Plasma with a temperature close to the chromospheric one is ejected in solar eruptions. Such plasma can occult some part of emission of compact sources in active regions as well as quiet solar areas. Absorption phenomena can be observed in the microwave range as the so-called "negative bursts" and also in the He II 304Å line. The paper considers three eruptive events associated with rather powerful flares. Parameters of absorbing material of an eruption are estimated from multi-frequency records of a "negative burst" in one event. "Destruction" of an eruptive filament and its dispersion like a cloud over a huge area observed as a giant depression of the 304Å line emission has been revealed in a few events. One such event out of three ones known to us is considered in this paper. Another event is a possibility. PACS numbers: 96.60.qf
IntroductionProminences (filaments) in many solar events erupt and draw away from the Sun as parts of Coronal Mass Ejections (CMEs). Partial plasma flows from an eruptive prominence along its legs down to the solar surface are often observed. "Failed" eruptions are also known, when an eruptive prominence or filament after lift-off rapidly decelerates and falls at nearly the same position 1 where it was located before the eruption [1]. Observations of the 18.11.2003 eruptive event with the CORONAS-F/SPIRIT telescope in the He II 304Å line revealed one more scenario. An eruptive filament disintegrated to form a Y-like cloud, flew above the solar surface a distance of more than the solar radius and, probably, landed far from the eruption site [2,3]. A similar anomalous eruption was observed in the 13.07.2004 event [4]. Detailed observations of this event revealed an eruption from an active region of a compact filament and its subsequent dispersion over a huge area comparable with a quarter of the visible solar disk. These events were accompanied with impulsive flares.Eruptive events associated with flares produce various phenomena of different temporal and spatial scales. These phenomena are observed in diverse spectral domains (see [5]). These are flare arcades whose emission is registered from X-rays up to radio waves. Other phenomena are dimmings, i.e., depressions of soft X-ray and extreme ultraviolet (EUV) emissions that reach significant sizes and exist from a few hours up to two days. The major cause of quasi-stationary dimmings is plasma density decrease due to expansion of eruptive structures. Shock waves excited by impulsive eruptions from active regions are manifest in Moreton waves and some "EUV waves" (or "EIT waves"). Propagation of shock waves is traced from slowly drifting type II bursts at metric and decimetric waves. Most likely, shock waves form leading edges of fast CMEs, especially decelerating ones [6].Erupted plasmas with nearly chromospheric temperatures can occult some part of the solar emission and absorb its detectable fraction. Absorption phenomena are observed in various emission ranges. Erupted plasmas show up in the Hα line mainly as surges, which ...