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<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 />
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