Using data from the extreme ultraviolet imaging telescope (EIT) on SOHO and
the soft X-ray telescope (SXT) on Yohkoh, we examine a series of morpholog
ically homologous solar flares occurring in National Oceanic and Atmospheri
c Administration (NOAA) active region 8210 over May 1-2, 1998. An emerging
flux region (EFR) impacted against a sunspot to the west and next to a coro
nal hole to the east is the source of the repeated flaring. An SXT sigmoid
parallels the EFR's neutral line at the site of the initial flaring in soft
X rays. In EIT each flaring episode begins with the formation of a crinkle
pattern external to the EFR. These EIT crinkles move out from, and then in
toward, the EFR with velocities similar to 20 km s(-1). A shrinking and ex
pansion of the width of the coronal hole coincides with the crinkle activit
y, and generation and evolution of a postflare loop system begins near the
time of crinkle formation. Using a schematic based on magnetograms of the r
egion, we suggest that these observations are consistent with the standard
reconnection-based model for solar eruptions but are modified by the presen
ce of the additional magnetic fields of the sunspot and coronal hole. In th
e schematic, internal reconnection begins inside of the EFR-associated fiel
ds, unleashing a flare, postflare loops, and a coronal mass ejection (CME).
External reconnection, first occurring between the escaping CME and the co
ronal hole field and second occurring between fields formed as a result of
the first external reconnection, results in the EIT crinkles and changes in
the coronal hole boundary. By the end of the second external reconnection,
the initial setup is reinstated; thus the sequence can repeat, resulting i
n morphologically homologous eruptions. Our inferred magnetic topology is s
imilar to that suggested in the "breakout model" of eruptions [Antiochos, 1
998], although we cannot determine if our eruptions are released primarily
by the breakout mechanism (external reconnection) or, alternatively, primar
ily by the internal reconnection.