This paper examines the effect of streamwise diffusion on the distribu
tion of mean scalar concentrations associated with surface releases in
the atmospheric surface layer. We use a two-dimensional (2D) (streamw
ise-vertical) Lagrangian stochastic model to simulate dispersion. Befo
re applying the model, we test its validity by comparing model results
of mean concentration and streamwise mass flux density with wind tunn
el data reported by Raupach and Legg (1983, Journal of Fluid Mechanics
136, 111-137). The results from simulations conducted with the 2D sto
chastic model indicated that: (1) inclusion of streamwise dispersion i
n a model provides a plausible explanation for the ''-2'' asymptote ob
served in Project Prairie Grass for the fall-off of ground-level conce
ntrations under unstable conditions, and (2) streamwise diffusion play
s a minor role in dispersion under stable conditions. (C) 1998 Elsevie
r Science Ltd. All rights reserved.