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Last modified
7/28/2009 2:39:06 PM
Creation date
4/18/2008 10:00:18 AM
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Weather Modification
Title
Design of Physical Cloud Seeding Experiment for the Arizona Atmospheric Modification Research Program - Final Report
Date
2/1/1991
Weather Modification - Doc Type
Report
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<br />EXECUTIVE SUMMARY <br /> <br />This report documents planning for comprehensive physical cloud seeding experiments to be <br />conducted on the Mogollon Rim of Arizona. The goal of these experiments is to validate <br />hypothesized physical processes following seeding, The planning included the development of <br />(1) experimental designs for both ground-based and airborne seeding of winter clouds, (2) analysis <br />approaches to be applied to the resulting measurements, and (3) cost estimates for the overall <br />program. The entire physical experiment program, from equipment procurement and contracting <br />through field observations, final analysis and reporting, would require 5 years. This assumes a <br />separate analysis group will work simultaneously with the field group and that measurement <br />programs will be carried out during years 2 through 4" The total cost of the 5-year program is <br />estimated to be $9.5 million. <br /> <br />Past attempts at physical seeding experiments with winter clouds were reviewed and briefly <br />described. Some common factors affecting either success or failure were identified. For example, <br />airborne identification and tracking of the seeded volume were very important in the successful <br />experiments, especially in the complex airflow near mountains. These factors require that mountain <br />experimental areas be carefully chosen to permit low level aircraft sampling during storms. Changes <br />in ice particle concentration were the most detectable characteristic of seeding at ground level. <br />Frequent monitoring of the silver content of the snowfall helped validate targeting in silver iodide <br />(AgI) seeding experiments. Negative factors included attempts to "piggy-back" physical experiments <br />on statistical designs and inadequate analysis during and between observational programs so that <br />needed design improvements were recognized too late. <br /> <br />The entire Mogollon Rim, from near Flagstaff to the White Mountains on the New Mexico border, <br />was considered in choosing an experimental area for physical seeding experiments. By a process <br />of elimination the "best" target site was determined to be Allen Lake, 60 km south-southeast of <br />Flagstaff. It is near the rim's crest, has few peaks to interfere with low level flight, has good road <br />access and electrical power, and is in a large enough clearing for operation of key instrumentation <br />systems. A Doppler weather radar could be operated north of Allen Lake in a position that would <br />permit scanning from cloud tops to near the ground. The project operations center would be <br />colocated with the radar while project aircraft would be based at Scottsdale. <br /> <br />The various scientific uncertainties concerning Arizona winter clouds are addressed. These include <br />limited knowledge of the spatial and temporal distributions of supercooled liquid water over the rim, <br />and of ice crystal formation, growth and fallout trajectories, especially when many crystals aggregate <br />into large snowflakes. Whether conditions exist such that seeding might sometimes reduce snowfall <br />is an open question. These and other important issues will be investigated during the course of the <br />experimental program. <br /> <br />Several sophisticated observing systems are recommended for use in the physical experiments. <br />These include a microwave radiometer for detection of water vapor and liquid water; a Doppler <br />acoustic sounder to monitor winds in the lowest kilometer; a scanning Doppler radar for storm <br />structure, cloud top, and wind observations; two rawinsonde systems to obtain vertical profiles of <br />wind, temperature, and moisture; and various surface sensors including high resolution precipitation <br />gauges and an ice particle imaging probe. An instrumented cloud physics aircraft would monitor <br />the seeding agent and a variety of cloud characteristics. A seeding aircraft would dispense AgI ice <br />nuclei and also make some cloud measurements. <br /> <br />ill <br />
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