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There is a threshold at the lower end at <br />which point ambient conditions (air temp, <br />sunlight, etc) over-ride the small increase <br />in flows. Once the threshold is met, <br />increased flows will lower water <br />temperatures until there is an equilibrium <br />with flows and other factors (again, air <br />temp, sunlight, etc.) <br />d <br />L <br />? <br />R <br />L <br />d <br />Qc. <br />G <br />d <br />? <br />L <br />d <br />*J <br />? <br />? <br />Discharge (cfs) 1200