geometry and steep pressure gradients, the outflow reaches ~700–800 km/s — nearly double the slow wind.
  6. The stream sweeps Earth. As the Sun rotates (~27 days synodic), the open funnel points at Earth periodically; the high-speed stream arrives 2–3 days later.
  7. A CIR builds. Where fast wind overtakes slow wind ahead of it, it compresses the field into a Corotating Interaction Region — the actual storm driver.
  8. Geomagnetic activity. If the compressed field turns southward, it reconnects with Earth's magnetosphere, lighting auroras and driving a G1–G2 storm.

Key numbers: hole vs quiet corona vs sunspot

PropertyCoronal holeQuiet corona / closed loops
Magnetic fieldOpen (extends to interplanetary space)Closed (loops return to surface)
Temperature~1 MK (10⁶ K)~1.5–3 MK
Electron density~1–3 × 10⁸ cm⁻³~3–10 × 10⁸ cm⁻³ (roughly 3× denser)
EUV / soft X-ray lookDark (low emission)Bright
Solar wind producedFast, ~700–800 km/sSlow, ~300–400 km/s
LifetimeWeeks to many months (recurrent)Loops evolve over hours–days
Peaks in the solar cycleSolar minimum (large polar holes)Active regions peak at solar maximum

A key relation: the wind speed – expansion factor law

Why is coronal-hole wind fast? A robust empirical result (Wang & Sheeley, 1990) links the wind speed at Earth to how quickly the open magnetic flux tube spreads out between the Sun's surface and the source surface (~2.5 solar radii). Define the expansion factor:

fs = (R / Rss)² · [B(R) / B(Rss)]

where:

  • fs — the flux-tube expansion factor (dimensionless);
  • R — the solar radius (≈ 6.96 × 10⁵ km) at the photospheric footpoint;
  • Rss — the source-surface radius (≈ 2.5 R) where the field is taken purely radial;
  • B(R), B(Rss) — the magnetic field strength (in gauss or tesla) at the footpoint and at the source surface.

The empirical rule is an inverse relationship: the fastest wind comes from flux tubes that expand the least (small fs), which is exactly the situation deep in the interior of a large coronal hole. Near a hole's boundary, where the field flares out rapidly, fs is large and the wind is slower. So the deep, uniformly-open core of a big polar hole at solar minimum produces the steadiest, fastest ~800 km/s streams. A companion diagnostic uses the footpoint field magnitude and the distance to the nearest coronal-hole boundary (Riley et al.); both encode the same physics — geometry sets speed.

History: from "M-regions" to Skylab

For decades, geomagnetic records showed disturbances that returned every ~27 days, as if some invisible feature on the Sun kept sweeping past Earth. In the 1930s Julius Bartels named these unseen drivers "M-regions" (M for magnetic), but no one could point to what they were on the solar disk — active regions and flares did not fit the recurrence. The mystery lasted until the space age. In 1973–1974, astronauts aboard NASA's Skylab used the Apollo Telescope Mount to take the first sustained soft X-ray images of the corona and revealed large, persistent dark regions. When these coronal holes were tracked against recurrent geomagnetic activity, the identification was clean: the long-hypothesized M-regions were coronal holes, and their open field lines were funnelling the fast solar wind straight at Earth. Later missions — Yohkoh (soft X-rays, 1991), SOHO and STEREO, and SDO/AIA (continuous EUV since 2010) — turned coronal holes into routinely-monitored, forecastable features, and Parker Solar Probe and Solar Orbiter are now sampling the fast wind close to where it is born.

Common misconceptions

  • "A coronal hole is a hole in the Sun." No — nothing is missing. It is a region of open magnetic field; the plasma is just thinner and cooler, so it emits less light at hot wavelengths.
  • "They're dark in every image." Only at hot EUV/X-ray wavelengths. In visible light the photosphere underneath looks completely normal.
  • "Coronal holes and sunspots are the same dark features." Opposite physics — sunspots are cool, closed-field photospheric spots dark in visible light; coronal holes are open-field coronal regions dark in X-ray/EUV.
  • "They cause huge storms like solar flares." Their storms are usually mild-to-moderate (G1–G2) but frequent and recurrent — quite unlike a big coronal mass ejection.
  • "They only appear at solar maximum." The biggest, most stable holes cap the poles at solar minimum; at maximum they shrink and scatter.
  • "The wind takes hours to reach us." Even the fast ~800 km/s stream needs about 2–3 days to cross the ~150 million km to Earth.

Frequently asked questions

Why do coronal holes look dark?

Because they are cooler and less dense than the surrounding corona. Open magnetic field lines let hot plasma escape as solar wind instead of being trapped in bright closed loops. With less material and a lower temperature (~1 million K versus ~1.5–3 million K in quiet corona), a coronal hole emits far less soft X-ray and extreme-ultraviolet light — so it registers as a dark patch in instruments like SDO/AIA (193 Å, 211 Å) and older Skylab/Yohkoh X-ray images. It is only 'dark' at those hot wavelengths; in visible light the photosphere below looks perfectly normal.

How fast is the solar wind from a coronal hole?

Coronal holes launch the fast solar wind, typically 700–800 km/s at 1 AU, versus roughly 300–400 km/s for the slow wind from closed-field regions. That is about 0.25% of the speed of light. A high-speed stream crosses the ~150 million km from the Sun to Earth in roughly 2–3 days. The fast wind is also hotter, less dense, and steadier in composition than the slow wind, with a lower proton flux but higher speed.

Where are coronal holes usually located?

Near solar minimum, large stable coronal holes cap both the north and south poles, where the Sun's global dipole field is open to space. Near solar maximum the polar holes shrink or vanish and smaller, shorter-lived holes appear at low and mid latitudes. Low-latitude and 'isolated' holes matter most for space weather because their fast streams can sweep directly across Earth's orbital plane (the ecliptic).

How long does a coronal hole last?

Coronal holes are remarkably long-lived. A large hole can persist for many solar rotations — months at a time — because the underlying open-field topology is stable. Since the Sun rotates about once every 27 days as seen from Earth, the same hole sweeps past our planet again and again, producing recurrent, roughly 27-day-periodic geomagnetic disturbances. This recurrence is a signature that distinguishes coronal-hole storms from one-off coronal mass ejection impacts.

Do coronal holes cause geomagnetic storms and auroras?

Yes, but usually mild-to-moderate ones. When a high-speed stream overtakes the slower wind ahead of it, it forms a Corotating Interaction Region (CIR) with compressed, turbulent magnetic field. If that field turns southward (negative Bz) it reconnects with Earth's magnetosphere, driving G1–G2 class geomagnetic storms, auroras at high latitudes, and elevated radiation-belt electron fluxes. Coronal-hole storms are typically weaker than major CME-driven storms but far more frequent and predictable.

What is the difference between a coronal hole and a sunspot?

They are almost opposites. A sunspot is a region of intense, closed, concentrated magnetic field in the photosphere that looks dark in visible light because it is cooler than its surroundings (~3800 K vs ~5800 K). A coronal hole is a region of open, diffuse field in the corona that looks dark in X-ray/EUV because the plasma is thin and cool there. Sunspots are photospheric and closed-field; coronal holes are coronal and open-field. Sunspots peak at solar maximum; the biggest coronal holes appear at solar minimum.

When were coronal holes discovered?

They were first clearly seen in soft X-ray images taken from NASA's Skylab space station in 1973–1974, though hints of 'M-regions' driving recurrent geomagnetic activity had been inferred from the ground decades earlier (Julius Bartels coined 'M-region' in the 1930s). Skylab's Apollo Telescope Mount linked those long-suspected M-regions to real dark coronal features, and later missions — Yohkoh, SOHO, STEREO, and SDO — mapped them continuously and confirmed them as the source of the fast solar wind.