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Gunnison River / Aspinall Unit Temperature Analysis -Phase I <br />. Page 11 <br />Temperature Profile <br />0 <br />0.0 <br />10.0 <br />20.0 <br />30.0 <br />_ 40.0 <br />E <br />~ 50.0 <br />a <br />m <br />~ 60.0 <br />70.0 <br />80.0 <br />90.0 <br />100.0 <br />Temp C <br />Figure 7. Temperature Profiles for Blue Mesa Reservoir (Sapinero Basin), <br />2000. <br />An analysis of temperature profile data for each of the three basins indicates that there is <br />very little longitudinal variation in temperature. Bottom temperatures in the deepest part <br />of the reservoir (Sapinero Basin) are very cold and stay relatively constant throughout the <br />summer (Figure 7). <br />Over 50% of the tributary inflow comes from the Gunnison River (NPS, 1996), which in <br />1996 was the coldest of the four major tributaries (Cebolla, Soap, and Lake Fork) <br />(Johnson, et al., 1997). <br />Numerous profiles were provided for the years 1997 - 2000 for Blue Mesa Reservoir. Of <br />these years, 1997 runoff was well above average and 2000 runoff was well below <br />average. Profiles for 1997 are displayed in Figure 8 and profiles for 2000 are shown in <br />Figure 7. Estimated release temperatures during these two years are shown in Figure 9. <br />Hydrosphere Resource Consultants <br />5 10 15 20 25 <br />