There are several successful techniques for removing relatively high-f
requency ''noise'' due to propagating inertial-gravitational waves in
model forecasts. Not all behavior that is sometimes considered noise i
s necessarily spurious, however, including that due to tidal forcing.
Published evidence of the natural existence of high-frequency behavior
within numerical weather prediction and general circulation models is
briefly reviewed and some additional evidence with yet another model
is introduced. In this new model, the existence of local diabatic bala
nces is also examined. Imposing balances or filters at scales where hi
gh-frequency oscillations are naturally and realistically occuring cau
ses errors which may become more significant as we demand more accurat
e models and atmospheric analyses. The intention of this paper is to s
timulate further research into the naturally occuring high-frequency b
ehavior in numerical models, as well as in the atmosphere, for the pur
pose of improving both models and atmospheric analyses.