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<br />16 <br /> <br />likely that .only.a ~raction of this amount could be realized. <br />~.~............-......,...~-..-- <br /> <br />:.- <br /> <br />"'-~9\!!I <br /> <br />To put this value in perspective, consider it in terms of the <br /> <br />average 70 year annual runoff.~~~:o..t~e Beaver River (which drains the <br />~".'''~''':'''''''_'''':,--...=..._..c_ '- _ ~ -....;'''"--'_.... <br /> <br />~ <br /> <br />target area) -- 38,250 acre feet. Cloud seeding during appropriate <br /> <br />"- <br />periods of storms with the ideal conditions described above and with 100 <br /> <br />percent efficiency would have produced a 45 percent increase over the <br /> <br />-- <br /> <br />natural runoff. <br /> <br />/30/8 <br />- <br /> <br />"3e z..~O - <br />- FEBRUARY 8-9, <br /> <br />::s'i% <br /> <br />III. CASE STUDY STORM <br /> <br />1985 <br /> <br />A. Overview <br /> <br />The Objective of this analysis was to assemble a case study <br /> <br />description of one STORM event and to intercompare the observations that <br /> <br />were obtained in order to arrive at a better understanding of the <br /> <br />.~ <br /> <br />precipitation formation processes and the potential for cloud seeding <br /> <br />opportunities. A large variety of measurements were made, including: <br /> <br />dual wavelength radiometer, Ka-band radar, C-band radar, rawinsondes, <br /> <br />surface observations of precipitation type and amount, LIDAR, and the <br /> <br />icing probe. <br /> <br />The February 8-9 STORM was a large scale cold frontal system which <br /> <br />went through several different phases of structure and precipitation <br /> <br />processes. The additional orographic component could not be readily <br /> <br />differentiated from the large scale storm. This one STORM provided about <br /> <br />13 percent of the total precipitation during the two-month project. <br /> <br />Some positive potential for cloud seeding was likely because <br /> <br />considerable supercooled liquid water was present during both light and <br /> <br />heavy precipitation periods, and cloud temperatures were generally in <br /> <br />the range -5 to -20oC. <br />