We examine the evolution of magnetized, differentially rotating buoyant ele
ments ejected through the surface of an accretion disk into an unmagnetized
ambient medium, using axisymmetric magnetohydrodynamic calculations. The e
volution occurs in three distinct stages. First, angular momentum transfer
along radial magnetic field lines allows part of each element to plunge tow
ard the rotation axis. Next, the vertical gradient in total pressure accele
rates some of the material at the axis upward to escape speed, forming a je
t collimated by an azimuthal field. Finally, material near the base of the
jet is brought close to solid-body rotation by Lorentz forces, the jet ceas
es, and material subsequently ejected through the disk surface angles away
from the axis and enters a magnetocentrifugal flow. Jets are produced over
a large range in injection and Alfven speeds, while the magnetocentrifugal
flows reach escape speed only when mass flux per field line is low. This me
chanism may be useful in explaining the speeds, variability, and mass flow
rates of jets and winds from protostars and T Tauri stars.