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WSPC03871
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Last modified
1/26/2010 11:36:38 AM
Creation date
10/9/2006 4:14:31 AM
Metadata
Fields
Template:
Water Supply Protection
File Number
8200.700
Description
Colorado River Basin General Publications - Augmentation-Weather Modification
State
CO
Basin
Colorado Mainstem
Water Division
5
Date
3/1/1979
Author
DOI-BOR
Title
Project Skywater - Fiscal Years 1975-78 Report - Atmospheric Resources Management Program
Water Supply Pro - Doc Type
Report/Study
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<br />002555 <br /> <br />CONTRACTOR: Meteorology Research, Inc., Altadena, California <br />CONTRACT NO. 14-06-0-7536 <br />PRINCIPAL INVESTIGATOR: Theodore B. Smith <br />PERIOD: July 1,1974, to June 30,1975 <br />FUNDING: $50,532 <br /> <br />This study evaluated a combination of precipitation-measuring tech- <br />niques. The potential for improving the accuracy and reliability of <br />data was investigated by comparing radar, aircraft, and surface <br />rain gage measurements which could be applied to projects such as <br />HIPLEX. <br /> <br />Findings showed that: <br /> <br />(1) The precision in size distribution measurements of a single <br />l-km sample is relatively low. <br /> <br />(2) The precision of l-km sample measurements decreases slightly <br />with increase in measured rainfall amounts. <br /> <br />(3) For a given size distribution, the reliability in the esti- <br />mates of LWC, R, and Z decreases in the order given. <br /> <br />(4) The RR40 device yields the most reliable measurements of <br />drop size distribution, followed respectively by the PMS and foil <br />(automode) devices for size ranges where measurements can be made <br />by all three instruments. <br /> <br />(5) Compared to the PMS device, the RR40 device yields higher <br />estimates of LWC and R, but lower estimates of Z for particle size <br />ranges where measurements can be made by both instruments. <br /> <br />(6) Negligible biases exist in the estimate of Rand Z between <br />the PMS and foil devices. <br /> <br />(7) The PMS device measures raindrop size distributions more <br />accurately than the other devices. This conclusion is based upon <br />the close correspondence found in the estimates of Rand Z with <br />the respective measurements of the surface gages and the WSR-57 <br />radar. Indirectly, the superior radar estimates of surface <br />rainfall which were based on the R vs. Z relationships derived <br />from the PMS measurements further indicate that the measurements <br />are more accurate. In cont rast, 1 arge di screpanci es in the <br />surface rainfall radar estimates were found based on the R vs. Z <br />relationships derived from measurements by the RR40 device. <br /> <br />Based upon the limited number of storm cases analyzed in this study, <br />it is indicated that: <br /> <br />111-8 <br />
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