We discuss the structure of the reconnection layer as recorded by ISEE
2 during an outbound crossing of the dayside, northern magnetopause o
n October 29, 1979. Besides a rotational discontinuity, this crossing
shows slow mode shock structure. We interpret this event theoretically
in terms of magnetic field line reconnection based on a pulse-like Pe
tschek-type model, rather than in terms of steady state reconnection o
n a moving magnetopause. Our model is generalized through the introduc
tion of a space-and time-varying reconnection rate. Furthermore, the m
agnetic fields and velocities on either side of the magnetopause curre
nt sheet may have arbitrary strength and orientation with respect to e
ach other; additionally, the densities on either side of the current s
heet may be different in general. Using boundary/initial conditions fr
om the spacecraft data, we calculate the temporal/spatial behavior of
all reconnection-associated structures. In particular, having chosen a
suitable trajectory through the magnetopause, we consider the tempora
l behavior of the magnetic field and plasma parameters as these reconn
ection-associated events pass by. The results reproduce the behavior o
f the data reasonably well.