Type-II radio bursts are typically observed below ∼ 400 MHz and are characterized by the narrowband, slowly drifting fundamental and harmonic structures. Here we report an unusual high-frequency wide-band type-II burst with a starting frequency as high as 670 MHz and an instantaneous bandwidth as wide as ∼ 300 MHz. We used radio imaging from the Nançay Radio Heliograph, spectroscopic data from ORFEES, extreme-ultraviolet (EUV) observations from Solar Dynamics Observatory, and white-light observations from LASCO to determine the nature and origin of the observed radio burst as well as its propagation in the corona. The estimated average spectral drift is ∼ 2. 18 MHz s^-1, its mean duration at each frequency is ∼ 3 min, and the maximum brightness temperature can exceed 10¹1 to 10¹2 K. According to the simultaneous EUV and radio imaging data, the radio sources are distributed over a relatively broad region centered on a dip in the nose front of the shock-like EUV wave structure. The dip is likely caused by the strong interaction of the eruption with the overlying closed dense loops that are enclosed by the large-scale streamer structure, indicating that the type-II burst originates from coronal mass ejection shocks interacting with dense, closed-loop structures. The observations suggest that the unusual wide-band high-frequency type-II radio burst originates from a dense streamer region in the corona; this is further evidenced by an EUV shock-like structure that steepens very close to the solar surface, at ∼ 1. 23 R_⊙, and the fact that the type-II radio source coincides with the shock dip. The wide-band feature is due to the source stemming from a region with significant density variations and not due to the intensity variations across the shock structure.
Vasanth et al. (Thu,) studied this question.