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<br />C\l <br />C"-. <br />~ <br />~ <br /> <br />~i:r: <br /> <br />21. Forecasts. --All 1n.t"low forecasts for lake Melld, as measured <br />at the Grand Canyon, Ariz., gaging station (pl. 2) are prepared b;y the <br />United States Bureau of Reclamation, BouJ.der Cit;y, Benda. The methods <br />used lire based upon intensive studies involving statistical correlatiOJ:\s. <br />Forecasts are prepered the first da;y of each IIIOnth, or as otherwise <br />needed, during the period 1 January through 1 August. In all. forecasts <br />derived from past flows, the undepleted flow at Grand Canyon, Ariz. is <br />predicted for the period Apr1l through July. Records show that this <br />flow is practically the same as the inflow to Ialte Powell. The final <br />forecast is obtained by subtracting the estimated depletion during the <br />Apr1l..July period by translllOuntain diversions and effective storage <br />spece in upstream reservoirs, eXCluding Ialte Powell. Effective storage <br />spece in upstream reservoirs is computed for Flaming Gorge, Blue Meaa, <br />and NlIvajo reservoirs, which are Colorado River Storage Project reser- <br />voirs. This spece is defined as the lesser of the actual spece available, <br />or the usable spece available. The usable space is the difference betveen <br />the min1mum forecasted inflow vol\lllle for any specified runoff period and <br />expected normJ. releases. The min1mum forecast 18 def1.ned as the esti- <br />mated inflow volume that, on the average, will be exceeded 19 times out <br />of 20. <br /> <br />28. The United States Bureau of Reclamation is continually improving <br />and revising forecasting methods. Each season, the mat reliable fore- <br />cast Dlllthod is chosen in advance of the forecast date by the Bureau of <br />Recl.amation. Forecasts are generall;y based upon accuaulated precipitation, <br />water equivalent of snow, antecedent runoff, or a combination of these <br />elements. A list of 13 precipitation stations used in developing 1 Jan- <br />uary, 1 February, and 1 March runoff forecasts is siven in table 6. <br />Locations of these precipitation stations are shown on plate 2. Infor- <br />mation on snow courses used in forecasting is given in the U.S. S011 <br />Conservation Service publication "Water Supply Outlook." Table 1 lists <br />the average contribution of subarea drainages to April-July runoff at <br />Grand Canyon, Ariz. Subarea drainages are shown on plate 2. <br /> <br />29. The maximum forecast, which is used in determining flood- <br />control releases, is selected by the Bureau of Reclamation. This forecast <br />is defined as the estimated inflow volume in acre-t~et that, OJ:\ theav- <br />erage, will not be exceeded 19 times out of 20. '!'he IIIBJdmwn forecast is <br />calcul/lted by adding to the mean forecast the so-called l-in-lO error, <br />as determined by the Bureau of Reclamation, using statistical methods. <br />'!'he l-in-10 errors for forecasts made in 1968 are given in the follOWing <br />table: <br /> <br />Dllte Forecast method l-in-lO error <br /> <br />1 January....: Accumulated precipitation.............: <br /> <br />: Million acre-feet <br />4.0 <br />3.4 <br />3.2 <br /> <br />1. FebrtlBry_..:... .do.................................: <br />~ }4e.rcb......:... .do................. ~...............: <br /> <br />11 <br />