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Chinook salmon <br /> The fall-/late fall-run of Chinook salmon is currently the largest run of Chinook salmon in the San Joaquin River <br /> system. Because fall-/late fall-run Chinook salmon represent the greatest proportion of all four runs in the Central <br /> Valley,they continue to support commercial and recreational fisheries of significant economic importance. On <br /> September 16, 1999 (64 FR 50393),NMFS determined that listing was not warranted for the Central Valley fall- <br /> /late fall-run Chinook salmon ESU. However,the ESU was designated as a candidate for listing due to concerns <br /> over specific risk factors. On April 14,2004(69 FR 19975)the ESU was reclassified as a species of concern. The <br /> ESU includes all naturally spawned populations of fall-run Chinook salmon in the Sacramento and San Joaquin <br /> River Basins and their tributaries, east of Carquinez Strait. <br /> Chinook salmon adult migration—In general, adult fall-/late fall-run Chinook salmon migrate into the Sacramento <br /> River and its tributaries from July through December,with immigration peaking from mid-October through <br /> November(Exhibit 4.13-2). Fall-/late fall-run Chinook salmon spawn in tributaries of the San Joaquin River, <br /> including the Stanislaus River, Tuolumne River, and Merced River, several miles upstream of the project site. <br /> Optimum water temperatures for adult Chinook salmon migration have been reported to range from <br /> approximately 49 to 58 degrees Fahrenheit(°F),with adult migration continuing to occur at temperatures up to <br /> approximately 68°F (Bell 1973). <br /> Optimal temperatures generally range from 507 to 59°F for adult Chinook salmon migration and pre-spawning <br /> activity. Consistent temperatures of 60°F to 64°F are considered acceptable for migration by NMFS and U.S. <br /> Environmental Protection Agency(EPA), and EPA's criteria for migration is 68°F if there are thermal refuges in <br /> the system allowing fish to migrate and hold in cooler areas for some part of the migration period. This suggests a <br /> relatively slow increase in adverse thermal effects from 60°F to 68°F,where several types of low chronic stress <br /> have been documented(Berman 1990;Marine 1992; Poole et al. 2001), including potential for reduced swimming <br /> speed, increased disease, and reduced fecundity. There is reasonable agreement that consistent temperatures in the <br /> 64°F to 68°F range are somewhat stressful and create stress even with short-term exposure times of days to <br /> weeks. Above 68°F, disease rates have been documented to be quite high, including 100%mortality from disease <br /> outbreaks (Berman 1990). Because disease is a significant concern, and higher temperatures are clearly related to <br /> increased disease incidence and lethality, it is reasonable to assume that the adverse effects curve begins to <br /> steepen rapidly at higher temperatures and longer exposure times. <br /> Based on available information,the following temperature guidelines have been identified for adult Chinook <br /> salmon: <br /> ► Optimal range: 50°F to 60°F <br /> ► Range of increasing adverse effects: 61°F to 68°F <br /> ► Lethal effects: >68°F <br /> ► Behavioral avoidance: reported at 68°F <br /> Chinook salmon juvenile rearing and migration—Juvenile fall-run Chinook salmon emigrate from San Joaquin <br /> River tributaries (e.g., Stanislaus,Merced, and Tuolumne rivers)and other river tributaries to the delta during the <br /> late winter and spring(February—mid-June) (San Joaquin River Group 2001,2002, 2003,2004, 2005; CDFG <br /> unpublished data). <br /> Within a range of approximately 50°F to 60°F,warming temperatures appear to increase growth rates of rearing <br /> Chinook salmon and temperatures in this range are considered optimal or acceptable. Low-level stresses such as <br /> smolting problems may occur within and outside of this range,but high growth rates may be sustained in the 59°F <br /> to 66°F range, somewhat offsetting potential disease problems. <br /> Bartholow and Henriksen(2004)evaluated fall-run Chinook salmon mortality over a range of mean weekly water <br /> temperatures(constant daily mean temperature exposure, assuming variation throughout the day). Their analysis <br /> is consistent with an optimum high threshold of 60°F,where they find daily mortality rates are very low. They <br /> EDAW Manteca WQCF and Collection System Master Plans EIR <br /> Fisheries and Aquatic Resources 4.13-6 City of Manteca <br />