  We discuss the post-eruptive evolution of a "coronal dimming" based on
observations of the EUV corona from the Solar and Heliospheric Observatory and
the Transition Region and Coronal Explorer. This discussion highlights the
roles played by magnetoconvection-driven magnetic reconnection and the global
magnetic environment of the plasma in the "filling" and apparent motion of the
region following the eruption of a coronal mass ejection (CME). A crucial
element in our understanding of the dimming region evolution is developed by
monitoring the disappearance and reappearance of bright TRACE "moss" around the
active region giving rise to the CME. We interpret the change in the TRACE moss
as a proxy of the changing coronal magnetic field topology behind the CME
front. We infer that the change in global magnetic topology also results in a
shift of energy balance in the process responsible for the production of the
moss emission while the coronal magnetic topology evolves from closed, to open
and back to closed again because, following the eruption, the moss reforms
around the active region in almost exactly its pre-event configuration. As a
result of the moss evolution, combining our discussion with recent
spectroscopic results of an equatorial coronal hole, we suggest that the
interchangeable use of the term "transient coronal hole" to describe a coronal
dimming is more than just a simple coincidence.
