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<br />t <br />t <br />t <br />t <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />. <br />. <br />. <br />~ <br />~ <br />. <br />~ <br />~ <br />~ <br />. <br />~ <br />I <br />I <br />I <br />I <br />. <br />. <br />I <br />I <br />. <br />. <br />, <br />. <br />I <br />I <br />I <br /> <br />these observations included the National Weather Service and the National Resources <br />Conservation Service. The four complete months with seeding activities (December through <br />March) were evaluated using SNOTEL precipitation observations from the target area. April 1st <br />snow water content values from SNOTEL or NRCS manually observed snow course sites were <br />utilized in a separate evaluation. Six sites in the target area (five used in last year's evaluation. <br />plus Slumgullion which was added to include infonnation from the new portion of the target <br />area) were correlated with eleven precipitation sites. Nine snow waler observation sites in the <br />target area (comprising five sites used last year, plus two sites unavailable last year (Crested <br />Butte and Keystone). plus t\\.o new sites from the new southern portion of the target area) were <br />correlated "lith five sites in non-seeded control areas. Historical periods were selected to <br />exclude earlier seeding projects that may have impacted the observations. Individual station <br />records were examined for data quality. Data from potential control sites were averaged together <br />in dilTerent groupings and correlated (using linear regression techniques) with the average values <br />from the target sites to detennine the best set of control stations. one that provided both a high <br />correlation with the target and also provided some geographic "bracketing" of the target area. <br />Reasonably good correlations were established between control and target areas. with r values <br />ranging from 0.83-0.87. These equations were then used to estimate the amount of precipitation <br />and snow water content that would be expected for the 2003-2004 winter program based upon <br />the observations at the control sites. These estimates were then compared to the observed <br />average precipitation and snow water content at the target sites. <br /> <br />The precipilalion e\'aluation discussed in seclion 4.JA indicated a seedin~ dfeel of <br />+3~%. The snon water contenl evalualion (seelion 4.2.2) su~~esled a lar~er effecl~ <br />approximalelya 13-14% increase. It is unclear why the indicated increases in precipitation are <br />less than those indicated in the snow water contents. It is noted that a similar result was <br />indicated last year. NA WC's report for last year indicated a potential problem in the <br />precipitation measurements related to under catch of snowfall due to strong winds at the near- to <br />above-timberline locations in the target area. Examination of the plots of precipitation and sno\\" <br />water content from this past season did not seem to indicate such an effect. One possible <br />difference between the precipitation and snow water content evaluations that may partially <br />explain the different outcomes is the length of the historical periods used to develop the <br /> <br />59 <br />