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Last modified
7/28/2009 2:39:54 PM
Creation date
4/23/2008 12:04:05 PM
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Template:
Weather Modification
Contract/Permit #
87-1999
Title
Development of Empirical Equations of Ice Crystal Growth Microphysics for Modeling Analysis - Final Report
Date
9/1/1988
Weather Modification - Doc Type
Report
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<br />. <br /> <br />21 <br /> <br />. <br /> <br />unique design of the suspension chamber provided the necessary stability to <br />allow the crystal to be suspended for periods much longer than have been <br />previously achieved. The arrangement of the shelves in the fog chamber <br />helped to ensure that the air would become sufficiently homogeneous with <br />respect to temperature and droplet concentration. The honeycomb, which <br />was made replaceable in case of ice buildup, suppressed turbulence and <br />created a laminar flow. The design of the suction system evenly applied the <br />vacuum force and allowed quick changes of the flow without adjusting the <br />power of the vacuum cleaner. The redesigned pressure cooker produced <br />steam at a constant rate so that the liquid water content remained unchanged <br />during the entire growth period. These and other features eliminated <br />technical problems that prevented long growth periods under controlled <br />conditions, and made the simulation of the natural condition better. <br />However, a few drawbacks persisted that may have affected the <br />usefulness of this study. The pitot tube assembly consistently indicated fall <br />velocities about 20 to 40 percent higher than values obtained by later <br />investigators. This inconsistency, which will be shown later, is probably due <br />to the enhanced flow in the tube above the suspension chamber, which has <br />more cross sectional area. The plaster of paris method probably does not <br />reliably give the liquid water content of the supercooled fog. The difficulty in <br />accurately measuring the mass increase by water accumulation in the much <br />more massive U-shape tube and the possibility of ice formation in the tube <br />created some uncertainty for this method. Complex ice crystal shapes <br />presented difficulties in providing a consistent determination of the <br />dimension at low temperatures. Similarly, thin plates made the <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />. <br />
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