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Draft EIS_072312.pdf - Middle Fork American River Project ...

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20120723-4002 FERC PDF (Unofficial) 07/23/2012<br />

Minimum flow increases in the peaking and bypassed reaches in the wettest water<br />

year types would increase wetted stream perimeter, which may increase habitat area and<br />

habitat diversity in some reaches for fish and aquatic invertebrates. Increased edge habitat<br />

may improve rearing success of YOY fish in wet water years if shallow water or cover is<br />

available to increase their ability to avoid aquatic and terrestrial predation. Higher<br />

minimum flows should provide more area for aquatic macroinvertebrate communities<br />

that make up a large portion of the diet of trout and other fish.<br />

The range of proposed minimum flows in the peaking reach would be from 75 to<br />

450 cfs, whereas the Alternative 1 minimum flows would range from 90 to 450 cfs.<br />

However, many of the Alternative 1 minimum flows would be from 15 to 100 cfs higher<br />

than the comparable proposed minimum flows for comparable water years and time<br />

frames. For the reasons stated in the previous paragraph, this prevailing higher minimum<br />

flow would result in the Alternative 1 regime providing minor habitat enhancements<br />

compared with the proposed flow regime. However, we expect the primary factor that<br />

would limit the quality and quantity of aquatic habitat in the peaking reach to be flow<br />

fluctuations, rather than minimum flows. Daily peaking flow fluctuations would be<br />

maintained under both action alternatives, and effects of the new minimum flow regime<br />

in the peaking reach on fish and other aquatic biota are expected to be negligible because<br />

changes in wetted habitat area would be of very short duration and likely insufficient to<br />

affect behavior (e.g., foraging), food availability, or production of aquatic biota.<br />

Typically, the period of snowmelt and high runoff occurs between April through<br />

mid-June in the basin and the spring pulse flows in the action alternatives reflect this<br />

timing. Restoring flows that mimic the spring snowmelt pulse may provide benefits to<br />

the aquatic community by helping to maintain a variety of seasonal life-history behaviors.<br />

Spring minimum flows would be substantially higher than under existing conditions in all<br />

water-year types under both action alternatives and, when coupled with the pulse flow<br />

releases (see section 3.3.1.2, Geologic and Soils Resources, table 3.3.1-2), would provide<br />

flow changes that simulate those found under unregulated conditions during the seasonal<br />

snowmelt period. Both the proposed and Alternative 1 minimum flows would enhance<br />

flow conditions for spawning by resident rainbow trout during spring (i.e., mid-March to<br />

June), based on the results of PCWA’s instream flow analysis (PCWA, 2010b). Higher<br />

spring flows may provide access to additional spawning or rearing habitat but may also<br />

act to scour redds in some years, both of which occur under natural stream conditions.<br />

Precipitation in the <strong>Middle</strong> <strong>Fork</strong> <strong>American</strong> <strong>River</strong> watershed has high inter-annual<br />

variation; water-year types tend to be either wet or dry, with few years receiving<br />

“average” precipitation. Under existing conditions, no provision is made for within-year<br />

or between-year variation in flows to reflect local seasonal changes and water year types.<br />

Many fish and aquatic macroinvertebrate species may use changes in flows as cues for<br />

behaviors such as spawning or movements into appropriate winter or summer habitat.<br />

Year-to-year variations in flows may maintain species diversity by benefiting certain<br />

species in wet years and others in dry years. Western streams with intact seasonal flow<br />

variation are believed to be more resistant to invasion by fish from eastern U.S. streams<br />

107

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