Numerical simulations are used to determine the influence of the nonlocal a
nd local interactions on the intermittency corrections in the scaling prope
rties of three-dimensional turbulence. We show that neglect of local intera
ctions leads to an enhanced small-scale energy spectrum and to a significan
tly larger number of very intense vortices ("tornadoes") and stronger inter
mittency (e.g., wider tails in the probability distribution functions of ve
locity increments and greater anomalous corrections). On the other hand, ne
glect of the nonlocal interactions results in even stronger small-scale spe
ctrum but significantly weaker intermittency. Thus, the amount of intermitt
ency is not determined just by the mean intensity of the small scales, but
it is nontrivially shaped by the nature of the scale interactions. Namely,
the role of the nonlocal interactions is to generate intense vortices respo
nsible for intermittency and the role of the local interactions is to dissi
pate them. Based on these observations, a new model of turbulence is propos
ed, in which nonlocal (rapid distortion theory-like) interactions couple la
rge and small scale via a multiplicative process with additive noise and a
turbulent viscosity models the local interactions. This model is used to de
rive a simple version of the Langevin equations for small-scale velocity in
crements. A Gaussian approximation for the large scale fields yields the Fo
kker-Planck equation for the probability distribution function of the veloc
ity increments. Steady state solutions of this equation allows one to quali
tatively explain the anomalous corrections and the skewness generation alon
g scale. A crucial role is played by the correlation between the additive a
nd the multiplicative (large-scale) process, featuring the correlation betw
een the stretching and the vorticity. (C) 2001 American Institute of Physic
s.