Two methods for objective analysis of wind profiler data in time-heigh
t space are proposed and compared. One is a straightforward adaptation
of a procedure developed by Doswell for introducing time continuity i
nto a sequence of spatial analyses. The second technique, named the co
rrelation method, introduces a new rationale for selection of the Barn
es filter parameter that is based on knowledge of the statistical stru
cture of wind profiler data. The advantages and disadvantages of each
method are discussed. It is noted that the correlation method, in prin
ciple, allows the deduction of consistent sampling intervals in time a
nd space for the most dominant phenomena resolved by the data provided
by a given atmospheric observing system. It is recommended that an ob
jective analysis of wind profiler data be performed before single- or
multiprofiler kinematic calculations are made. In addition, it is show
n that the positions of extrema in kinematic quantities computed from
profiler triangles are relatively insensitive to the number of passes
used in the analysis procedures. In fact, it is demonstrated that mult
ipass Barnes-type schemes can overfit the original data, suggesting th
at a one-pass method may be preferable provided that the filter parame
ter is selected property.