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relationships between flow fluctuations and redd dewatering and ...

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juvenile str<strong>and</strong>ing, the results of the <strong>redd</strong> <strong>dewatering</strong> analysis indicate that, as expected, greater<br />

drops in <strong>flow</strong> result in a greater percentage of salmon <strong>and</strong> steelhead/rainbow trout <strong>redd</strong>s being<br />

dewatered. However, the <strong>redd</strong> <strong>dewatering</strong> analysis did not show <strong>flow</strong> threshold patterns, as<br />

were observed for juvenile str<strong>and</strong>ing.<br />

A basic assumption of all instream <strong>flow</strong> studies is that a stream is in dynamic equilibrium. When<br />

a channel is in dynamic equilibrium, there is an approximate balance <strong>between</strong> sediment supply<br />

<strong>and</strong> transport, so that the channel pattern <strong>and</strong> cross-sectional profile of the entire stream is<br />

consistent (Bovee 1996). For a stream in dynamic equilibrium, it would be expected that large<br />

<strong>flow</strong> events would not result in a significant change in <strong>flow</strong>-habitat <strong>relationships</strong>. Recent high<br />

<strong>flow</strong>s on the Yuba River (Figure 13) have resulted in significant channel changes. While we do<br />

not have direct evidence that the Yuba River is in dynamic equilibrium, our findings on the<br />

American River that the January 1997 flood did not result in a substantial change in Chinook<br />

salmon or steelhead spawning <strong>flow</strong>-habitat <strong>relationships</strong> (US Fish <strong>and</strong> Wildlife Service 2000)<br />

offer support that the results of this study are still applicable to the Yuba River.<br />

USFWS, SFWO, Energy Planning <strong>and</strong> Instream Flow Branch<br />

Yuba River Redd Dewatering <strong>and</strong> Juvenile Str<strong>and</strong>ing Report<br />

September 15, 2010<br />

CONCLUSION<br />

The model developed in this study is predictive for <strong>flow</strong>s ranging from 400 cfs to 4,500 cfs for<br />

<strong>redd</strong> <strong>dewatering</strong> <strong>and</strong> juvenile str<strong>and</strong>ing upstream of Daguerre Point Dam, <strong>and</strong> for <strong>flow</strong>s ranging<br />

from 150 cfs to 4,500 cfs downstream of Daguerre Point Dam. This study supported <strong>and</strong><br />

achieved the objective of modeling the effects of <strong>flow</strong> decreases on Chinook salmon <strong>and</strong><br />

steelhead/rainbow trout spawning habitat <strong>and</strong> maximum potential juvenile entrapment in the<br />

Yuba River <strong>between</strong> Englebright Dam <strong>and</strong> the Feather River.<br />

REFERENCES<br />

Becker, C.D., D.A. Neitzel <strong>and</strong> D.H. Fickeisen. 1982. Effects of <strong>dewatering</strong> on Chinook salmon<br />

<strong>redd</strong>s: tolerance of four developmental phases to daily <strong>dewatering</strong>s. Transactions of the<br />

American Fisheries Society 111: 624-637.<br />

Bovee, K.D., editor. 1996. The Complete IFIM: A Coursebook for IF 250. U.S. Geological<br />

Survey, Fort Collins, CO.<br />

Bradford, M.J., G.C. Taylor, J.A. Allen <strong>and</strong> P.S. Higgins. 1995. An experimental study of the<br />

str<strong>and</strong>ing of juvenile coho salmon <strong>and</strong> rainbow trout during rapid <strong>flow</strong> decreases under<br />

winter conditions. North American Journal of Fisheries Management 15: 473-379.<br />

California Department of Fish <strong>and</strong> Game. 2001. Evaluation of effects of <strong>flow</strong> <strong>fluctuations</strong> on<br />

the anadromous fish populations in the Lower American River. Sacramento, CA:<br />

California Department of Fish <strong>and</strong> Game, Stream Evaluation Program, Technical Report<br />

No. 01-2.<br />

27

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