During the year-long Surface Heat Budget of the Arctic Experiment (1997-199
8) the NOAA Environmental Technology Laboratory operated a 35-GHz cloud rad
ar and the DOE Atmospheric Radiation Measurement Program operated a suite o
f radiometers at an ice station frozen into the drifting ice pack of the Ar
ctic Ocean. The NASA/FIRE Arctic Clouds Experiment took place during April-
July 1998, with the primary goal of investigating cloud microphysical, geom
etrical, and radiative properties with aircraft and surface-based measureme
nts. In this paper, retrieval techniques are utilized which combine the rad
ar and radiometer measurements to compute height-dependent water contents a
nd hydrometeor sizes for all-ice and all-liquid clouds. For the spring and
early summer period, all-ice cloud retrievals showed a mean particle diamet
er of about 60 mum and ice water contents up to 0.1 g/m(3), with the maximu
m sizes and water contents at approximately one fifth of the cloud depth fr
om the cloud base. The all-liquid cloud retrievals had a mean effective par
ticle radius of 7.4 mum, liquid water contents up to 0.7 g/m(3), and a mean
droplet concentration of 54 cm(-3). Maximum retrieved liquid drop sizes, w
ater contents, and concentrations occurred at three fifths of the cloud dep
th from the cloud base. As a measure of how representative the FIRE-ACE air
craft flight days were of the April-July months in general, retrieval stati
stics for flight-day clouds are compared to the mean retrieval statistics.
From the retrieval perspective the ice particle sizes and water contents on
flight days were similar to 30% larger than the mean retrieved values for
the April-July months. Retrieved liquid cloud parameters during flight days
were all about 20% smaller. All-ice and/or all-liquid clouds acceptable fo
r these retrieval techniques were observed about 34% of the time clouds wer
e present; at all other times, mixed-phase clouds precluded the use of thes
e single-phase retrieval techniques.