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<br />. <br /> <br />. <br />. <br /> <br />~ <br /> <br />SNOW COURSE DATA <br /> <br />Snow course data provide another measure of the precipita- <br />tion by examining the change in the water equivalent of <br />the snow during the period being examined. The snow course <br />readings are taken at various locations around the first of <br />each month. The use of such data for precipitation analy- <br />sis purpOSeS is inexact at best, since a portion of the <br />moisture is lost due to evaporation, snow melt and runoff, <br />especially during the spring months. Obviously, the eleva- <br />tion of the recording station is also significant. <br /> <br />The snow course data for various locations inside and out- <br />side the project are shown in Figure 2. Since measure- <br />ments are available for only the first day of each month, <br />we considered the reports of February 1st and May 1st. <br />The changes (the May 1st water equivalent of the snow ex- <br />pressed as a percent of the February 1st water equivalent) <br />are depicted in Figure Z. <br /> <br />From the data considered, it can be seen that a 200 to <br /> <br /> <br />250 percent increase in the water content of the snow <br /> <br /> <br />occurred over the Grand Mesa National Forest where the <br /> <br /> <br />project was located. Although slightly greater increases <br /> <br /> <br />are observed near Wolf Creek Pass, an extensive dry zone <br /> <br /> <br />separates these two areas. <br /> <br />Page 7 <br />