In February 1204, a Japanese courtier named Fujiwara no Teika wrote three words into his diary that physicists are still arguing about: red lights in the northern sky over Kyoto. Red aurorae at that latitude are rare — they require a genuinely large magnetic storm. Three nights of them suggests recurrent solar flares. Eight hundred years later, a team at the Okinawa Institute of Science and Technology went looking for the tree-ring signature of the solar proton event that should have caused it. They found nothing. No spike. No signal. Just silence where the physics says there should have been one.
This is the problem with the new method for detecting sub-extreme solar proton events: it works, but not completely. And that matters enormously, because as humans return to deep space, sub-extreme SPEs are becoming the dominant radiation threat — not the rare catastrophes everyone already knew about.
What Miyahara et al. Actually Did
The paper, published April 10 in Proceedings of the Japan Academy, Series B, combines two techniques that do not obviously belong together. The first is ultra-precise carbon-14 dating of tree rings — a method the OIST team spent a decade developing. When high-energy protons from a solar particle event slam into the atmosphere, they produce a measurable spike in carbon-14 that gets locked into organic material including tree rings. The second technique is medieval Japanese poetry. Specifically, the Meigetsuki, the diary of Fujiwara no Teika, which records aurora sightings in Kyoto at specific dates going back to the 12th century. The diaries give you a timestamp; the tree rings give you the chemistry. Use the poetry to narrow your search window, then look for the isotopic signature.
The result: a method capable of detecting sub-extreme SPEs — events that are 10–30% the size of the extreme cases, but occur far more frequently, and were previously invisible to the geological record. "Previous studies on historical SPEs have focused on rare, extremely powerful events," said Professor Hiroko Miyahara. "Our paper provides a basis for detecting sub-extreme SPEs — events that occur more frequently and are around 10–30% of the size of the most extreme cases, but still hazardous."
The team dated one such event to winter 1200 through spring 1201 CE — a period during the Medieval Solar Activity Maximum, when the Sun was substantially more active than it is today. They also confirmed something the space physics community has long suspected: solar cycles during that period ran 7–8 years, not the modern 11. The shorter cycle reflects a more energetic, more volatile star.
The 1204 Problem
Here is the part the OIST press release does not emphasize: the Meigetsuki records red aurorae in Kyoto on February 21 and 23, 1204. The diary's author describes three nights of them. Miyahara's own paper states flatly: "We found no enhancement in carbon-14 around 1204 CE when prolonged low-latitude aurorae were observed in Kyoto, Japan, as recorded in Meigetsuki."
The poetry says something happened. The tree rings say nothing did. The method they built to detect sub-extreme SPEs apparently cannot detect all sub-extreme SPEs — including some that were strong enough to push aurorae down to Kyoto. The authors acknowledge this gap and offer no definitive explanation. Possible reasons: the event was below the detection threshold, or the carbon-14 produced did not distribute evenly, or the aurorae were generated by a mechanism that did not produce the expected proton flux. Miyahara told Discover Magazine she is "excited to look further into what solar conditions could cause" events that leave an atmospheric fingerprint without a corresponding isotopic one.
That is a live scientific question. It also undercuts the cleaner narrative that the poetry "predicts" or "uncovers" solar storms. The method is real. It is also incomplete.
Why This Is an Artemis Problem
The reason this matters now is not the 13th century. It is the 2020s.
In 1972, between Apollo 16 and Apollo 17, a string of solar proton events occurred. Miyahara's paper frames it directly: "had these coincided with either expedition, the astronauts would have been helplessly exposed to deadly particle radiation." Apollo 16 launched April 16, 1972. Apollo 17 launched December 7, 1972. The SPEs fell between them — close enough that a mission scheduled differently would have been in the wrong place at the wrong time. The astronauts survived because the timing gods were kind. The physics was not.
The same physics applies to Artemis II, which will carry four astronauts beyond low Earth orbit for the first time since 1972. The Orion spacecraft has a storm shelter — a more-shielded area where crew reconfigure the cabin by piling equipment against the walls to add mass between themselves and incoming particles. NASA calls this "adding mass." Astronauts call it hunkering down. The shelter is designed to keep acute doses below 150 millisieverts under the worst-case solar storm the Sun is expected to produce.
That is for extreme events. Sub-extreme SPEs are different. They are smaller, more frequent, and previously undetectable — which means the statistical baseline for how often they occur, and what dose rates they produce, has been essentially nonexistent. The new method changes that. For the first time, builders have a framework for estimating how frequently the common-but-invisible events happen, not just the rare ones that leave obvious signatures.
This matters for electronics as much as for humans. SPEs cause single-event upsets in electronics, latch-up in semiconductors, and total-dose degradation in solar cells. Commercial constellations in low Earth orbit have some magnetic field protection. A lunar base, a Mars transit vehicle, or a satellite in lunar orbit does not. If sub-extreme SPEs are 10–30% of extreme-event magnitude but occur substantially more often — and the data from the Medieval Solar Maximum suggests cycles ran shorter and hotter — then the cumulative radiation exposure for long-duration deep-space missions is higher than current models assume.
NASA's career limit for effective dose is 600 millisieverts. For Artemis II's 10-day mission, galactic cosmic ray exposure alone is expected to be about 5% of that career limit. Add a sub-extreme SPE, and that fraction changes fast.
What Builders Can Actually Use
The paper's practical contribution is the detection framework, not a complete catalog. The team demonstrated the method works by finding one confirmed event (1200–1201 CE) and identifying the 1204 gap as a genuine detection limit. Scaling this — running the ultra-precise C-14 analysis across more tree-ring samples from more periods — would give mission planners a statistical distribution of sub-extreme event frequency and magnitude. That is what does not exist today.
The 1204 discrepancy complicates the picture. If the method misses some fraction of real events — especially events large enough to produce low-latitude aurorae — then any statistical distribution built using this technique will be a lower bound, not a complete count. The authors know this. The paper does not resolve it.
Miyahara's own statement on integrated approaches is worth quoting in full: "Historical literature provides a candidate time window, and dendroclimatology enables direct intercomparison between detected SPE and reports of sunspots and auroras recorded in literature. Integrated approaches like these are necessary to accurately reconstruct past solar activity." The poetry is a guide, not a machine. It narrows where to look. The isotopic signature does the measurement. When they disagree — as they do in 1204 — something interesting is happening that the model does not yet explain.
The space weather community is already at work integrating this kind of proxy data into longer-range models. The European Space Agency's Vigil mission, slated for 2031, will sit at the L5 Lagrange point specifically to give early warning of solar storms aimed at Earth and cis-lunar space. University of Michigan researchers have built a machine-learning model, running on NASA supercomputers, that forecasts solar activity up to 24 hours in advance using decades of solar imagery. These are real capabilities. The Miyahara method adds historical depth — a longer baseline — that makes the statistical models better.
The Takeaway
The 1972 Apollo near-miss is the story's anchor. Something in the Sun almost killed astronauts on their way to the Moon, and nobody designed a mission around that risk because nobody had a number for how often it happens. The Miyahara paper gives you that number — or the beginning of one. Sub-extreme SPEs are the more common case, they are hazardous, and for the first time they are not invisible.
The 1204 gap is the piece's most interesting footnote. A detection method built to find these events has a blind spot for some of them. That is not a reason to dismiss the result. It is a reason to keep looking.
Sources: Miyahara et al., 2026, Proceedings of the Japan Academy, Series B; OIST News Release, April 10, 2026; NASA Science, March 2026.