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Stage/Discharge Data Collection <br />Green River <br />In order to predict the flooding discharge of a bottomland accurately, a thorough data collection effort <br />conducted before and during the runoff season is preferable. This was possible at the SR site in 1997. <br />On four occasions during the runoff season, water surface elevations (stages) and corresponding <br />discharges for the Green River at Jensen were documented for the SR reach. The SR cross section <br />endpoints, established in April 1997, were used to determine and record water surface elevations. <br />Discharges ranged from 12,300 cfs to 20,400 cfs, bracketing the flooding discharges of interest. <br />Typically, the water surface elevations were determined at the edge of water near the top of bank on the <br />side of the river where the bottomland was located. Observations of the water surface relative to the top <br />of bank and adjacent bottomland were also documented at the different discharges. For reference, <br />tabulations of the recorded water surface elevations, dates, and discharges for the SR cross sections can <br />be found in the 1998 technical report. <br />Due to availability and extent of discharge data recorded by the Green River at the Jensen gage, the <br />Jensen data were used for the stage/discharge analyses. From the stage measurements and recorded <br />discharge data at Jensen, stage/discharge rating curves were developed for all six cross sections at the <br />SR bottomland site. The results of these analyses are detailed in Chapter Four of this report. <br />For the SN, IM, and SL properties, stage/discharge data were not collected during the 1997 runoff <br />season. A hydraulic model was developed from cross section surveys and a high water reference mark <br />on the Jensen Highway 40 bridge for the SN/IM properties. Similarly, a hydraulic model was developed <br />for the SL properties using stage/discharge data from the 1996 and 1997 data collection efforts at the <br />Horseshoe Bend and Bonanza Bridge sites. Additional stage discharge data was ,however, collected <br />during the 1998 runoff season in order to improve the modeling. Further discussion of the modeling effort <br />• can be found in Chapter Four of this report. For these three sites, additional stage measurements will be <br />collected during the 1998 runoff season to further improve the accuracy of the flood predictions <br />Gunnison River <br />Stage measurements were taken at the five BC site cross sections on six different days during the 1997 <br />runoff season. Gunnison River flows ranged from 6400 cfs to 9200 cfs. One discharge measurement <br />was taken on May 21St, 1997. The Gunnison River near Grand Junction, Colorado was used for the rest <br />of the calibration. For the Dad's Flat site, stage measurements were taken on four occasions, with flows <br />ranging from 7900 cfs to 9000 cfs. One discharge measurement was performed on May 31St, 1997.- No <br />stage discharge data was taken at either site in 1998. <br />Colorado River <br />The BO/BR ponds were not surveyed until the fall of 1997. Therefore, the majority of the stage data were <br />collected in 1998. Water surface elevations (staq~es) were surveyed at cross section BR-4 on five <br />different days between March 12th, 1998 and July 6t , 1998. Discharges ranged from 2270 cfs to 10,200 <br />cfs. This data was used to re-calibrate the HEC-RAS flood prediction model developed iri 1997. The <br />accompanying technical report has more details of the modeling. <br />• <br />2-3 <br />