We compare the predictions of incompressible, analytic reconnection theory
with numerical simulations performed using a time-dependent, doubly periodi
c code. The properties of the simulated current sheets are shown to be in g
ood quantitative agreement with recent planar analytic reconnection solutio
ns based on X-point merging driven by sheared incompressible flows. We conc
lude that the analytic treatment is not seriously compromised by assuming a
n open flow geometry and a one-dimensional current layer. The analytic mode
ls, when augmented by nonlinear saturation arguments, are also shown to pro
vide resistive scaling laws that accord well with computed merging rates. B
y way of contrast, we have found no computational evidence for the osculati
on of separatrices in current sheets, even for the case of classical head-o
n reconnection in which all shearing flows are absent. We attribute this to
the dynamic nature of the simulated current sheet. Our simulations provide
some evidence that dynamic current sheets can break up into magnetic islan
ds, but whether this fragmentation can be attributed to the tearing mode in
stability remains unclear.