The research, led by Yutong Li of Dezhou University together with colleagues at Dezhou University and Purple Mountain Observatory of the Chinese Academy of Sciences, focuses on a noise storm observed on 24 December 2023. The team combined dynamic radio spectra from the ORFEES spectrograph and the RSTN San Vito station with radio imaging from the Nançay Radioheliograph in France, and paired these with extreme-ultraviolet and magnetogram data from NASA’s Solar Dynamics Observatory, including its Atmospheric Imaging Assembly and Helioseismic and Magnetic Imager. X-ray measurements from the GOES 16 satellite provided the flare timeline. This multiwavelength approach allowed the researchers to track, nearly simultaneously, where the radio source sat in the corona, how its intensity evolved, and what the magnetic field was doing below it.

The radio source turned out to be co-spatial with active region 3529, a magnetically complex area on the solar disk. One of the study’s technically revealing findings concerns the spatial structure of the emission: the source showed frequency-dependent spatial dispersion, meaning that emission at different radio frequencies originated from slightly different locations above the active region. Because the frequency of plasma emission is tied directly to the local electron density, which generally decreases with height in the corona, this dispersion maps out the density stratification of the closed magnetic loops that host the storm. It confirms that the emission arises from electrons trapped within overlying closed structures rather than from freely propagating streams far from the flare site.

The pivotal moment came with an M2.9-class flare from the same active region. As the flare began, the noise-storm intensity did not surge; instead, it dropped. The emission then recovered after the flare’s impulsive phase, and, strikingly, the storm shifted to higher frequencies. In the language of plasma physics, a shift to higher emission frequencies implies a shift to higher electron densities, which in turn suggests that the radio source moved to lower altitudes or that denser plasma became involved in the emission process. The authors interpret this as the signature of the flare-driven magnetic reconfiguration compressing or reshaping the loop system in which the nonthermal electrons were trapped.

What kept the storm alive before the flare? Based on the multiwavelength evidence, the researchers propose that small-scale magnetic reconnection occurring below the storm source, in the period leading up to the eruption, supplied a continuous resupply of nonthermal electrons into the overlying closed magnetic structures. These energetic electrons, injected upward into loops where they became magnetically trapped, sustained the plasma emission that observers record as chains of type I bursts. This picture ties the longevity of noise storms to a steady engine of low-level reconnection rather than to a single impulsive acceleration event, a distinction that has long been debated in solar radio physics.

During the flare itself, the observations captured dramatic evidence of reconnection in progress above the active region. The radio spectra showed type III bursts with bidirectional frequency drifts, the hallmark of electron beams accelerated at a reconnection site and streaming simultaneously upward and downward along magnetic field lines. Because the drift rate of a type III burst encodes the density gradient the beam traverses, the direction and rate of drift reveal where the acceleration happened. Even more telling, the starting frequency of these bidirectional bursts gradually decreased over time. Since a lower starting frequency corresponds to a lower ambient density and therefore a greater height, the authors suggest that the reconnection site itself was moving upward through the corona as the flare progressed, consistent with the rising geometry of an erupting magnetic system.

The flare’s most consequential effect on the noise storm was magnetic rather than radiative. The reconnection event ejected plasma bidirectionally, restructuring the coronal magnetic field above the active region. In the pre-flare configuration, closed loops had provided the magnetic cages that confined nonthermal electrons long enough for them to generate coherent type I emission through plasma processes, a mechanism first outlined in the classic work of Ginzburg and Zhelezniakov in 1958 and refined by many theorists since. Once the flare scrambled those loops, the trapping efficiency collapsed. Electrons that would otherwise have bounced back and forth along closed field lines escaped or were precipitated, the supply of confined energetic particles was interrupted, and the storm was suppressed. The quieting of the radio emission was therefore not a simple absence of energy but the destruction of the magnetic architecture required to store it.

Recovery followed a logical sequence. As post-flare magnetic reconnection subsided and the coronal field relaxed back toward a closed, stable configuration, conditions favorable for electron trapping were re-established. New or re-formed closed loops once again confined nonthermal electrons, the plasma emission mechanism resumed, and the noise storm returned, now at higher frequencies reflecting the altered density structure of the rebuilt loop system. The full cycle, suppression at flare onset, recovery afterward, and a frequency shift tracking the magnetic evolution, provides a coherent narrative in which the flare acts as a modulator of the storm through magnetic restructuring rather than as a simple amplifier or destroyer of radio emission.

The broader significance of the result extends beyond a single event. Noise storms are among the most common manifestations of nonthermal activity in the solar corona, and their occurrence is known to be closely linked to the local magnetic configuration and to the acceleration of nonthermal electrons. By demonstrating that a moderate M-class flare can visibly reorganize the trapping structures of a storm in near real time, the study provides an observational benchmark for models that connect coronal magnetic evolution to radio diagnostics. Because meter-wave radio emission probes densities and heights that are difficult to access with extreme-ultraviolet imaging alone, noise storms serve as sensitive barometers of coronal change, and flare-induced modulations of the kind documented here could become a routine diagnostic for tracking magnetic reconfiguration during eruptions.

The work also carries practical weight for space-weather research. Radio bursts in the meter wavelength range can interfere with terrestrial and satellite communications systems, and understanding what controls their onset, persistence, and cessation improves the physical basis for forecasting disruptive solar radio events. The datasets underpinning the study, including the ORFEES and Nançay Radioheliograph observations available through the Radio Solar dataBase at Nançay, the RSTN San Vito spectra archived by NOAA’s National Centers for Environmental Information, and the SDO and GOES 16 measurements, are all publicly accessible, allowing other researchers to test the proposed sequence of pre-flare electron supply, flare-driven disruption, and post-flare recovery in additional events. If the pattern holds more generally, forecasters may one day read the rise and fall of a noise storm as a live record of magnetic reconnection reshaping the corona above an active region.

Subject of Research: Modulation of type I solar radio noise storms by flare-driven magnetic reconnection above an active region

Article Title: Type I Solar Radio Bursts Modulated by Solar Flares

Article References: Li, Y., Li, C., Tang, Y., Gai, N., Li, Z., Cui, Z., Gao, Y., Wang, Y., Xu, X., & Huo, X. (2026). Type I Solar Radio Bursts Modulated by Solar Flares. Solar Physics, 301(10), Article 150. https://doi.org/10.1007/s11207-026-02736-9

Image Credits: AI Generated

DOI: 10.1007/s11207-026-02736-9

Keywords: type I radio bursts, noise storms, solar flares, magnetic reconnection, solar corona, active region 3529, nonthermal electrons, type III bursts, plasma emission, Nançay Radioheliograph, SDO, space weather