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Last modified
7/28/2009 2:37:07 PM
Creation date
4/16/2008 10:29:18 AM
Metadata
Fields
Template:
Weather Modification
Contract/Permit #
14-06-D-5640
Project Name
Park Range Atmospheric Water Resources Program
Title
Park Range Atmospheric Water Resources Program - Phase II - Part A
Date
11/15/1966
Weather Modification - Doc Type
Report
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<br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br />I <br /> <br />. 1 1 0 . 1 d' <br />dlameter and containing approximately 2 x () partlc es per gram was lS- <br />pensed from 8300 foot Emerald Mountain using a Metronic s Associates Model <br />5 FP Ae ro sol Generator System, The plume~ was traced by flying the airc raft <br />with re spect to known landmarks on the ground, The real time sensor unit <br />used on the aircraft consists of a vacuum source drawing air and particles <br />into a chamber where particles are activated by the radiation from an ultra- <br />violet lamp, The particles then go through a light trap into a second chamber <br />where their phosphore scence is measured by a sensitive photomultiplier tube. <br />On the last two flights a real time freezing nuclei detector was flown in con- <br />junction with the ZnS (ktector and silve r iodide particle s released simul- <br />taneously with the ZnS particle s. <br /> <br />Calibration <br /> <br />The calibration curves for two units installed in the aircraft used in <br /> <br />over half of these tests is presented in Figure 48, These points came from <br />I basic data of the mass of 2210 pigment collected on a filte r at a known flow <br />rate and for a known inte rval. No data points we re omitted. Also the out- <br />I put of the photomultiplier tube is checked periodically with a radioactive <br />source of known output. <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br />I <br /> <br />Tables VIII and IX summarize the tracer releases of Phase II-Part A. <br /> <br />Tests were made on 24 days and termed Daisy VIII through Daisy XXXI. Lo- <br />cal single-theodolite pibals, radar winds from Mt. Harris and high resolu- <br />tion wind information from the 45 foot level of Emerald Mountain were avai1- <br /> <br />able, For some flights, a vertical temperature profile was obtained from <br />a vortex thermometer in the aircraft, <br /> <br />The result of one test is presented in Figure 49; the plots for other <br />flights will be found in Appendix D, Individual tracks where tracer material <br />was found are listed giving the time, altitude and length along the track where <br />signal was found. A subjective estimate of the location and width of the <br />plume is given, the plume width being defined as that width judged to include <br /> <br />- 81 - <br />
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