Abstract: Accounting for the current knowledge of the PBL structure
and characteristics, a new set of turbulence parameterizations to be used
in atmospheric dispersion models has been derived. That is, expressions
for the vertical profiles of the Lagrangian length scale li
and time scale Ti and diffusion coefficient
Ki (i = u, v, w) are proposed. The classical
statistical diffusion theory, the observed spectral properties and
observed characteristics of energy containing eddies are used to estimate
these parameters. The results of this new method are shown to agree
with previously determined parameterisations.In addition, these
parameterisations give continuous values for the PBL at all elevations
()
and all stability conditions from stable to stable
,
where h and zi are the turbulent heights in
stable or neutral and convective PBL, respectively, and L is
the Monin-Obukhov length. It is the aim of this work to present the
general derivations of these expressions and to show how they
compare to previous results. Finally a validation of the present
parameterisation, obtained by inserting it in a Lagrangian particle
model, will be shown. The Copenhagen data set is simulated. This
data set is a particularly suited for this validation, since most
of the Copenhagen tracer experiments were performed in stability
conditions that are the result of the relative combination of
wind shear and bouyancy forces. As a consequence, a para,eterisation
scheme, able to deal contemporary with neutral and slightly
convective condition, is to be preferred.