A 3-GHz profiler has been developed by the National Oceanic and Atmospheric
Administration's Aeronomy Laboratory to observe the evolution and vertical
structure of precipitating cloud systems. The profiler is very portable, r
obust, and relatively inexpensive, so that continuous, unattended observati
ons of overhead precipitation can be obtained, even at remote locations. Th
e new profiler is a vertically looking Doppler radar that operates at S ban
d, a commonly used band for scanning weather radars (e.g., WSR-88D). The pr
ofiler has many features in common with the 915-MHz profiler developed at t
he Aeronomy Laboratory during the past decade primarily for measurement of
lower-tropospheric winds in the Tropics. This paper presents a description
of the new profiler and evaluates it in the field in Illinois and Australia
in comparison with UHF lower-tropospheric profilers. In Illinois, the new
profiler was evaluated alongside a collocated 915-MHz profiler at the Flatl
and Atmospheric Observatory. In Australia it Was evaluated alongside a 920-
MHz profiler during the Maritime Continent Thunderstorm Experiment. The res
ults from these campaigns confirm the approximate 20-dB improvement in sens
itivity, as expected for Rayleigh scatter. The results show that the new pr
ofiler provides a substantial improvement in the ability to observe deep cl
oud systems in comparison with the 915-MHz profilers.