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<br />~ <br />u <br /> <br /> <br />800 <br /> <br />-+-1997, wettest <br />_ ...... _ 1920, 25% <br />~1967,med~n <br />~ 1919, 75% <br />~ 1934, driest <br /> <br />200 <br /> <br />8/21 <br /> <br />9/10 <br /> <br />9/30 <br />Date <br /> <br />10/20 <br /> <br />11/9 <br /> <br />11/29 <br /> <br />Figure 2.3. Seasonal hydrographs for the driest (1934), 75% exceedance (1919), median (1967), <br />25% exceedance (1920), and wettest (1997) years recorded on the Yampa River, Maybell gage. <br /> <br /> 550. <br /> 500 ..--.. <br /> . <br /> 450 '., <br /> 400 <br /> 350 <br /> 300 <br />,-, <br />ol!l <br />CJ 250 <br />- <br />Cll <br />~ <br />l.o 200 <br />~ <br />-= <br />CJ <br />III <br />Q 150 <br /> 100 <br /> 50 <br /> 0 <br /> Ol Ol Ol Co 2- tl tl <br /> ::J '" <br /> :! ~ ~ Vl Vl 0 0 <br /> '" en N lil 0 ... <br /> N N <br /> Date <br /> <br /> <br />.--50%1 <br />,! i <br />i- '60%1 <br />'-70% <br />1-,.. 80% I <br />!-90%1 <br /> <br />> <br />o <br />Z <br />,.:. <br /> <br />> <br />o <br />:iT <br />N <br /> <br />Figure 2.4. Fall hydrograph for the Yampa River, Mayben gage showing percentile flows. <br /> <br />total annual depletions occur in the months of April, May and June. Natural flow was reduced by an <br />average of only 6% for those three months. The fall and winter months of October through March <br />accounted for 8% of the annual water diversions and natural flow was reduced by about 6%. Depletions <br />had the greatest impact during August and September, when natural flows for the 17-year period were <br /> <br />22 <br />