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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: Factors Affecting Species Environment<br />

small tributary flows. The NAS also hypothesized that adding substantial amounts of<br />

warm water could reduce the size of these thermal shelters, although that hypothes<strong>is</strong> was<br />

not supported by research at the Red Cap Creek thermal refuge (Benson and Holt<br />

2005) 34 .<br />

Generally, during late spring and early summer, flows from Iron Gate Reservoir tend to<br />

be below equilibrium temperature on the order of 2 to 4 ºC. However, the effect <strong>is</strong><br />

dimin<strong>is</strong>hed with increased d<strong>is</strong>tance from the dam. The cooler water temperature <strong>is</strong><br />

attributed to the source of the water, the IGD reservoir. Note that the warmest reach of<br />

the <strong>Klamath</strong> River <strong>is</strong> between Scott River and Shasta River.<br />

Figure 3-15. Longitudinal view of daily mean water temperatures from IGD to Turwar, on June 1<br />

in a typical year.<br />

12-13C<br />

13-14<br />

14-15<br />

15-16<br />

16-17<br />

17-18<br />

15 °C or cooler 15 °C or warmer<br />

Scott<br />

.<br />

River<br />

Iron Gate Dam<br />

.<br />

Shasta River<br />

Turwar<br />

.<br />

Salmon River<br />

Trinity . R<br />

Source: Figure 5, p. 9, Cramer F<strong>is</strong>h Sciences 2007 Technical Memorandum 7.<br />

34<br />

National Academy of Science <strong>new</strong>s release dated February 6, 2002. News release obtained on July<br />

5, 2007 at http: //www8.nationalacademies.org/onpi<strong>new</strong>s/<strong>new</strong>sitem.aspx?RecordID=10296<br />

222

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