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<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 />Spring and peak flows recorded at the Maybell gage were fairly similar for the years <br /> <br />1998, 1999 and 2000, with peak flows of 10,040 cfs, 9,980 cfs and 9,830 cfs, respectively <br /> <br />(Figure 2). Also since the median peak flow for the period of record for the Maybell gage (84 <br /> <br />years) is 10,000, these three years are in the range ofa normal peak flow. The 2000 spring <br /> <br /> <br />hydrograph dropped fast and by mid June flows were well below those of the two prior years <br /> <br />(Figure 2). <br /> <br />12000 <br /> <br />10000 <br /> <br />8000 <br /> <br />6000 <br /> <br />4000 <br /> <br />2000 <br /> <br />o <br />3/15 3/29 4/12 4/26 5/10 5/24 <br /> <br />J!! <br />(.) <br /> <br />1998 <br /> <br />1999 <br /> <br />2000 <br /> <br /> <br />6/7 <br /> <br />6/21 7/5 <br /> <br />7/19 <br /> <br />Figure 2. Mean daily flow between March 15 and July 31 at the Maybell gage, Yampa River <br />for 1998, 1999 and 2000. <br /> <br />Summer flows were below normal in 2000 which provided an opportunity to sample <br /> <br />the river under different flow conditions than the two prior years, which were near normal <br /> <br />(Figure 3). The minimum flow in 2000 was 30-cfs compared to 166 cfs in 1999 and 115 cfs in <br /> <br />1998. The median minimum summer flow for the period of record is 128 cfs. The 10-day <br /> <br />minimum flow (tenth lowest during the summer) in 1998, 1999, and 2000 was 170 cfs, 212 <br /> <br />cfs, and 50 cfs, respectively with a median condition of IS3 cfs. Flow was below 93 cfs <br /> <br />5 <br />