The Hydrologic Impacts From the Diversion of Winter Flows of ...
The Hydrologic Impacts From the Diversion of Winter Flows of ...
The Hydrologic Impacts From the Diversion of Winter Flows of ...
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snowpack for fall and spring conditions. Smart and Fleming's<br />
1985 estimate <strong>of</strong> 10 percent CU for <strong>the</strong> Santa Fe Ski Area may<br />
be a reasonable estimate <strong>of</strong> <strong>the</strong> CU at Ski Rio. <strong>The</strong> ski areas<br />
are situated on like soils and topography with<br />
similiar<br />
slope orientation.<br />
Wright Water Engineers and Leaf (1986, p. 9)<br />
investigated <strong>the</strong> CU <strong>of</strong> water used to make artificial snow<br />
for Colorado Ski Country USA. <strong>The</strong> study assembled data from<br />
six different ski resorts throughout Colorado and<br />
modeled<br />
<strong>the</strong> watershed loss associated with <strong>the</strong> snowmaking.<br />
<strong>The</strong><br />
average CU from <strong>the</strong> six resorts for<br />
was 22 percent, 6 percent initial<br />
an average water ye~r<br />
loss and 16 percent<br />
watershed loss.<br />
Ski Rio is located halfway between<br />
Santa Fe Ski Area<br />
and <strong>the</strong> resorts studied in Colorado. <strong>The</strong><br />
conditions and<br />
settings from both studies are similiar and so an<br />
average<br />
between <strong>the</strong> two CU estimates has been used in this study.<br />
<strong>The</strong> estimate for CU <strong>of</strong> Cordova creek water at ski Rio is 16<br />
percent <strong>of</strong> <strong>the</strong> total diversion.<br />
Figure 2.<br />
5