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<br />514 <br /> <br />ized in the natural precipitation process. Artificial ice crys- <br />tals produced in the presence of this SL W will grow in a few <br />minutes into small snowflakes, thereby utilizing more of the <br />SL W before it evaporates on the downwind side of the moun- <br />tain. Additional ice crystals can be produced by dropping dry <br />ice pellets or releasing silver iodide (AgI) crystals from air- <br />craft into the clouds upwind of the barrier or by operating <br />AgI generators on the ground. Most operational projects in <br />the Sierra Nevada have used the ground-release method be- <br />cause of its relatively low cost. <br />Generally, operational programs seed all promising cloud <br />formations with no cases reserved as controls; consequently, <br />it is difficult to evaluate their efficiency. Nevertheless, statis- <br />tical evaluations of operational cloud-seeding programs in <br />the Sierra Nevada, based on comparisons of streamflow <br />from target and control basins in both seeded and non seeded <br />years, have indicated increases in runoff of roughly five to 15 <br />percent (Henderson, 1966; Elliott and Lang, 1967). . <br />During the 1960s Pacific Gas and Electric Company con- <br />ducted randomized seeding experiments near Lake Almanor <br />in the Feather River Basin (Mooney, and Lunn, 1969), and <br />the Fresno State College Foundation conducted Project <br />CENSARE (Central Sierra Research) in the Stanislaus and <br />Mokelumne Basins. Both groups concluded thatseeding ef- <br />fects depended strongly on wind direction, temperature, at- <br />mospheric stability, and other storm characteristics, but <br />their results were not in complete agreement. <br /> <br />3. The design of SCPP <br /> <br />SCPP was conceived in the early 1970s in the hope that a via- <br />ble seeding technology could be developed to increase precip- <br />itation and runoff to alleviate future water problems in Cali- <br />fornia, including salinity problems in the San Joaquin delta. <br />The program officially began in February 1973, with the sign- <br />ing of a cooperative agreement between the state of Califor- <br />nia and the Bureau of Reclamation. The following three <br />years were taken up with design studies and environmental <br /> <br />Vol. 67, No.5, May 1986 <br /> <br /> <br />,~ ", \ <br />'\\ ,..., ~ \ ~~NO <br />,< I , \, IRNI <br />'" I ,~, \ <br />\ '''' -,",' \ <br /> <br />"~ '{.\;.I I <br />, '\ ,101 I <br />, \ , ,1000", \ I <br />, , I,' \SI I I <br />I, ,'Wi II <br />\ \ \ \ I Li.E "II \ <br />I , , \ I TAHOE ,\\11 <br />AMERICAN \ ,\ I II' I I <br />, \I lill <br />\ ",I ,II, <br />, \ ' ',' \ I \ \ , <br />RIVEif' , , ~ ,./ ,,",' ,,'00 <br />\ , ''''~ '6' ' <br />, , , Iii'.', . I \ <br />'FRESH POND '<.,,, I'~~, I <br />BASIN 0' If PI \ "".', I '00 <br />, , \ "~'" <br />, , \ \ <br />, , \ , <br />, , \ noo <br />I '1000 <br />1000 1500 <br /> <br />FIG. 1. Map ofthe Sierra Cooperative Pilot Project area, which is <br />essentially the American River Basin. Smoothed topographic con- <br />tours are shown as dashed lines and labeled in meters. The total area <br />of the Basin above Folsom is 4220 km2, of which 1265 km2 is above <br />1830 m and receives 90 percent or more of its winter precipitation as <br />snow. The annual runoff averages 3.23 X 109 m3. <br /> <br />assessments. During 1974, 21 public meetings were held in <br />California and Nevada to discuss environmental issues and <br />the public's responses were analyzed. It was concluded that, <br />while it was unlikely that the project would harm the envi- <br />ronment, environmental studies should be included in the <br />program and the public should be kept informed of SCPP <br />activities. <br />On the basis of a design study completed in 1976 by <br />MBAssociates, the American River Basin (ARB) was se- <br />lected to be the primary study area. Figure 1 outlines the lo- <br />cation of the ARB and lists some of its important character- <br />istics. <br />As most of California, including the ARB, has a Mediter- <br />ranean climate, more than 90 percent of the annual precipita- <br /> <br />Distance From Crest (KM) <br /> <br /> 120 100 80 80 40 20 0 20 40 <br /> Barrier (Stylized) 1603 1800 <br /> 2500 - 1589 1800 <br /> 1413 '1:1 <br /> 2000 - .... 1400 ~ <br /> ,,- , <br />i 1107 -- 1200 "& <br /> - ... <br /> 969 , <br />c:: 1500 - " .... 1000 !!l <br /> ..... ..... <br />0 ,...- o' <br />i 800 ::l <br /> 600 ..... <br />1000 - 553. 596 600 ~ <br />iii ./ ~ <br /> 500 - ./ 400 <br /> ./ 143. 200 <br /> Sacramento Auburn Blue Canyon Crest Reno <br /> <br /> <br />FIG. 2. Barrier traverse plot of winter season (Nov.-Apr.) precipitation totals across the SCPPproject area using SCPP precipitation-gauge <br />network. Individual values are network-wide averages based upon 1978/79 through 1983/84 winter-season observations within 20-km dis- <br />tance-from-crest partitions. Values marked by asterisks (0) are from cooperating agencies. <br />