Utilizing multiwavelength observations and magnetic field data from SDO/AIA,
SDO/HMI, GOES and RHESSI, we investigate a large-scale ejective solar eruption
of 2014 December 18 from active region NOAA 12241. This event produced a
distinctive three-ribbon flare, having two parallel ribbons corresponding to
the ribbons of a standard two-ribbon flare, and a larger-scale third
quasi-circular ribbon offset from the other two ribbons. There are two
components to this eruptive event. First, a flux rope forms above a
strong-field polarity-inversion line and erupts and grows as the parallel
ribbons turn on, grow, and spread part from that polarity-inversion line; this
evolution is consistent with the tether-cutting-reconnection mechanism for
eruptions. Second, the eruption of the arcade that has the erupting flux rope
in its core under goes magnetic reconnection at the null point of a fan dome
that envelops the erupting arcade, resulting in formation of the quasi-circular
ribbon; this is consistent with the breakout reconnection mechanism for
eruptions. We find that the parallel ribbons begin well before (12 min)
circular ribbon onset, indicating that tether-cutting reconnection (or a
non-ideal MHD instability) initiated this event, rather than breakout
reconnection. The overall setup for this large-scale (circular-ribbon diameter
100000 km) eruption is analogous to that of coronal jets (base size 10000 km),
many of which, according to recent findings, result from eruptions of
small-scale minifilaments. Thus these findings confirm that eruptions of
sheared-core magnetic arcades seated in fan-spine null-point magnetic topology
happen on a wide range of size scales on the Sun.Comment: 36 pages, 14 figures. Accepted for publication in Ap