Relative Positions of Type I and Type III Solar Metre-Wave Bursts

Abstract

Solar metre-wave noise storms commonly show continuum and short-lived narrow-band bursts (Type I) at high frequencies and fast-drift bursts (Type III) at low frequencies (Malville 1962; Hanasz 1966; Boischot et al. 1970; Moller-Pedersen 1974; see also Figs. 2-3 of this paper). The Type I and Type III emissions have the same sense of polarization (Komesaroff 1958; Suzuki 1978). Impressed by this spectral association, Malville (1962) and Boischot et al. (1970) suggested that the two types of emission might be excited by the same electron stream. However, Type I emission is associated with sunspots and strong photospheric magnetic fields (McCready et al. 1947; Payne-Scott and Little 1951; Le Squeren 1963) and for this reason Kai (1970) suggested that Type I emission arises on strong closed magnetic loops. Type III emission, by contrast, almost certainly arises on open or quasi-open (large-loop) magnetic field lines (Wild et al. 1959, 1963). Thus on these models one would expect Type I and Type III emissions to arise from different magnetic regimes and different areas of the Sun. Kai’s (1970) and Stewart and Labrum’s (1972) Culgoora radioheliograph observations, which suggested that Type I and Type III sources are always separated on the Sun, seemed to clinch the matter. Kai’s model and his statement ‘Type III sources avoid the precise location of Type I storm centres’ gained wide acceptance (e.g. Boischot et al. 1971; Elgaroy 1977; Stewart 1977).

Coronal Radio Bursts: A Signature of Nanoflares?

“…Type I bursts show strong similarities with flare-related decimetric and metric radio spikes and are often associated with the production of electron beams revealed by decametric type III bursts (see Klein 1994 and references therein), 2. Type I and decametric type III sources are, in general, close to each other (Gergely & Kundu 1975;Duncan 1981), 3. On occasion, there is a one-to-one correspondence between individual type I and type III bursts (Aubier, Leblanc, & Møller-Pedersen 1978;Leblanc, Poquérusse, & Aubier 1983).…”