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