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/? <br />O <br />0 <br />0 <br />x <br />U <br />a? <br />L <br />m <br />U <br />N <br />ca <br />N <br />11 <br /> <br />50 <br />40 <br />30 <br />20 <br />10 <br />0 WI-Mill <br />1895 1905 <br />100 <br />C <br />c? <br />L <br />Q <br />U <br />C <br />a? <br />a <br />a? <br />L <br />U_ <br />80 <br />60 <br />40 <br />20 <br />> 20,000 10-20,000 < 10,000 <br />Peak flow (cfs) <br />0 <br />Figure 2. Peak flows (m cfs) in the 15-mile reach (Stratum 9) from 1897 to 1997 (top) and <br />frequency of years with peak flows meeting various thresholds required for movement of bed <br />materials, during pre- and post-development periods (bottom). Data is from various USGS <br />gagin stations and corrected for downstream diversion withdrawals; periods of pre- and <br />post-development periods are 1897-1942 and 1954-1997, respectively (see Osmundson and <br />Kaeding 1991). Threshold flows for initiating movement of bed materials (10,000 cfs) and <br />for producing widespread mobilization of the bed (20,000 cfs) are averages from threshold <br />flows modeled for two sites in Stratum 9 by Van Steeter (1996). <br />1915 1925 1935 1.945 1955 1965 1975 1985 1995 <br />Year <br />5