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<br />" <br /> <br />392 <br /> <br />j, KORMAN, S, M, WIELE AND M, TORIZZO <br /> <br />Table V. Effects of dam operations on the availability of suitable shoreline habitat for the seven study rel:l.cl'Ies. Plus and minus <br />~igns deoOlc whelher operatiol\':. have increas.ed or decreased suitable shoreline hiibitat 3\aitabi!ity relative to pre-dam condi- <br />tions. The number of symbols denotes the signiJ1cance level of the operations effect3- <br /> RI R2 R3 R4 R5 ALe PAL <br />JiJnuary <br />Febnlary +++ <br />March +++ ++ <br />April +++ +++ + + <br />May +++ +++ + +++ +++ +++ ++ <br />June +++ +++ ++ +++ +++ +++ <br />July <br />August <br />September <br />Ocwber <br />November ++ <br />December <br />No. positive effects 2 6 2 2 4 3 2 <br />No. negative effects 8 2 8 8 4 8 3 <br />A+. _, P ~ 0.05; ++. --, P ~ O.OI~ +++. -- -, p ~ 0.001. <br /> <br />The large changes in the extent of daily variation in discharge under different operating periods (Figure 8) had a <br />strong effect on the amount of suitable habitat ?rea that persisted across typical daily discharge ranges (Table VI). We <br />used September as an index month for this analysis because the average daily discharge range was well represented <br />by the discharges that we modelled in this study (Table II), and with discharge ranges seen in other months. During <br />the pre-dam period. the daily range in discharge for September was minimal. increased to 226-566 m'/s during the <br />'no action' period, and was reduced to 425-566 m',s under the current operating regime (MLFF). Persistent suitable <br />shoreline habitat was almost completely eliminated in the post-dam period under the 'no action' regime at all sites. <br />The reduction in daily variation in discharge under the MLFF regime resulted in the persistence of small amounts of <br />suitable habitat at all reaches except PAL, where the increase was much larger, The amount of persistent total suitable <br />habitat in the pre-dam period was reduced by 60-90% under the 'no action' regime at all study reaches and by 50- <br />70% under the MLFF regime for all reaches except PAL, where the reduction was only 20%. <br /> <br />EfJecls of discharge and calch per unil effort indexing <br /> <br />The potential for discharge changes to increase variatio,n in ePE data was highly variable among reaches. The <br />190 electrofishing samples taken in 1993 between river km 99 and 107 were collected over a discharge range of 175 <br />to 550m'/s. but more than 80% were collected over a narrower range of 200 and 4oom'Is (Figure 9). In the worst <br />case (R4), the amount of suitable shoreline habitat area decreased fourfold over the 200-400 m',s range, Under the <br />assumption of an inverse linear relationship between suitable habitat area and catchability (Equation I), this <br />change implies thai ePE deosities taken at 400 m3 'S could be fourfold greater than those taken at 200 m'ls, <br />Reaches RI and ALe showed potential for variations in ePE densities as high as Iwo- and 1.5.fold. respectively, <br />over this same discharge range, whereas R3 and R5, where suitable shoreline habitat area was relatively insensitive <br />to changes in discharge. showed little potential for increased variability even at the extreme ends of the discharge <br />range where sampling was conducted. Reaches R2 and PAL showed a limited potential for ePE estimates to <br />decrease at higher discharges because of increases in suitable shoreline habitat area. <br /> <br />Dispersal <br /> <br />The ability of a reach to retain particles tended to decline with increasing discharge, but the pattern varied con- <br />siderably owing to differences in the morphology among reaches and the swimming behaviours that were modelled <br />(Figure 10). In general, the more effective the behaviour at moving a particle to the low-velocity area near the <br />banks, the higher the retention rate, Thus, a geotactic behaviour, where all the swimming velocity is focused in <br /> <br />Copyright <<) 2004 John Wiley & Sons. lid. <br /> <br />Ri\.tr Rtf. Applic. 20: 379-400 (2004) <br />