The structure of solar radio noise storms
Claude Mercier, Prasad Subramanian, Gilbert Chambe, P. Janardhan

TL;DR
This study uses high-resolution solar radio imaging to analyze the structure and size of noise storms, revealing their stable core sizes, density-related origins, and challenging classical models of their vertical structure.
Contribution
The paper provides new high-resolution observations of solar noise storms, revealing stable core sizes, their altitude dependence on frequency, and insights into scattering effects and vertical structure.
Findings
Core sizes are stable over an hour, with a minimum of 31-35 arcsec.
Noise storms originate at densities higher than the ambient corona.
Observed sizes suggest scattering effects may be overestimated in past models.
Abstract
The Nan\c{c}ay Radioheliograph (NRH) routinely produces snapshot images of the full sun at frequencies between 150 and 450 MHz, with typical resolution 3 arcmin and time cadence 0.2 s. Combining visibilities from the NRH and from the Giant Meterwave Radio Telescope (GMRT) allows us to produce images of the sun at 236 or 327 MHz, with a large FOV, high resolution and time cadence. We seek to investigate the structure of noise storms (the most common non-thermal solar radio emission). We focus on the relation of position and altitude of noise storms with the observing frequency and on the lower limit of their sizes. We present results for noise storms on four days. The results consist of an extended halo and of one or several compact cores with relative intensity changing over a few seconds. We found that core sizes can be almost stable over one hour, with a minimum in the range 31-35…
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