An Eulerian inert tracer dispersion model was developed for use in associat
ion with a meteorological model. A truly horizontal diffusion scheme was us
ed in a terrain-following co-ordinate system and a "one-side" diffusion sch
eme was used at terrain bounded grid points. An implicit scheme was used fo
r vertical diffusion to ease the time step restriction imposed by high-reso
lution vertical levels. The model was incorporated into a mesoscale meteoro
logical model and inert tracer distribution in and around a partially ideal
ised urban source area was simulated. Comparison with observations showed t
hat the simulations captured the diurnal variation of tracer concentration
well. The magnitudes of the concentrations in the urban area varied inverse
ly with the urban heat Bur, largely due to the effect the latter had on the
depth of the mixing layer. The horizontal distribution of the tracer was i
nfluenced by the orographically induced wind field at the mesoscale. The tr
acer model may be incorporated into other meteorological models with slight
modification or run as an independent model as long as suitable wind field
and vertical diffusivity are specified. (C) 2000 Elsevier Science Ltd. All
rights reserved.