We examine the impact of diurnal variability on the synoptic behavior of oz
one observed by the Upper Atmosphere Research Satellite (UARS). Synoptic pr
oducts generated via Kalman filtering are compared against those recovered
via Fast Fourier Synoptic Mapping (FFSM). In FFSM products, tracer anomalie
s defining distinct air masses that originate from different latitudes are
approximately conserved. In Kalman products, the same anomalies and the acc
ompanying air masses are diluted with their surroundings. The origin of the
se differences is traced to the different space-time spectrum inherent to t
he two synoptic products. In the spectrum of Kalman products, high zonal wa
venumbers are exaggerated at low frequency relative to their counterparts i
n FFSM. This pathological behavior appears to result through aliasing from
diurnal variability that is undersampled in the UARS observations. We discu
ss the relevance of these findings to subsequent analyses and to estimating
momentum sources in the middle atmosphere.