Sun’s Biggest Sunspots Had Superflare Potential, New Study Finds

Researchers from the Max Planck Institute for Solar System Research (MPS) and the University of Colorado have found new evidence that the Sun’s largest historical sunspots could, in rare cases, produce superflares.

Solar flare energy scaling relates observable properties of active regions (ARs), sunspots, and flare ribbons to the total energy released during a flare. The recent Krivova et al. (2026) study uses an empirical chain of relations grounded in modern SDO observations to estimate upper limits for the largest historical sunspots.

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Researchers from the Max Planck Institute for Solar System Research (MPS) and the University of Colorado have found new evidence that the Sun’s largest historical sunspots could, in rare cases, produce superflares.

The study, led by Natalie Krivova and published on 10 September 2026 in Philosophical Transactions of the Royal Society A (arXiv:2603.09474), focuses on empirical upper limits for solar flare energies.

The team analyzed data from NASA’s Solar Dynamics Observatory (SDO) on more than 300 of the strongest flares observed between 2010 and 2016. They related flare energy (via flare-ribbon areas as a proxy for magnetic reconnection) to the size of the associated active regions.

They then extrapolated the upper- envelope statistical relations (focusing on the extreme tail of the distribution) to historical sunspot records, which have been systematically tracked for centuries.

The standout case is the Great Sunspot of April 1947 (Active Region 14886), one of the largest on record. It covered roughly 0.6% of the visible solar disk (maximum corrected area ~6,100- 6,132 millionths of the solar hemisphere), with a diameter about 40 times that of Earth. No superflare occurred then.

This builds on a 2024 MPS- led study (published in Science) of ~56,450 Sun- like stars observed by Kepler.

That work found superflares occur roughly once per century on such stars, far more frequently than earlier estimates.

The new results indicate the Sun is, in principle, “superflare- capable” because it can form sufficiently large and complex active regions/sunspots. Extreme events would still be rare, and the relationship between the largest flares, coronal mass ejections, and extreme solar particle events (inferred from cosmogenic isotopes) is not one- to- one.

No superflare has been directly observed on the modern Sun, and whether one has ever occurred remains an open question. The work strengthens the case that such events are physically plausible on the basis of observed solar structures and stellar statistics, with potential relevance for extreme space weather risks to technology and infrastructure.

The Carrington Event (also called the Carrington Storm or solar storm of 1859) remains the most intense geomagnetic storm in recorded history. It peaked on 1- 2 September 1859 during solar cycle 10 and is named after British astronomer Richard Carrington, who made the first observation of a solar flare associated with it.

The flare originated in a large sunspot group. Modern estimates of its maximum corrected area range from roughly 2,300- 3,500 millionths of the solar hemisphere (msh), with some reconstructions adopting ~3,100 msh as a conservative value. This places it among the larger historical active regions, though smaller than the record 1947 Great Sunspot (~6,100 msh).

Late August 1859: A large, complex sunspot group was visible on the Sun. Auroral activity and magnetic disturbances began around 28- 29 August, indicating earlier coronal mass ejections (CMEs) from the same region.

1 September 1859, ~11:18 GMT: Richard Carrington (and independently Richard Hodgson) observed a brilliant white- light flare lasting about 5 minutes while sketching the sunspot group. Carrington described “two patches of intensely bright and white light.” Magnetometers simultaneously recorded a “crochet” (solar flare effect) caused by enhanced ionospheric ionization.

~17- 18 hours later (early 2 September): A fast CME arrived at Earth, triggering the main geomagnetic storm. The short transit time implies an unusually high speed (roughly 2,000 and more km/s).

The flare originated in a large sunspot group. Modern estimates of its maximum corrected area range from roughly 2,300- 3,500 millionths of the solar hemisphere (msh), with some reconstructions adopting ~3,100 msh as a conservative value. This places it among the larger historical active regions, though smaller than the record 1947 Great Sunspot (~6,100 msh).

Flare magnitude estimates (modern GOES soft X- ray scale, revised) typically fall in the range X45- X146, with many studies centering around ~X45. Bolometric (total radiated) energy estimates are on the order of a few ×1032\times 10^{32} erg, with some approaching ∼1033\sim 10^{33}erg depending on conversion factors from soft X- ray class. Recent analyses of Carrington’s original drawings have suggested even higher values in some scenarios (e.g., ~X80 range), though uncertainties remain large.

Auroras: Extremely bright and widespread. They were visible at unusually low geomagnetic latitudes, down to ~18- 25° (Caribbean, Central America, Hawaii, Colombia, and possibly lower). People in the northeastern United States could read newspapers by auroral light; gold miners in the Rocky Mountains woke and began preparing breakfast, thinking dawn had arrived. Displays lasted many hours and included red, green, and other colors.

Geomagnetic storm intensity: Estimates of the storm’s strength (Dst index) range widely from about -800 nT to as low as -1,750 nT or lower in early analyses (based partly on the Colaba, India magnetogram). More recent re- evaluations often place it around -900 nT or somewhat stronger, still far exceeding modern extreme events (e.g., March 1989 Quebec storm ~–589 nT). Rapid field changes induced strong geoelectric fields.

Telegraph systems: Widespread disruption across Europe and North America. Operators reported electric shocks, sparks, and fires at stations. In some cases (notably the Boston- Portland line), operators disconnected batteries and continued transmitting messages using only the currents induced by the storm, the so- called “auroral current” or “celestial power.”

The Carrington Event is the benchmark for extreme space weather. A comparable event today could severely disrupt satellites, GPS, power grids, and communications, with potential economic costs in the hundreds of billions to trillions of dollars (depending on the region and duration of outages).

It is often treated as a “1- in- 100 to 1- in-500 year” (or rarer) event, though related extreme solar particle events inferred from cosmogenic isotopes (e.g., AD 774/775) indicate that even stronger particle events have occurred over millennia.

In the context of the recent Krivova et al. (2026) study, the Carrington active region’s size yields estimated flare energies consistent with independent historical reconstructions (typically ~1×10331 \times 10^{33} erg under upper envelope scalings, with higher outliers possible), reinforcing that it ranks among the most energetic flares in the observational record while remaining below true stellar superflare energies (>1034>10^{34}erg).

The event also marks the birth of solar– terrestrial physics: Carrington cautiously noted the coincidence between the flare and the subsequent magnetic storm, establishing the first clear observational link.

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Here are the confirmed publication details for the two related papers from the Max Planck Institute for Solar System Research (MPS) and collaborators, both appearing in the same 2026 issue of Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences:

Natalie Krivova et al., “Empirical flare energy limits for the largest historical sunspots”

This is the main empirical study discussed previously. It uses SDO/RibbonDB flare data (2010- 2016) to derive upper- envelope scaling relations between active-region/sunspot size and flare energy, then extrapolates to the largest historical sunspots (especially the April 1947 Great Sunspot).

It concludes that such regions could, in rare extreme cases, reach bolometric energies of a few ×1034\times 10^{34}erg, overlapping the lower end of the stellar superflare regime.

Published:  Philosophical Transactions of the Royal Society A Mathematical, Physical and Engineering Sciences (2026)

DOI: 10.1098/rsta.2025.0290

Valeriy Vasilyev et al., “Linking solar magnetism, extreme solar particle events and stellar superflares”

This is a complementary review/synthesis paper. It discusses the connections (and differences) between extreme solar particle events (ESPEs, inferred from cosmogenic isotopes), solar magnetic activity, and stellar superflares observed on Sun- like stars. It notes that while both ESPEs and superflares involve extreme magnetic energy release, the relationship is not one- to- one.

Published:  Philosophical Transactions of the Royal Society A Mathematical, Physical and Engineering Sciences (2026)

DOI: 10.1098/rsta.2025.0261

These two papers were highlighted together in the Max Planck Society press release of 10 September 2026 (“Sonne: Neuer Hinweis auf Superflares” / “Sun: New Evidence of Superflares”).

The Krivova paper provides the new empirical evidence that the Sun’s largest recorded sunspots have the potential to power superflare -level energies, while the Vasilyev paper places that finding in the broader context of solar- stellar comparisons and extreme particle events.

Finding the 1859 Carrington Event in Tree Rings

The 1859 Carrington Event, the most intense geomagnetic storm in recorded history (peaking September 1–2, 1859), was driven by a massive coronal mass ejection (CME) from the Sun, causing widespread telegraph disruptions, brilliant auroras visible near the equator, and white-light solar flares observed by Richard Carrington.

A vibrant display of the Northern Lights (auroras) illuminating the night sky with green, purple, and blue hues, framed by tall power lines and silhouettes of people observing the natural phenomenon.

The 1859 Carrington Event, the most intense geomagnetic storm in recorded history (peaking September 1–2, 1859), was driven by a massive coronal mass ejection (CME) from the Sun, causing widespread telegraph disruptions, brilliant auroras visible near the equator, and white-light solar flares observed by Richard Carrington.

Tree rings detect solar events via spikes or anomalies in radiocarbon (Δ¹⁴C). High-energy solar protons from solar energetic particle (SEP) events collide with atmospheric nitrogen, producing excess ¹⁴C that mixes into CO₂ and gets fixed into tree cellulose during photosynthesis. This creates sharp, annual spikes for extreme “Miyake events” (e.g., AD 774, 993), but subtler signals for moderate storms like Carrington.

Breakthrough in 2024: Researchers led by Joonas Uusitalo (University of Helsinki) detected the first tree-ring signature of the Carrington Event in subarctic Scots pines (Pinus sylvestris) from Lapland, Finland (high latitudes: Inari, Värriö, Hetta; ~68–69°N). They analyzed 5–8 replicate annual samples per year from 1853–1871 across three trees, measuring Δ¹⁴C via accelerator mass spectrometry (AMS) at three labs (Helsinki, ETH Zurich, Yamagata).

Close-up of a tree trunk showing tree rings with a vibrant aurora borealis in the night sky.

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From Watts Up With That?

By Anthony Watts

An illustration of the Sun's surface showing a coronal mass ejection along with a historical sketch of sunspots from September 1, 1859, by astronomer Richard Carrington, including a scale reference for Earth.

A research group coordinated by the University of Helsinki was able to measure a spike in radiocarbon concentration of trees in Lapland that occurred after the Carrington flare. This discovery helps to prepare for dangerous solar storms.

The Carrington Event of 1859 is one of the largest recorded solar storms in the last two centuries. It was seen as white light flares on a giant sunspot group, fires at telegraph stations and disturbances in geomagnetic measurements, as well as aurorae even in tropical regions. 

In a joint study carried out by the University of Helsinki, Natural Resources Institute Finland and the University of Oulu, a sign of an increase in radiocarbon concentrations following the Carrington storm was detected for the first time in tree rings. Previously, radiocarbon traces have only been detected from far more intense solar storms.

Discovery through a cosmic marker

Encounters between strong magnetised clouds of charged particles released from the Sun, known as solar plasma flows, and Earth’s geomagnetic field result in geomagnetic storms. The geomagnetic field directs the solar storm particles into the atmosphere primarily through the Polar regions. The most visible consequence of the phenomenon are aurorae. 

In the upper atmosphere, sufficiently high-energy particles can, through nuclear reactions, also produce radiocarbon (14C), a radioactive isotope of carbon. Over the course of months and years, radiocarbon ends up in the lower atmosphere as part of atmospheric carbon dioxide, and eventually in plants through photosynthesis. The process of photosynthesis preserves the information contained in carbon dioxide in the annual rings of trees.

To obtain the information held by radiocarbon, samples are extracted by carving from the wood material grown over individual years. The samples are processed to cellulose and the cellulose into pure carbon by burning and chemical reduction. The fraction of radiocarbon in pure carbon is measured using a particle accelerator. 

“Radiocarbon is like a cosmic marker describing phenomena associated with Earth, the solar system and outer space,” says Markku Oinonen, Director of the University of Helsinki’s Laboratory of Chronology, who headed the study.

Mapping solar storms

A solar storms corresponding to the Carrington event in modern times would disrupt electrical and mobile networks and cause major problems for satellite and navigation systems, leading to problems in, for example, air traffic. This is why accurate knowledge of solar behaviour benefits society.

Solar storms smaller and more common than the Carrington storms can be studied with measuring devices and satellites nowadays, while larger ones can be investigated, for example, by measuring radiocarbon concentration in tree rings. 

So far, it has not been possible to study specifically medium-sized storms such as the Carrington event, which have not occurred in modern times, using conventional radiocarbon techniques. This recent study opens up a potential new way of investigating the frequency of Carrington-sized storms, which may help to better prepare for future threats.

Increasingly accurate information on the carbon cycle

The results were interpreted using a numerical model of radiocarbon production and transport developed by researchers at the University of Oulu.

“The dynamic atmospheric carbon transport model was specifically developed for describing geographical differences in the distribution of radiocarbon in the atmosphere,” says Postdoctoral Researcher Kseniia Golubenko from the University of Oulu. 

What was significant in the recently published study was how the radiocarbon content of trees in Lapland differed from that of trees at lower latitudes. The first measurements were carried out at the Accelerator Laboratory of the University of Helsinki, while repeat measurements conducted in two other laboratories significantly reduced the previous uncertainties.

The discovery can help to better understand atmospheric dynamics and the carbon cycle from the time before human-generated fossil fuel emissions, enabling the development of increasingly detailed carbon cycle models.

“It’s possible that the excess of radiocarbon caused by the solar flare was primarily transported to the lower atmosphere through northern regions, contrary to the general understanding of its movement,” muses Doctoral Researcher Joonas Uusitalo from the Laboratory of Chronology.

Other sources of radiocarbon

“It’s also possible that the cyclic change in the production of radiocarbon in the upper atmosphere caused by the variation in solar activity has resulted in the local differences on the ground level seen in our findings,” Uusitalo adds.

According to Uusitalo, the dominant fraction of radiocarbon is produced by galactic cosmic rays coming from outside the solar system, even though exceptionally strong solar storms generate individual bursts of the isotope in the atmosphere. Cosmic rays, in turn, are weakened by solar wind, a continuous flux of particles originating in the Sun that fluctuates between stronger and weaker in 11-year cycles. 

The topic requires further research. Historical records show that significant geomagnetic storms also took place in 1730 and 1770, which is why their tracking is likely to be in focus next.

The recently published study was carried out as a collaborative project of the University of Helsinki’s Laboratory of Chronology and Department of Physics, and Natural Resources Institute Finland. Researchers from the University of Oulu, Nagoya University, Yamagata University and ETH Zurich also contributed to the study. The study received funding from the Research Council of Finland, the Finnish Cultural Foundation and the Emil Aaltonen Foundation.

Original article: Joonas Uusitalo, Kseniia Golubenko, Laura Arppe, Nicolas Brehm, Thomas Hackman, Hisashi Hayakawa, Samuli Helama, Kenichiro Mizohata, Fusa Miyake, Harri Mäkinen, Pekka Nöjd, Eija Tanskanen, Fuyuki Tokanai, Eugene Rozanov, Lukas Wacker, Ilya Usoskin, Markku Oinonen. Transient Offset in 14C After the Carrington Event Recorded by Polar Tree Rings. AGU, 2024.

DOI: 10.1029/2023GL106632

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Transient Offset in 14C After the Carrington Event Recorded by Polar Tree Rings

Researchers analyzed annual Δ¹⁴C from subarctic Scots pines (Pinus sylvestris) in Finnish Lapland (>68°N). Multiple replicates (5–8 per year) from three trees were measured via accelerator mass spectrometry across 1853–1871.

No immediate spike in the 1859 or 1860 ring.

A statistically significant transient offset (excess Δ¹⁴C) appeared in high-latitude trees compared to mid-latitude records, peaking during 1861–1863 (~3–6‰ higher, with averages around 3.5‰ in 1862).

The offset faded by ~1864–1865, lasting ~4 years.

Solar energetic particles (SEPs) from the Carrington Event entered the atmosphere preferentially over the poles due to Earth’s geomagnetic funneling. Excess ¹⁴C production occurred mainly in the polar stratosphere.

Faster stratosphere-troposphere exchange (STE) in the Arctic (due to polar vortex dynamics and weaker stratification) transported this ¹⁴C downward more rapidly. Trees at high latitudes incorporated it into cellulose during photosynthesis, creating a delayed but persistent local excess not diluted globally.

Atmospheric models (e.g., SOCOL-AERv2) partially reproduce this polar enhancement but underestimate its magnitude, suggesting gaps in understanding high-latitude carbon transport.

A Scots pine tree with a cut tree ring is illuminated by colorful northern lights in the background, surrounded by a snowy landscape.

From The Geophysical Research Letters – Wiley Online Library

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