The prediction models for tropospheric scintillation on earth-satellite pat
hs from Karasawa, Yamada, and Allnutt and ITU-R are compared with measureme
nt results from satellite links in Europe, the United States, and Japan at
frequencies from 7 to 30 GHz and elevation angles of 3 to 33 degrees. The e
xisting prediction models relate the long-term average scintillation intens
ity to the wet term of refractivity at ground level. The comparison shows t
hat the seasonal variation of scintillation intensity is well predicted by
this relation, but for the annual average some additional meteorological in
formation is needed. A much better agreement with measurement results is fo
und when a parameter representing the average water content of heavy clouds
is incorporated. This confirms the assumption that scintillation is, at le
ast partly, associated with turbulence inside clouds. The asymmetry between
the distributions of signal fade and enhancement can also be explained by
turbulence inside clouds. The asymmetry depends on the intensity of the sci
ntillation, which is consistent with the theory assuming a thin layer of cl
oudy turbulence. A new model based on this theory predicts the distribution
s of signal fade and enhancement significantly better.