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<br />1 <br /> <br /> <br />1 <br /> <br />L <br /> <br /> <br /> <br />1 <br />1 <br />t <br /> <br /> <br />1 <br /> <br /> <br /> <br />Table 2. 1. Table showing which floodplain sites are located in which river reach and the river <br />mile for each reach. <br />Reach <br />Site Code number <br />Start RM End RM <br />BB 1 290.0 283.0 <br />HB,BC 2 283.0 276.0 <br />SR,BA 3 276.0 269.0 <br />AB 4 269.0 262.0 <br />L7,L 10 <br />and J4 <br />5 <br />262.0 <br />255.0 <br />SB,OCD <br />and OCW <br />6 <br />255.0 <br />248.0 <br />GENERAL SITE DISCUSSION <br />To provide rearing habitat for young-of-year native species, these floodplain wetlands <br />must be accessible to the fish during the narrow window of time in which larval fish are drifting <br />in the river channel. As river flows rise above flooding levels, the wetlands begin to fill. The <br />time it takes for each site to fill depends on main channel flows, the size of the site, and the <br />configuration of the connection with the river. Levee removal sites take several days to a week <br />to reach equilibrium with the river after connection is made. As river flows rise and fall, water <br />will surge in and out of the wetland until high spring flows subside permanently usually in mid <br />to late June. The number and duration of these filling surges varies widely from year to year. If <br />the levee removal sites are to be useful to larval native fish, the filling events and inflow surges <br />must occur at the same time as larval drift in the main channel of the river. Figures for each year <br />since 1947 were made that depicted the correlation between water surges (days of ascending flow <br />above 19,000 cfs pre-dam and 13,000 cfs post-dam) into wetlands and the average date for the <br />presence of drifting larval razorback suckers (calculated from Muth et al. 1998). From these <br />figures, a potentially good pre-dam year appears to be 1957 (Figure 2.2). We hypothesize this <br />year was good because of the duration of surging flows and the timing of these surges. <br />Assuming average bankf ill discharge of 19,000 cfs, water from the river would have been <br />surging into floodplain wetlands for a total of 18 days during this flood period. Secondly, many ... <br />of these "surge days" occurred later in the year when the likelihood razorbacks would be drifting <br />is greater. Based on these characteristics, the best year for both pre-dam and post-dam periods <br />was 1983. Surges would have occurred for a total of 36 days under the current levee removal x <br />flooding level of 13,000 cfs. And many of these days occurred later in the year. Another. <br />potential good post-dam year was 1995 (24 days of surges). For the three years of Le vee <br />Removal Study, 1996 and 1998 were poor years for larval access of floodplain wetands (Figure <br />16 ?"?