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Our new Biological Assessment is out - Klamath Basin Crisis

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: Factors Affecting Species Environment<br />

may be warmer than equilibrium temperature. The effects of th<strong>is</strong> thermal lag dimin<strong>is</strong>h<br />

with d<strong>is</strong>tance downstream.<br />

The temperature modeling indicated that tributary inputs and meteorological conditions<br />

are the primary temperature drivers through<strong>out</strong> the year downstream from the Scott<br />

River. Thus, the ability to control temperature in the lower <strong>Klamath</strong> River through flow<br />

management at IGD <strong>is</strong> limited because ambient temperatures and tributary flows<br />

downstream are much larger than those from IGD, depending on season and annual<br />

variability (see earlier Figure 3-16).<br />

During smolt <strong>out</strong>-migration, the Proposed Action has some effect on temperatures<br />

downstream of IGD; however, temperatures remain within the optimum range for<br />

survival during the majority of the smolt migration for a wide range of flow releases (see<br />

Appendix 3-C), and therefore has a limited effect on smolt survival.<br />

Later in the spring and on through the summer, temperatures exceed tolerable levels and<br />

coho salmon are relegated to thermal refugia through<strong>out</strong> most of the main stem or must<br />

migrate into non-natal tributaries (Figure 3-17). During summer, releases from IGD have<br />

little influence on temperatures downriver of the Shasta River. Thus, high temperatures<br />

in the <strong>Klamath</strong> River sharply limit the rearing capacity for coho salmon in the main stem<br />

during summer, and heat energy balances dictate that releases of any magnitude from<br />

IGD can have little influence below the Shasta River (Cramer F<strong>is</strong>h Sciences 2007<br />

Technical Memorandum 5).<br />

Figure 3-17. Longitudinal profile of daily maximum, mean, and minimum water temperatures in<br />

the <strong>Klamath</strong> River for July 1 (top graph), August 1 (middle graph) and September 1 (bottom<br />

graph), as predicted from the temperature model, given 2001 meteorology and tributary flows.<br />

30<br />

25<br />

Temperature (C)<br />

20<br />

15<br />

10<br />

5<br />

0<br />

Shasta River<br />

Scott River<br />

185 175 165 155 145 135 125 115 105<br />

95<br />

85<br />

Salmon River<br />

Trinity River<br />

75 65 55 45 35<br />

25<br />

15<br />

5<br />

Mean<br />

Max<br />

Min<br />

River Mile<br />

1-Jul<br />

225

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