The question of whether a temperature mixing layer evolves in a self-simila
r manner is of importance in developing and validating theories about scala
r mixing. The simplicity of the flow encourages the thought that it is self
-similar, but several laboratory experiments at moderate Peclet numbers hav
e found inconsistencies with self-similar behavior. The experimentalists ar
e limited, however, by the length of the wind tunnels and by difficulties i
n aligning the virtual origins of the scalar and velocity fields. Direct nu
merical simulations virtually eliminate both these problems, and large-eddy
simulations add the ability to study an approximation to the case of an in
finite Peclet number. These two simulation techniques are used in this pape
r to show that the mixing layer at a moderate Peclet number very nearly evo
lves with a single length and time scale, and that behavior consistent with
self-similarity is observed in the case of an infinite Peclet number. In a
ddition, the results show that direct numerical simulations can accurately
reproduce the data from wind tunnel experiments downstream of a turbulence
grid, and that large-eddy simulations are a valuable research tool for stud
ying the large-scale characteristics of mixing. (C) 2000 American Institute
of Physics. [S1070-6631(00)00801-1].