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Biological Opinions - Bureau of Reclamation

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Table 4.3. UKL fill rate adjustment factor.<br />

Fill_rate_diff (ft/day) Fill_rate_adjust_wet Fill_rate_adjust_dry<br />

< -0.02 0.6 0.2<br />

0 1.0 1.0<br />

> 0.03 1.4 1.0<br />

“Fill_rate_diff” is the difference between the recent fill rate <strong>of</strong> UKL and the average fill rate<br />

needed to reach 4,142.80 ft (1,262.73 m) on March 1. Positive values indicate recent fill rates<br />

exceed the average rate needed to reach 4,142.80 ft (1,262.73 m) on March 1. Negative values<br />

indicate recent fill rates are less than the average rate needed to reach 4,142.80 ft (1,262.73 m)<br />

on March 1.<br />

The “wet” and “dry” modifiers to the fill rate adjustment term are defined by the UKL<br />

cumulative inflow index. The UKL cumulative inflow index (Upper Klamath<br />

Lake_cum_inf_ind) is not calculated by the model, but instead is part <strong>of</strong> the model input<br />

dataset. Because the model does not calculate the index, it must be calculated on a daily basis<br />

during real-time operations over the life <strong>of</strong> the proposed action, as follows:<br />

Upper Klamath Lake Index =<br />

The day t-1 term indicates the value on the previous day. The index is then normalized between<br />

0 and 1. Drier hydrologic conditions are defined as a value <strong>of</strong> the UKL cumulative inflow<br />

index less than 0.30. An index value greater than 0.30 indicates any condition not defined as<br />

dry but does not distinguish between average or wet conditions.<br />

4.2.3.1.3 Net Accretion Adjustment<br />

Releases from IGD can be greatly affected by the accretions between Link River Dam and IGD.<br />

Low net accretions may result in the need to release more water from Link River Dam to<br />

produce calculated IGD flows. High net accretions may result in less water being released from<br />

Link River Dam to meet calculated IGD flows. The accretion adjustment modifies Link River<br />

Dam releases in all hydrologic conditions between October 1 and November 15. Therefore,<br />

higher releases at Link River Dam may <strong>of</strong>fset low seasonal accretions downstream. Although<br />

values are included in Table 4.4 for all conditions, the accretion adjustment is applied after<br />

November 15 only in relatively dry conditions (defined by an UKL cumulative inflow index<br />

value less than 0.30), when accretions below Link River dam are low and the accretion<br />

adjustment is necessary to meet calculated IGD flows. Accretion adjustment multipliers are<br />

presented in Table 4.4. As with other adjustment factors, intermediate multiplier values are<br />

obtained by linear interpolation.<br />

20

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