2015
DOI: 10.1088/0004-637x/811/1/5
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Destabilization of a Solar Prominence/Filament Field System by a Series of Eight Homologous Eruptive Flares Leading to a Cme

Abstract: Homologous flares are flares that occur repetitively in the same active region, with similar structure and morphology. A series of at least eight homologous flares occurred in active region NOAA 11237 over 16 -17 June 2011. A nearby prominence/filament was rooted in the active region, and situated near the bottom of a coronal cavity. The active region was on the southeast solar limb as seen from SDO/AIA, and on the disk as viewed from STEREO/EUVI-B. The dual perspective allows us to study in detail behavior of… Show more

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Cited by 14 publications
(10 citation statements)
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“…The minifilaments show a slow-rise, followed by a fast-rise as they erupt (MOVIE1 and MOVIE2), analogous to many longer-scale filament eruptions (e.g. Sterling & Moore 2005;Panesar et al 2015). Table 1; (g-i) show HMI magnetograms of the same region.…”
Section: Evolution Of Minifilaments and Jetsmentioning
confidence: 91%
“…The minifilaments show a slow-rise, followed by a fast-rise as they erupt (MOVIE1 and MOVIE2), analogous to many longer-scale filament eruptions (e.g. Sterling & Moore 2005;Panesar et al 2015). Table 1; (g-i) show HMI magnetograms of the same region.…”
Section: Evolution Of Minifilaments and Jetsmentioning
confidence: 91%
“…Moreover, even if one could predict that a certain trigger mechanism will take place, it would still be hard to predict whether an eruption will produce a CME or remains confined (e.g., Moore et al, 2001;Török and Kliem, 2005;Guo et al, 2010) as we know little about the conditions under which trigger mechanisms can succeed in switching on driving mechanisms. In fact, it seems that, at least in some events, several confined eruptions are required before a full eruption can occur (e.g., Panesar et al, 2015;Chintzoglou et al, 2015;Liu et al, 2016).…”
Section: Initiation Mechanisms Of Solar Eruptionsmentioning
confidence: 99%
“…This follows from the finding that a full eruption requires a certain fraction of the active-region flux to reside in the current-carrying, erupting flux (Bobra et al 2008;Savcheva & van Ballegooijen 2009;Su et al 2011). Alternatively, a part of the stabilizing overlying flux can be removed, as conjectured, e.g., in Panesar et al (2015), but this requires a multipolar source structure and an external agent (see, e.g., Török et al 2011), which jointly exist only in a minority of the eruptions. If the flare associated with the confined eruption involves the standard flare reconnection, which can be inferred from the formation of flare ribbons and loops, then the addition of flux is already initiated by the flare reconnection of the confined eruption itself.…”
Section: A General Picture Of Flux Rope Formation By Confined Eruptionsmentioning
confidence: 99%