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<br />Therefore, the combined discharge of the upper Colorado, <br />Green, and San Juan Rivers contributing to the peak <br />discharge of the June 1921 flood at Lees Ferry was <br />approximately 167,000 fi3/s. <br /> <br />Revised Estimate of the Peak Discharge of the <br />1921 Flood at Lees Ferry <br /> <br />Because the peak discharge of the Jnne 1921 flood <br />had to be the same throughout the Lees FelT)' reach, <br />extrapolations of the stage-discharge rating curves at the <br />Lees Ferry Gage and the three staff gages in the l-mile- <br />long reach upstream were used to establish constraints on <br />the peak discharge of this flood (fig. 12), A strong reversal <br />in curvature is evident in the stage-discharge rating curves <br />defined by the data from the Lees Feny, Number 4, and <br />Cable Gages, and a mild reversal in curvature is evident in <br />the stage-discharge rating curve defined by the data from <br />the Number 1 Gage, At stages in excess of those at which <br />the reversal in curvature occurs at these four gages, <br /> <br />analyses of the goodness of fit oflinear and power-law <br />regressions indicate that the high-stage parts of the <br />stage-discharge rating curves at these gages are best <br />approximated by either a linear or a power-law relation, <br />in which discharge is proportional to stage raised to a <br />power of less than one (fig, 12). <br />The reversals in curvature of the stage-discharge <br />data at the Lees Ferry Gage for the entire pre-dam period <br />of 1921-{j2 and for only water-years 1921-22 both <br />occur at a stage of 15 ft. Linear regressions fit to the <br />1921-{j2 and 1921-22 data above this stage are virtually <br />identical (fig, 12A), and have R2 values of 0.929 and <br />0,932, respectively. Similarly, power-law regressions <br />fit to the 1921-{j2 and 1921-22 data above this stage are <br />also virtually identical (fig. 12A), and have R2 values of <br />0.932 and 0.974, respectively. The similarity of the <br />regressions fit to the 1921-{j2 and the 1921-22 data <br />indicates that the upper end of the stage-discharge rating <br />curve at the Lees Ferry Gage was fairly stable over time, <br /> <br />A. 240,000 8,240,000 <br /> 220,000 PUBLISHED PEAK DISCHARG 220,000 PUBLISHED PEAK DiSCHARGE <br />0 OF THE 1921 FLOOD 0 OF THE 1921 FLOOD <br />z 200,000 Z 200,000 <br />0 0 <br />() () <br />w 180,000 w 180,000 <br />U) U) <br />a: a: <br />w 160,000 w 160,000 <br />Q. Q. <br />t- REVERSAL IN Iii REVERSAL IN <br />w 140,000 CURVATURE 140,000 CURVATURE <br />w OF DATA w OF DATA <br />u. w u. <br />() 120,000 I I () 120,000 <br />1ii t- W 1ii W <br /> u.D I J: <br />::> 100,000 00 t- ::> 100,000 t- <br />() w9 u. () u.O <br />~ COu. 0 ~ 00 <br />ui 80,000 e'> w ui 80,000 wO <br />co U)S! '" '" ",IT' <br /> ;:': <!- <br />a: 60,000 "'- a: 60,000 t;~ <br /><! <! U) <! <br />a: w '" I ,,- <br />() 40,000 Q. <! 0 40,000 <! <br />U) W U) W <br />0 Q. 0 Q. <br /> 20,000 20,000 <br /> 0 0 <br /> 5 10 15 20 25 30 35 40 5 10 15 20 25 30 35 40 <br /> STAGE AT LEES FERRY GAGE, IN FEET STAGE AT NUMBER 4 GAGE, IN FEET <br /> <br />EXPLANATION <br /> <br />o 1921--B2 DATA <br /> <br />- LINEAR AND POWER-LAW REGRESSIONS FIT TO ALL <br />THE 1921-62 DATA ABOVE A STAGE OF 15 FEET <br /> <br />,,--~ "". V~ LINEAR AND POWER-LAW REGRESSIONS FIT TO ONLY <br />THE 1921-22 DATA ABOVE A STAGE OF 15 FEET <br /> <br /> <br /> <br />EXPLANATION <br /> <br />o 1921-23 DATA <br /> <br />- LINEAR AND POWER-LAW REGRESSIONS FIT TO THE <br />1921-23 DATA ABOVE A STAGE OF 16 FEET <br /> <br />Figur. 12. Linear and power-law extrapolations of the stage-discharge rating curves at the Lees Ferry, Number 4, Cable. and Number 1 Gages, <br />{AI Rating curve at the lees Ferry Gage defined by 1he 4,114 non-ice.affected discharge measurements made during water years 1921-62, Stage is rela1ive <br />to the Dugway Gage and Lees Ferry Gage datum of Sep1ember 21, 19211see Appendix BI, Shown for comparison are the peak stages of the 1921 and <br />1884 floods and the published peak discharge of1he 1921 flood,lb1 Ra1ing curve at1he Number 4 Gage defined by the 209 discharge measurements made <br />during water years 1921-231hat included stage observations at the Number 4 Gage, Stage is relative to the Number 4 Gage datum of September 29. 1921 <br />[see Appendix BI, Shown for comparison are 1he peak s18ge and published peak discharge of the 1921 flood, Stage is relative to the Number 1 Gage datum <br />of September 26, 1921 {see Appendix 81. Shown forcomparison are the peak stage and published peak discharge olthe 1921 flood, <br /> <br />'O(1).38 <br />. '."'. Colorado River floods at Lees Ferry 27 <br />