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I INTRODUCTION <br />i <br />The closing of Glen Canyon Dam in March 1963 produced a <br />major change In temporal discharge patterns of the Colorado River <br />in Glen and Grand canyons (Figure 1.1). During the predam period <br />of measure, annual discharge volumes and maximum discharges <br />varied greatly from year to year.. Maximum flows exceeding 50,000 <br />cubic feet per second (cfs) were common. For 20 years following <br />the dam's closure, during which time Lake Powell was filling, <br />regulated maximum flows exceeded 50,000 cfs in one year and <br />30,000 cfs in only two additional years. Since early 1983, <br />however, a combination of high runoff from snowmelt and the high <br />stage of Lake Powell has resulted in maximum flows at Lee's <br />Ferryl between 45,000 cfs and 92,600 cfs. In contrast, minimum <br />flows, both pre- and post-dam, have been An the range of 1,000- <br />4,000 cfs during most recorded years. <br />Prior to the closure of Glen Canyon Dam, there was little <br />daily variation in discharge of the Colorado River in the study <br />area. Rather, the variation was seasonal, largely due to <br />snowmelt runoff (April-June) with occasional summer floods and <br />periods of summer drought. Since the onset of regulated flows, <br />the seasonal pulse in discharge from snowmelt has continued, <br />although much abated in most years. Much of the variation, <br />however, now occurs on a daily basis with dam releases dictated <br />by needs for hydropower in the growing metropolitan areas of the <br />southwestern United States. This variation, which is reminiscent <br />of tides in marine systems, has no known corollary in the <br />evolutionary history of the native flora and fauna of the <br />Colorado River. <br />During peaking power periods, minimal water is released from <br />the reservoir at night when the demand for power is low, and <br />discharge is increased dramatically during high demand daytime <br />hours. Weekends and holidays are often characterized by extended <br />periods of low flow. <br />1Throughout this report we will observe the spelling "Lee's <br />Ferry" in reference to the sight formerly occupied by John D. Lee <br />and used to ferry boats across the Colorado River. In this <br />respect, we follow Rusho and Crampton (1981) and concur with <br />their finding that the spelling "Lees Ferry" as commonly used is <br />"...both in poor grammar and poor history, since no person named <br />Lees was ever involved." <br /> <br />-9-