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<br />14 <br /> <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />riffle was surveyed on August 8 and 9 and again on October 19 and 20, 2000. Waterline shots <br />were made on June 27 and 28,2001, and at a lower flow on July 31 and August 1. <br /> <br />Colorado River, Clifton study site <br /> <br />A second study site in the IS-Mile Reach of the Colorado River was labeled the Clifton <br />station. A 4.25 kilometer stretch of the between river miles 177.7 and 180.4 was surveyed on <br />May 31, June 1,2,4 and 5, 2000. This site is just upstream of the original site, surveyed in 1999, <br />now called the Corn Lake station but in prior reports it was named the IS-Mile Reach station. A <br />total of 45,000 usable bathymetric survey points were collected at the Clifton station using the <br />boat GPS/sonar equipment. <br /> <br />Aerial photography of the 15Mile reach of the Colorado River has been digitized by <br />Mesa County Survey System and was purchased from them to aid in identification of landmarks <br />and waterline boundaries. We accomplished this by using the latitude and longitude brass <br />marker at the intersection of 31 and C Road for a reference pin for our survey. Therefore, both <br />the Corn Lake and Clifton survey can have associated photography. <br /> <br />Waterline/water surface measurements were taken with the GPS walking method on <br />August 1,2 and 3,2000, January 23,24,25 and 26, 2001 and the final set on June 18,19 and 20, <br />2001. <br /> <br />Dolores River, Big Gypsum study site <br /> <br />Over a three-day period, May 16, 17, and 18,2000, bathymetric data was collected along <br />a 3-km section of the Dolores in the Gypsum valley. As was the case with the Yampa River, <br />there were lower than normal runoff flows made data collection using the sonar more difficult <br />and certain parts of the river were too shallow for the sonar. Several days were spent in June and <br />July 2000 logging addition points by the walking method. This walking method logs points from <br />the GPS with a Psion data collector running Field Face software. Waterline/water surface shots <br />were made on July 6 and 7,2000 and on June 13 and 14,2001. <br /> <br />Acoustic Doppler and Marsh McBernie Velocity Meters <br /> <br />For model calibration, it is important to have observed measurements of depth and <br />velocity at known flows. While depth can be gathered using the same technologies that are used <br />in determining bathymetry, velocity measurements require another set of instruments. Two <br />different technologies were used for measuring velocities in this project, the GPS and flow <br />meter/wading rod, and the GPS and Acoustic Doppler. Because of low summer flows the boat- <br />mounted acoustic-Doppler was not used to gather velocity data in 2000. A detail description of <br />both techniques was given in Anderson and Stewart (2000). <br /> <br />Data Reduction and Preparation <br /> <br />The use of GPS, sonar, and the COMLOG program produced a large number of <br />coordinate points at each site, and data sets had to be checked for quality and quantity. The <br />