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• desirable to determine the flow requirements within these <br />reaches for YOY squawfish. Such flow requirements result <br />from analysis of both physical habitat and biologic data; <br />the results presented in this phase of the report only <br />define the species requirements with respect to depth, <br />velocity, and substrate. <br />3. Certain habitat types, based both on PHABSIM results and <br />actual fish captures, offer little suitable habitat at any <br />normal flow, but may serve as refugia during extremely <br />low-flow periods. In such cases, passage from normally <br />suitable reaches to these areas might allow short-term <br />survival during such severe conditions as were seen in <br />1977 or 1981. Also, such habitats, usually characterized <br />by poor physical diversity, may be selected as potential <br />habitat improvement locations. <br />4. To assure reproductive isolation between humpback and <br />roundtail chubs at Black Rocks, May mean monthly dis- <br />charges should be maintained in the 10,000 to 13,000 cfs <br />range; June flows, at least at the historic mean monthly <br />level, appear to be desirable. <br />5. The analyses of flow and WUA time series for natural vs <br />present level depletions demonstrated a generally positive <br />• effect upon squawfish YOY. However, the apparently narrow <br />range of suitable discharges at the Green River nursery <br />sites (especially Mineral Bottom) resulted in effects <br />ranging from high positive to high negative, depending <br />upon the month involved. It is quite possible that fur- <br />ther unspecified depletions in either river might result <br />in generally negative effects. At present, the discharge <br />ranges suggested should be adhered to. <br />6. The apparent suitability of low-regime flows for YOY <br />should not encourage neglect of temperature and sediment <br />transport consequences. The 3,500 cfs flow found to <br />provide excellent YOY habitat at Ouray and Mineral Bottom <br />would not be a suitable peak flow to ensure maintenance of <br />sand-transport equilibrium throughout the Green River. <br />Similarly, the 7000-8000 portion of the suitable Potash <br />YOY range, if allowed to become peak flow in the Colorado, <br />would not ensure sand-transport equilibrium, and might <br />alter the Black Rocks-Westwater temperature regime enough <br />to cause loss of reproductive isolation between humpback <br />and roundtail chubs. <br />LITERATURE CITED <br />• Bovee, K. D., and R. T. Milhous. 1978. Hydraulic simulation in instream <br />flow studies: theory and techniques. U.S. Fish and Wildlife <br />Service, Instream Flow Information Paper 5, FWS/OBS-78-33, Fort <br />Collins, CO. 130 p. <br />33