Radar measurement uncertainties associated with storm top, cloud top,
and other height measurements are well recognized; however, the author
s feel the resulting impacts on the trends of storm features are not a
s well documented or understood by some users of the WSR-88D system. D
etailed examination of radar-measured life cycles of thunderstorms occ
urring in Arizona indicates substantial limitations in the WSR-88D's c
apability to depict certain aspects of storm-height attribute evolutio
n (i.e., life cycle) accurately. These inherent limitations are illust
rated using a vertical reflectivity structure model for the life cycle
of a simple, ''single-pulse'' thunderstorm. The life cycle of this si
mple storm is ''scanned'' at varying ranges and translation speeds. Th
e results show that radar-determined trends are often substantially di
fferent from those of the model storm and that in extreme cases the ra
dar-detected storm and the model storm can have trends in storm-top he
ight of opposite sign. Caution is clearly required by both the operati
onal and research users of some products derived from operational WSR-
88D data.