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<br />I- 100 <br /><( <br />o <br />a:z <br />UJOO <br />",0- <br />a: ~ ~80 <br />:2wt) <br />OI", <br />~I-Z <br />OLL- <br />Z 0 ~60 <br />UJOO", <br />~~Z <br />00"'0 <br />>-UJ>- <br /><.( I ~40 <br />Of-O <br />LLZO <br />OOZ <br />a:0<( <br />UJUJa: <br />en u: ,-,20 <br />20W <br />"OI <br />Z:;;f- <br />00 <br /><( <br />S <br /> <br />/' WATER YEAR 1934 <br />.----WATER YEAR 1936 <br /> <br /> <br />o <br />1920 1930 1940 1950 1960 <br />WATER YEAR <br /> <br />1970 1980 1990 <br /> <br />Figure 17. Number of days when the daily mean discharge record at Lees <br />Ferry was modified on the basis of the dIScharge record at the Grand <br />Canyon gaging station. This figure includes days when discharge was <br />modified because of ice conditions and other reasons, such as during 1934 <br />and 1936 when the computed discharge on many days in the spring and <br />summer was reduced at Lees Ferry. <br /> <br />Methods Used in this Study to <br />Compute the Continuous Record of <br />Instantaneous Discharge for <br />Water Years 1921-86 <br /> <br />Following review of the methods used by the <br />USGS to compute the daily mean discharge record, <br />the first step in computing the continuous record of <br />instantaneous discbarge was to constmct a continnous <br />record of instantaneous stage from May 8, 1921, through <br />September 30, 1986, relative to the datum of thc Dugway <br />and Lees Ferry Gages established on September 21,1921. <br />For the period prior to installation of the continuous stage <br />recorder on January 19,1923, this step involved first <br />entering the stages measured at the three principal staff <br />gages in the reach (i.e" the LaRue Gage. Number I Gage, <br />and Dugway Gage) into computer tiles from the Oliginal <br />USGS field notebooks (see Appendix B for additional <br />background information on these staff gages). Each staff <br />gage had a different period of record and datum; the <br />LaRue Gage was installed on May 8,1921, and was <br />destroyeddming the June 1921 flood; the Number 1 Gage <br />was installed at the site of the LaRue Gage on June 24, <br /> <br />1921, but at a different datum; the Dugway Gage was <br />installed on August 5,1921, near the future location <br />and at thc same datum as the Lees Ferry Gage. Thus, <br />for the peliod prior to the beginning of record at the <br />Dugway Gage on August 14, 1921, the stages measured <br />on the LaRue and Number I Gages were converted <br />into equivalent stages on the Dugway Gage. This was <br />accomplished by tirst convcl1ing the stages measured on <br />the LaRue Gage into stages on the Number 1 Gagc <br />by a process described in Appendix D. Then, the stages <br />measured on cither the LaRue or Number I Gages plioI' <br />to August 14, 1921, were converted into equivalent stages <br />on the Dugway Gage on the basis of the relationship <br />betwecn the Number 1 and Dugway Gages developed <br />by the USGS on January 25, 1922. <br />For the period after installation of the Lees Ferry <br />Gage on January 19, 1923, with its continuous strip-chart <br />stage recorder, construction of the continuous record <br />of instantaneous stage involved digitizing all of the <br />stage-recorder graphs between January 19, 1923, and <br />September 30, 1986, such that all major breaks in <br />slope of the continuous stage record were captured, <br />These digitized stage records werc then corrected for time <br />and pen errors. During periods of ice effcct, the stage- <br />recorder graphs were digitized so that most, if not all, of <br />the ice effect was removed from the stage record. For <br />example, the period in fig. 16C was digitized by following <br />the dashed pencil line that was originally drawn on the <br />record by the USGS to COlTect for the ice-dlivcn lises in <br />stage. During the two peliods when large floods on the <br />Pari a River caused backwatered flow conditions in the <br />Colorado River at the Lees Feny Gage (on October 5, <br />1925, and on August 2, 1929; Appendix B), the resulting <br />increased stages were removed from the digitized stage <br />record by the same method. To augment and check the <br />stage records digitized from the stage-recorder graphs. the <br />digital stage-recorder records from Febmary 2, 1967. <br />through September 30, 1986, were also entered into <br />computer tiles. <br />The second step in this process was to convert the <br />continuous record of instantaneous stage into a continuous <br />rccord of instantaneous discharge by using the stage- <br />discharge rating curves and shift curvcs Oliginally used by <br />the USGS to compute the published daily mean <br />discharges. To accomplish this, all of the rating curves and <br />shift curves were entered into computer files and then <br />were used to compute instantaneous discharge for the <br />period from May 8, 1921, through September 30, 1986. <br />Finally, the discharges at Lees Ferry were reduced to <br /> <br />Computation of the Continuous Record of Instantaneous Discharge at Lees Ferry faT Water Years 1921-2000 37 <br /> <br />0223"3 <br />