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Scientific Investigations Report 2013–5135

Modeling the Water-Quality Effects of Changes to the Klamath River Upstream of Keno Dam, Oregon

Table 14. Final parameter estimates of the non-linear regression model for major inputs at selected sites in the Link-Keno reach of the Klamath River, Oregon, 2006–09.

[From Mohseni and others, 1998. Temperature values are in degrees Celsius. α, minimum water temperature. β, air temperature at the point of inflection. γ, slope at the inflection point]

Boundary or source Limb α β γ
Link River Rising, falling 24.6 9.2 0.199
Lost River Diversion Channel Rising, falling 24.3 8.5 0.201
Klamath Straits Drain Rising 25.4 8.1 0.219
Falling 26.2 9.8 0.192

First posted July 24, 2013

For additional information contact:
Director, Oregon Water Science Center
U.S. Geological Survey
2130 SW 5th Avenue
Portland, Oregon 97201

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