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<br />. LEFT <br /> <br />~~ <br /> <br />MIS COpy SHEET <br /> <br />'I; ;': ,;11" I {' 1,. ',";11(' {; ;"1 <br />-/ /,1 ,d i i., !11 ':d':': , ;:( <br /> <br />i'f:llll1'~"TipL .;1J'-'111d hr Iv!).',! Iii) ;'n <br />"!,'li .llld ri\:hf r'.J)"~,ill';. Il() dill <br />u;':c('f>c1 mnr;<l_n. <br /> <br />;: f(;;fT <br /> <br />~ <br /> <br />brganization (WMO, -1986) haspubf1she(fa-setO'f-.-~---- dispensers are small and targeting difficult in complex <br />guidelines for decision makers on the utility of cloud terrain should be considered. Marler (1992, this <br />seeding. It takes a cautious l'Osition toward cloud seeding conference) describes some recent studies in targeting <br />for precipitation enhancement as unequivocal proof of the effectiveness over Lake Almanor that begin to address this <br />efficacy of this technology is lacking. The AMS Policy question. <br />Statement, previously mentioned, takes a less conservative <br />position than the ~O, perhaps because the authors <br />include both scientists as well as members of the <br />operational weather modification community. <br /> <br />The American Society of Civil Engineers (ASCE, <br />1983), of which many water resources managers are <br />members, has published guidelines for the use of cloud <br />seeding to augment precipitation. They conclude that cloud <br />seeding may produce a 5 to 20 % increase in precipitation if <br />the proper planning is performed. The guidelines call for <br />not only an economic assessment, but also an <br />environmental and societal assessment of the benefits and <br />liabilities of cloud seeding. The assessment would be <br />followed by a design study that would 1) account for the <br />meteorological and topographical features of the target <br />area, 2) define suspension criteria for terminating seeding <br />during threatening weather, 3) define evaluation criteria for <br />assessing seeding effects and 4) require monitoring for <br />environmental impacts. Although excellent guidelines, they <br />are rarely implemented when projects begin. <br /> <br />Finally there is the Weather Modification <br />Association Statement of Capability (WMA, 1991). <br />Approved by many of the same individuals as the ASCE <br />document, it provides the same optimistic conclusions and <br />recommendations. <br /> <br />, <br /> <br />Shortly after Vonnegut's development of AgI as an <br />effective nucleation aerosol and a generator to dispense it <br />in-cloud, utility companies in California began seeding to <br />augment the winter snowpack in an effort to increase <br />hydro-electric power generation during spring runoff. Four <br />winter seeding programs that were initiated in the 1950's in <br />California for snowpack augmentation (the upper San <br />Joaquin, 1951, by Southern California Edison, the Kings <br />River project, 1955, sponsored by the Kings River <br />Conservation District, and the Mokelumne/Stanislaus and <br />Lake Almanor Programs, 1953 and 1954 respectively, both <br />sponsored by Pacific Gas and Electric (pG&E)) are still in <br />existence today. <br /> <br />Statistical analysis of the Kings River and Almanor <br />programs (Henderson, 1966; Mooney and Lunn, 1969) <br />suggests that seeding has produced about 5 to 10% <br />additional precipitation per season for the watersheds being <br />treated. It is obvious that the spc,nsors of these programs <br />are convinced that the technology being used to seed clouds <br />is satisfactory, in that it has not changed materially in <br />decades. Changes in AgI solutions for better combustion <br />and nucleation efficiency, and more reliable and better <br />located seeding generators have been the only substantive <br />modifications. Unfortunately, results of recently completed <br />research programs such as the Sierra Cooperative Pilot <br />Project (SCPP) (Reynolds and Dennis, 1986) have not <br />materially influenced the conduct of these ongoing <br />programs. Results showing that the SLW occurs at <br />relatively warm temperatures reducing AgI's effectiveness, <br />and that dispersion rates of AgI aerosols from ground <br /> <br />In contrast to these four programs, five other <br />California cloud seeding programs have been designed and <br />implemented on the basis of several years of randomized <br />seeding trials. Table 1 lists these programs, their sponsors, <br />the randomized projects conducted prior to their going <br />operational, and the primary purpose of each program. <br />Obviously the agencies involved have made a commitment <br />to use cloud seeding as a water resource management tool. <br />Two other programs that have been in existence since the <br />mid 1970's are the Kern and Kaweah River seeding <br />projects. This makes a total of eleven programs in <br />California that have been ongoing for more than 10 years. <br />A program in the Santa Clara Valley was terminated in <br />1987 after 36 years of operation when the benefits of the <br />program (the agency felt they were obtaining 10 to 12 % <br />increases in seasonal precipitation) could not justify the <br />(;osts. During the last few years of the program, costs had <br />risen due to the need for equipment upgrades and because <br />of a law suit brought against the water agency. The suit <br />was eventually settled in the agency's favor. More <br />importantly, during the 36 years, urban growth had <br />overtaken the once rural target area, making control of <br />runoff much more difficult. <br /> <br />With the onset of California's current 5-year <br />drought, ten other programs have begun since 1987. These <br />include the coastal communities of San Diego, San Luis <br />Obispo, Monterey, and Catalina Island and programs over <br />the San Gabriel Mountains in Los Angeles County, the <br />Calaveras and Tuolumne Rivers of the central Sierra, Lake <br />Berryessa and Davis Creek watersheds near the Bay area, <br />and the Mono-Owens River Basin project on the eastern <br />side of the Sierra Nevada. In all, twenty-one programs are <br />expected to operate during the 1991-92 winter season <br />(fig. 2). Estimatl'A1 total cost of these programs, including <br />operational as well administrative expenses but excluding <br />environmental document preparation and environmental <br />monitoring, exceeds $2 million. The cost per project <br />varies from $25,000 to $400,000 per year. This variation <br />in costs reflects to some extent the watershed size but, <br />more importantly, it indicates that the technology can be <br />modifitxl to'. accoimnodate what the market price will <br />support! Unfortunately, this variability in pricing damages <br />the public image of cloud seeding and its reputation in the <br />scientific community. <br /> <br />) "u' <br /> <br />If each project were to produce only an additional <br />65 X106 m3 (5,000 acre-ft) of additional runoff (for some <br />projects this is much less than 1 % of the seasonal runoff <br />for the watershed) and water is worth $100 per 1300 m3 (1 <br />acre-ft), the combined revenues from all projects would be <br />$10.5 million dollars, producing roughly a 5 to 1 <br />benefit/cost ratio. It is this expectation of a good return on <br />a modest investment that motivates water resource <br />managers to pursue cloud seeding. <br /> <br />01 <br /> <br />Even though the additional water developed by <br />seeding falls far short of what is needed for complete <br />