Constant sets for several turbulence closure models, based on data for
the atmospheric boundary layer, are proposed. They differ from those
currently used in engineering situations but are self-consistent and t
uned to represent atmospheric boundary-layer turbulence. The proposed
constant sets are tested in a simple, one-dimensional, neutrally-strat
ified planetary boundary-layer flow over a horizontally homogeneous an
d aerodynamically rough flat surface. Comparisons of model results wit
h similarity theory and large-eddy simulation show promise for improvi
ng boundary-layer predictions.