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Our new Biological Assessment is out - Klamath Basin Crisis

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<strong>Klamath</strong> Project Operations <strong>Biological</strong> <strong>Assessment</strong><br />

Coho Salmon: Effects of the Proposed Action on Coho Salmon<br />

Simulation of the Proposed Action showed that a wide range of flow releases<br />

from IGD had little effect on coho salmon smolt production from the <strong>Klamath</strong><br />

River <strong>Basin</strong> (Figure 3-29). The downstream effects from a different set of<br />

meteorology and tributary flows had a far greater effect on smolt production<br />

(approximately a 35 percent increase) than did increasing IGD flows from a 90<br />

percent exceedence to a 40 percent exceedence (approximately a 10 percent<br />

increase). Th<strong>is</strong> <strong>is</strong> a dramatic result, which the modeling revealed was caused by<br />

the inability of flows from IGD to produce suitable rearing temperatures for coho<br />

salmon during summer in the main stem below the Shasta River. If the<br />

temperature model had also been populated with a high runoff year such as 2006,<br />

another substantial increase in smolt production above the 2004 condition would<br />

have been indicated.<br />

Figure 3-29. Total simulated smolt production in year 10 using proposed flows (modeled<br />

2008 to 2018) at IGD for the 2001 and 2004 water year types.<br />

2001 Water Year Type<br />

Simulated smolt production (thousands)<br />

72<br />

70<br />

68<br />

66<br />

64<br />

62<br />

Baseline<br />

Proposed action<br />

0.9 0.8 0.7 0.6 0.5 0.4<br />

Flow exceedence probability<br />

The simulation results (d<strong>is</strong>played in Figure 3-29) suggest that the population can<br />

endure even in adverse environmental conditions in freshwater. Although smolt<br />

production <strong>is</strong> less than for the 2004 conditions when compared to 2001 tributary<br />

conditions, the simulated population did not collapse after four generations of<br />

continuous extreme drought (90 percent exceedence releases with 2001<br />

meteorology and tributary flows).<br />

An analys<strong>is</strong> was also completed for the smolt production under the Proposed<br />

Action and the smolt production under h<strong>is</strong>toric operations with a similar water<br />

year. Under all low modeled flow conditions (less than or equal to 50 percent<br />

exceedence) smolt production was 1 to 2 percent greater under the Proposed<br />

Action for conditions set either at 2001 or 2004 (Figure 3-30 and Figure 3-31).<br />

266

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