Abstract
The results of a study of the fine structure of an image of a microwave radiation source, which is usually located in the solar atmosphere above active regions, are presented. The source is equal to the whole active region in size (2–5 arcmin); it is conventionally called a “halo”. Observations of two active regions of different morphological types (NOAA 7123, 1992 and NOAA 11142, 2011) with a high angular resolution (2–5 arcsec) were used. According to these observations, the majority (>50%) of the halo consists of diffused optically transparent thermal plasma. A brighter underlying region shines through it; in the case of NOAA 7123, this region looks like a two-ribbon structure along the magnetic field neutral line with a radiation depression along the Hα filament. In the case of NOAA 11142, the halo brightening regions are associated with regions of cluster of small sunspots and pores. The conclusion is drawn that the brighter component of the halo is due to the cyclotron radiation of coronal plasma in a relatively weak magnetic field (600–800 Gs).
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Peterova, N.G., Opeikina, L.V. & Topchilo, N.A. “Halo” type sources from microwave observations with high angular resolution. Geomagn. Aeron. 54, 1053–1057 (2014). https://doi.org/10.1134/S0016793214080155
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DOI: https://doi.org/10.1134/S0016793214080155