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Gunnison River /Aspinall Unit Temperature Analysis -Phase I <br />Executive Summary, Page-A <br />EXECUTIVE SUMMARY <br />Introduction <br />Hydrology of the Gunnison basin has" been significantly altered by the construction and <br />operation of the Aspinall Unit (Blue Mesa, Morrow Point and Crystal Reservoirs), <br />numerous other smaller reservoirs, and diversion and return flow features related to <br />irrigation in the basin, particularly in the areas surrounding Montrose and Delta. Cold- <br />water releases from the Aspinall Unit reservoirs have been identified as a significant <br />impediment to re-establishment of pikeminnow habitat in the Gunnison River near Delta <br />(Osmundson, 1999). Results of Osmundson's work indicate that increasing mean water <br />temperatures at Delta by 1 °C in June, September and October, and by 2 °C in July and <br />August, would increase the mean annual thermal units (ATU) from 32 to 46 units. Such <br />an increase would put stream temperatures at Delta at a level similar to sites on the <br />Yampa and Colorado Rivers which have abundant populations of pikeminnow. <br />The objective of this phase I study was to determine the feasibility of increasing stream <br />temperatures in the Gunnison River at and below Delta, Colorado through structural and / <br />or operational modifications to the Aspinall Unit reservoirs. The project is being <br />approached in a two-step process. The first phase of the work, which this report <br />summarizes, includes: data collection and assessment; an overview of factors that may <br />constrain the Program's ability to meet temperature objectives; a cursory analysis of the <br />data with the intent of gaining insight into the primary physical processes governing <br />water temperature in the basin; and modeling recommendations for the second phase of <br />the work. <br />Phase II of the project, if approved, would involve development of numerical models of <br />both the Aspinall reservoirs and the Gunnison River downstream. The objective of phase <br />II would be to use these models to simulate temperatures in the river /reservoir system <br />under a variety of Temperature Control Device options and flow regimes. <br />Results and Recommendations <br />We must stress that the results presented here are based on a preliminary analysis of the <br />available data. We strongly recommend that a rigorous modeling effort be undertaken, <br />with a particular focus on how thermal regimes in the three Aspinall reservoirs could <br />change with installation of a temperature control device (TCD). <br />The results of phase I of the Gunnison River /Aspinall Unit Temperature Study indicate <br />that Aspinall Unit construction and operation has had a significant impact on water <br />temperatures at Delta, and that warmer release temperatures during the summer would in <br />most cases translate into warmer temperatures in the river near Delta. The findings also <br />indicate that a TCD on Blue Mesa Dam is likely to be the best approach to achieving <br />warmer releases from Crystal Dam. Although modified annual flow patterns have also <br />impacted water temperatures at Delta, complications arising from physical and <br />Hydrosphere Resource Consultants <br />