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Table 3. Percent decline of mean-monthly streamflow in the Gunnison <br />(Whitewater gage) and Colorado (Cisco gage) rivers during spring runoff <br />attributable to the Aspinall Unit. (Change from middle-development period to <br />post-Aspinall period.) <br />Month <br />Gunnison River <br />Change <br />Percent in <br />change CFS <br />Colorado River <br />Change <br />Percent in <br />change CFS <br />Percent of change <br />in Colorado River <br />due to Aspinall <br />April - 1.4 43.8 - 3.7 305.2 14.4 <br />May -25.1 1,864.1 -12.8 2,477.3 75.2 <br />June -32.2 2,326.7 -12.8 2,778.1 84.0 <br />July - 2.6 62.6 + 8.6 699.4 <br />(Table 3). Mean-monthly Colorado River flows have declined 2,477 and 2,778 <br />cfs for the same months. Because changes in Gunnison River flow directly <br />affect Colorado River flow, the Aspinall Unit is responsible for 75 to 85~ of <br />the decrease in average spring runoff since 1966 for the Colorado River at <br />Cisco (Table 3). <br />EFFECT OF CHANGES CAUSED BY THE ASPINALL UNIT ON THE ENDANGERED FISHES <br />Water Temperature <br />The Aspinall Unit reduced the temperature of the Gunnison River within <br />historic range of Colorado squawfish and razorback sucker. This temperature <br />reduction probably did not affect adult habitat, but may have affected <br />maturation of adult fish or spawning success--particularly of Colorado <br />squawfish. Pre-Aspinall temperatures in the lower Gunnison River were already <br />marginal for Colorado squawfish reproduction, but construction of the Aspinall <br />Unit reduced them further. Wiltzius (1978) suggested that construction of the <br />22 <br />