The purpose of this paper is to describe the latest version of a wake-vorte
x eddy-dissipation model devised by T. Sarpkaya ("New Model for Vortex Deca
y in the Atmosphere," Journal of Aircraft, Vol. 37, No. 1, 2000, pp. 53-61.
) and to compare its predictions with lidar observations obtained at Memphi
s and Dallas/Fort Worth airports. The model simulates the evolution of airc
raft-generated trailing vortices in an atmospheric environment defined by v
ertical profiles of potential temperature, eddy-dissipation rate, and cross
wind. Visual and quantitative comparisons of the time histories of altitude
, circulation, and lateral position of predicted and measured vortices are
presented.