Using an eruptive flare model based on a loss of equilibrium in a coro
nal flux rope, we show that the average horizontal component of the ph
otospheric field does not necessarily become more like a potential (cu
rrent-free) field immediately after the eruption begins. Therefore, re
cent observations showing that the average horizontal field becomes le
ss potential during the impulsive phase of a flare do not necessarily
imply that the magnetic energy in the corona has increased as has some
times been assumed. The flux-rope model which we use also has relevanc
e to coronal mass ejections. It differs from previous models because e
ruption is triggered solely by the converging motion of two photospher
ic field sources that lie below the coronal flux rope. Because this bo
undary condition is much simpler than that used in previous formulatio
ns, this particular version of the model is especially well-suited for
two-dimensional numerical simulations with translational symmetry.