We show that power spectra of granulation images or velocity fields ca
nnot be compared meaningfully with spectra from theoretical models bas
ed on turbulent cascades. The small scale power in these images is due
almost entirely to the sharp edges between granules and intergranular
lanes, not to turbulence in the usual sense. This is demonstrated wit
h a number of experiments with result from numerical simulations, and
with simpler synthetic data with power spectra similar to that of gran
ulation. The reason for the seemingly laminar behavior of the granulat
ion flow, in spite of the high Reynolds numbers involved, is the influ
ence of stratification on the local ratio of turbulence to bulk flow.
The rapid expansion of upflows, their deep origin and near-adiabatic s
tratification lead to low levels of turbulence in the overturning flui
d at the surface. Higher levels of turbulence are expected in the conv
erging flows near downdrafts, but mostly at scales that are below curr
ent observational resolution limits, and contributing relatively littl
e to the total convective flux and to spectral line broadening.