Cloud water contents and hydrometeor sizes during the FIRE Arctic Clouds Experiment

Citation
Md. Shupe et al., Cloud water contents and hydrometeor sizes during the FIRE Arctic Clouds Experiment, J GEO RES-A, 106(D14), 2001, pp. 15015-15028
Citations number
27
Categorie Soggetti
Earth Sciences
Volume
106
Issue
D14
Year of publication
2001
Pages
15015 - 15028
Database
ISI
SICI code
Abstract
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.