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<br />5,271 <br />3,470 <br />3,675 <br />3,970 <br />7,765 <br /> <br />72, 000 <br />38,960 <br />41,510 <br />45,880 <br />84,200 <br /> <br />I <br />I <br />I i <br />,I <br /> <br />I <br />I' <br />I <br />I <br />I <br />I ' <br />, <br />I' <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />lies above EI 9000. The portion of that peak flow attributable to snowmelt is <br />approximately 25,000 cfs and the major portion of the snow pack is located at <br />elevations above 9000 feet. The typical May 1 snowpack water equivalent for <br />that basin above 9,000 feet is 13 inches. The 72-hour PMP for that basin as <br />estimated froDl HMR49 is 6.3 inches. The estimated 500-year flood peak is <br />25,400 cfs and the ratio of the PMF to the 500-year flood is 2.83. The simi- <br />larity between the spring runoff hydrographs on the Colorado and Gunnison <br />Ri vel'S is illu;~trated in Fig. II-5 by the 1957 flood hydrographs. <br /> <br />4. Des:lgn Flood Estimates for <br />Oth,~r Gunnison River Projects <br /> <br />Des~~gn flood estimates for USBR projects located on the Gunnison <br />(16)(20) <br />River compare to those for the TM.-County Project estimated by Beck <br /> <br />as follows: <br /> <br />ProJect <br /> <br />TM.-Count:, <br />BI ue Mesa <br />Morrow Poj~nt <br />Crystal <br />Daninguez <br /> <br />Drainage Area (mi 2) <br /> <br />Estimated Design Flood <br />Peak Flow (cfs) <br /> <br />This canparison is shown graphically on the USER Peak Discharge Curve <br />(Fig. II-6). <br /> <br />5. PMF Calculation for Una Reservoir <br /> <br />The peak flow for the PMF was calculated in two slightly different <br />ways and then the res ults of the two methods were averaged. The average was <br />then checked for reasonableness by three other estimation methods. <br /> <br />The two primary estimation methods are based on: (1) adjustment of <br />the portion of the Tri-County PMF peak flow attM. butable to snownelt by the <br />direct ratio of the Una versus the Tri-County drainage areas above EI 9000; <br />and (2) adjustment of the snownelt peak by the direct ratio of the average <br /> <br />II-14 <br />