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1 <br />1 <br />1 <br />1 <br />1 <br />1 <br />1 <br />i <br />1 <br />1 <br />1 <br />1 <br />1 <br />1 <br />1 <br />Snow Conditions: <br />Snow course conditions were monitored using a compilation of the 23 SNOTEL sites in the <br />Upper Colorado River Basin. As indicated by Figure 2, the streamflow peak at Palisade occurred <br />approximately one month after maximum snow water equivalent occurred, similar to what <br />occurred in 1997 and 1998. The tail end of the 1999 snow water equivalent peak was just slightly <br />below average. <br />Figure 2 <br />Colorado. Basin SNOTEL Data <br />20 <br />18 <br />16 <br />14 <br />e <br />c <br />E 12 <br />m <br />w 10 <br />8 <br />N <br />6 <br />4 <br />2 <br />MOOD <br />12000 <br />1001X1 <br />WM <br /> ---- SWE, Waler Year 1999 <br /> - SWE, 30 Year Average " <br /> Streamflow Q Palisade . <br />8000 c <br />4000 <br />2000 <br />01? I I I I 1 I 1 3 1 1 110 <br />10n90 10MAS 11=00 12MM 12899 39048 1!2848 52848 60ffi 7RSO 82748 82848 <br />WaW Year <br />Provislonaldata, subJeclto change <br />May 1999 Proiect Area Snow Conditions <br />Snowpack-water content on April 1 was 77 percent of the 1966-1995 average throughout the <br />Colorado Big Thompson Project (CBT) watersheds. The Green Mountain or Blue River (West <br />Slope) watershed was the highest at 92 percent of average. The lowest snowpack water content <br />on the CBT Project was recorded for the Lake Estes watershed (east slope watershed) at 62 <br />percent of average. <br />Snowpack water content on April 1 was below normal on the Fryingpan-Arkansas Project <br />watersheds. The Upper Arkansas River watershed (east slope) was 83 percent of average. The <br />Fryingpan River watershed was 69 percent of average. <br />7