We have utilized large-eddy simulations to simulate the transition fro
m an aircraft wake dominated by the interaction of vortex-pair dynamic
s and engine plume buoyancy to one dominated by atmospheric dispersion
. Our investigation concentrates on the period from a few seconds to s
everal minutes after the wake is generated, during which the essential
ly two-dimensional vortex-pair is broken up into a variety of three-di
mensional eddies. Our initial conditions are taken from near-wake simu
lations for three aircraft: the B-737, the B-747, and the ER-2. Compar
isons of our simulations, for conditions representative of the atmosph
ere in the upper troposphere and the lower stratosphere, with wake pho
tographs taken from the ground show very similar features. In the abse
nce of wind shear, the vortex pair go through a linking instability th
at is affected both by engine buoyancy and ambient turbulence. The res
ultant series of vortex rings continue to descend, leaving the wake wi
th the appearance of a series of suspended puffs. When the mean atmosp
heric shear is sufficiently large, the ambient vorticity can erode one
member of the vortex pair, leading to a breakup mode with a much shor
ter wavelength.