A model for the dispersion of Gaussian puffs into the planetary boundary-la
yer is presented. The model relies on the relative diffusion theory in whic
h the rate of expansion of the puff is expressed in terms of the spectral p
roperties of turbulence. A new spectral formulation for the turbulent veloc
ities is used, which is valid for different stability conditions ranging fr
om stable to convective. As a preliminary model evaluation, a continuous pl
ume from the experimental campaign of Copenhagen is reproduced as a superpo
sition of discrete emitted puffs. Comparison between predicted and measured
ground-level concentration data shows a good agreement both for crosswind
integrated concentrations and arcwise maxima.