Solar flares are among the most dramatic and energetic phenomena in the solar system, capable of releasing in minutes the equivalent energy of millions of nuclear bombs. These explosive events, driven by the Sun’s magnetic field, can have far-reaching consequences, from disrupting satellite operations to affecting radio communications and power grids on Earth. Despite decades of study, the precise mechanisms that trigger large solar flares have remained incompletely understood. New observations from the European Space Agency’s Solar Orbiter spacecraft now offer unprecedented insight into how these colossal eruptions begin—not as a single, sudden blast, but as a cascading avalanche of smaller magnetic disturbances that rapidly amplify into a powerful flare.
This breakthrough comes from one of the most detailed observations ever recorded of a major solar flare, captured during Solar Orbiter’s close approach to the Sun on 30 September 2024. The findings, published on January 21 in Astronomy & Astrophysics, reveal that subtle, localized magnetic reconnection events can spread swiftly through the solar atmosphere, driving a chain reaction that culminates in a large-scale eruption. Much like a snow avalanche that starts with a minor shift before racing downhill, a solar flare can grow from seemingly small instabilities into a violent release of energy.
Solar flares occur when vast amounts of magnetic energy, stored in twisted and stressed magnetic field lines in the Sun’s atmosphere, are suddenly released. This release happens through a process called magnetic reconnection, in which oppositely directed magnetic field lines break and reconnect into a new configuration. The rapid reorganization converts magnetic energy into heat, radiation, and the kinetic energy of charged particles. Plasma can be heated to millions of degrees, while particles are accelerated to relativistic speeds and flung into space.
The strongest solar flares can trigger geomagnetic storms if their effects reach Earth, potentially interfering with satellites, navigation systems, and communication networks. Because of these risks, understanding how flares originate and evolve is a central goal of space weather research. Until now, scientists lacked direct observations of the earliest stages of large flares, making it difficult to determine how small-scale processes lead to global eruptions.
Solar Orbiter’s unique suite of instruments has changed this picture. During the September 2024 event, four instruments worked in concert to observe different layers of the Sun with extraordinary detail. The Extreme Ultraviolet Imager (EUI) captured high-resolution images of the solar corona, resolving structures only a few hundred kilometers across and updating every two seconds. Meanwhile, the Spectral Imaging of the Coronal Environment (SPICE), the Spectrometer/Telescope for Imaging X-rays (STIX), and the Polarimetric and Helioseismic Imager (PHI) simultaneously examined the Sun’s atmosphere from the hot corona down to the visible surface, or photosphere.
This rare alignment of observing conditions allowed scientists to track the evolution of the flare over approximately 40 minutes before it reached its peak. According to lead author Pradeep Chitta of the Max Planck Institute for Solar System Research, such comprehensive, high-cadence observations are extremely uncommon due to limited observing windows and onboard data storage constraints. The spacecraft was, quite literally, in the right place at the right time.
When EUI began observing the region roughly 40 minutes before the flare’s peak, it revealed a dark, arch-shaped filament composed of plasma threaded by twisted magnetic field lines. This filament was connected to a cross-shaped magnetic structure that slowly brightened over time. Close-up views showed that new magnetic strands appeared in nearly every image frame, forming and evolving on timescales of just seconds. Each strand twisted like a tightly wound rope, held in place by magnetic forces.
As more of these strands formed and accumulated, the magnetic system grew increasingly unstable. Eventually, the stressed configuration could no longer be maintained. Small reconnection events began to occur, breaking and reforming magnetic connections in rapid succession. These events did not remain isolated. Instead, they spread through the region, triggering additional reconnections in a cascading sequence. This avalanche-like process produced sudden bursts of brightness that signaled escalating energy release.
At 23:29 Universal Time, a particularly strong brightening marked a critical transition. Shortly afterward, part of the dark filament detached and erupted outward, unrolling violently as it moved through the corona. Along its length, bright flashes revealed reconnection sites in extraordinary detail. The main flare erupted around 23:47 UT, but its roots were clearly visible in the earlier, smaller-scale disturbances.
These observations demonstrate that a large solar flare does not need to originate from a single, coherent reconnection event. Instead, it can emerge from many smaller reconnections that interact and reinforce one another. This finding provides direct evidence that the avalanche model—long proposed to explain the collective behavior of many small solar flares—also applies to individual, large flares.
The study also sheds new light on how energy is deposited into the Sun’s atmosphere during a flare. Using combined data from SPICE and STIX, the research team tracked high-energy X-ray emissions that reveal where accelerated particles release their energy. During the September flare, X-ray and ultraviolet emissions were already increasing before the flare peaked. As the avalanche intensified, particle acceleration surged, with electrons reaching speeds of 40 to 50 percent of the speed of light.
One of the most striking discoveries was the observation of fast-moving, ribbon-like streams of glowing plasma descending through the solar atmosphere—described as “raining plasma blobs.” These features are signatures of energy being deposited into lower atmospheric layers as particles accelerated during reconnection collide with denser plasma. Remarkably, this plasma rain continued even after the flare’s most intense phase had subsided, revealing a prolonged energy-release process that had never before been observed with such spatial and temporal resolution.
After the eruption, the solar atmosphere gradually relaxed. EUI images showed the cross-shaped magnetic structure settling into a calmer configuration, while STIX and SPICE recorded cooling plasma and declining particle emissions. PHI captured the effects of the flare on the Sun’s surface, completing a three-dimensional picture of the entire event from its magnetic roots to its energetic aftermath.
These findings mark a major advance in solar physics. They reveal that large solar flares are not instantaneous explosions but the result of rapidly spreading magnetic instabilities that behave like avalanches. The discovery that such cascades can accelerate particles to extremely high energies challenges existing models and highlights the need for even more detailed observations. As Pradeep Chitta notes, future missions with higher-resolution X-ray imaging will be essential to fully disentangle these complex processes.
By uncovering the hidden dynamics at the birth of a solar flare, Solar Orbiter has brought scientists closer to predicting these powerful events and mitigating their effects on Earth. In doing so, it has transformed our understanding of how the Sun releases its immense magnetic energy—and how small changes can unleash extraordinary cosmic storms.
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