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Analysis of the August 7, 1972 white light flare: Light curves and correlation with hard X-rays
Authors:David M Rust  Frank Hegwer
Institution:1. Sacramento Peak Observatory, Air Force Cambridge Research Laboratories, 88349, Sunspot, N.M., U.S.A.
3. High Altitude Observatory, National Center for Atmospheric Research, 80303, Boulder, Colo., U.S.A.
Abstract:Cinematic, photometric observations of the 3B flare of August 7, 1972 are described in detail. The time resolution was 2 s; the spatial resolution was 1–2″. Flare continuum emissivity at 4950 Å and at 5900 Å correlated closely in time with the 60–100 keV non-thermal X-ray burst intensity. The observed peak emissivity was 1.5 × 1010 erg cm?2 s?1 and the total flare energy in the 3900–6900 Å range was ~1030 erg. From the close temporal correspondence and from the small distance (3″) separating the layers where the visible emission and the X-rays arose, it is argued that the hard X-ray source must have had the same silhouette as the white light flare and that the emission patches had cross-sections of 3–5″. There was also a correlation between the location of the most intense visible emissions near sunspots and the intensity and polarization of the 9.4 GHz radio emission. The flare appeared to show at least three distinct particle acceleration phases: one, occurring at a stationary source and associated with proton acceleration gave a very bluish continuum and reached peak intensity at ~ 1522 UT. At 1523 UT, a faint wave spread out at 40 km s?1 from flare center. The spectrum of the wave was nearly flat in the range 4950–5900 Å. Association of the wave with a slow drift of the microwave emission peak to lower frequencies and with a softening of the X-ray spectrum is interpreted to mean that the particle acceleration process weakened while the region of acceleration expanded. The observations are interpreted with the aid of the flare models of Brown to mean that the same beam of non-thermal electrons that was responsible for the hard X-ray bremsstrahlung also caused the heating of the lower chromosphere that produced the white light flare.
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