HR: 1340h
AN: A23C-0959    [Abstracts]
TI: Characterization of Mixed-Phase Clouds in the Laboratory
AU: * Foster, T C
EM: tfoster@calpoly.edu
AF: Physics Department, California Polytechnic State University, San Luis Obispo, CA 93405 United States
AU: Hallett, J
EM: hallett@dri.edu
AF: Desert Research Institute, 2215 Raggio Parkway, Reno, NV 89512 United States
AB: A technique was developed in which a mixed-phase cloud of controllable ice and water content is created. First a freezer filled with a water droplet cloud becomes supercooled. Then, in an isolated small volume of the freezer, an adjustable adiabatic expansion locally nucleates ice. Finally the two regions of the cloud are vigorously stirred together producing a mixed-phase cloud throughout the chamber. At this point the water droplets evaporate and the crystals grow at a slow measurable rate, until a fully glaciated cloud results. Experiments were carried out at temperatures near -20 C in a standard top-opening chest freezer. A cloud of supercooled water droplets several micrometers in diameter was produced by a commercial ultrasonic nebulizer. Ice was nucleated using the discharge of an empty compressed air pistol pumped to different initial pressures. In that process high-pressure room temperature air in the pistol expands adiabatically, cooling the air enough to nucleate water droplets which then freeze homogeneously if sufficiently cold. The freezer was partitioned with thick movable walls of foam material to isolate the ice cloud in a small volume of the freezer before mixing occurs. Clouds of supercooled water droplets or of ice particles are readily produced and examined in collimated white light beams. They look similar visually in some cases although normally large crystals with flat reflecting surfaces clearly differ due to the flashes of reflected light. When the pistol is discharged into the supercooled water cloud, it displays a distinct hazy bluish "plume." But discharge into the ice particle cloud leaves no such plume: that discharge only mixes the particles present. This discharge is a test of glaciation in our initially mixed freezer cloud. A visible plume indicates that supercooled water remains in the cloud and no plume indicates the cloud is entirely ice at a high concentration. Our first unsuccessful experiments were done with the freezer partitioned in two halves with one section nucleated by a liquid nitrogen cooled wire. When the halves were mixed the glaciation time was too short to measure, due to the fact that the nucleating process produced too many ice particles initially and this resulted in too rapid an evaporation-deposition process. Subsequently the freezer was partitioned into a large volume containing a high LWC cloud of supercooled water and a small volume of low LWC cloud. The smaller volume was nucleated with a low initial pressure air pistol discharge. (The number of ice particles produced in such a nucleation process can be determined by discharging the pistol into a full freezer of supercooled cloud, rapidly stirring the cloud, and measuring the average ice particle separation.) Then the barrier is removed and the clouds mixed and at a measured time later the pistol is discharged a second time, at a higher initial pressure, to test for the cloud glaciation state. Theory associated with the evolution of the mixed cloud, in which water droplets evaporate and crystals grow, is well known and equations developed using the Bergeron-Findeison theory are used in this study. Glaciation times are measured for different initial ice particle concentration and LWC. They are long, of the order of tens of seconds, for low concentrations of ice particles in the initial mixed cloud and large LWC. This is consistent with theory. It is suggested that the technique we employ may prove useful on a small scale in determining the amount of glaciation of natural clouds.
DE: 3300 ATMOSPHERIC PROCESSES
DE: 3311 Clouds and aerosols
SC: Atmospheric Sciences [A]
MN: Fall Meeting 2005