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Biological Opinions - Bureau of Reclamation

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scenario, actions and elements <strong>of</strong> the baseline within <strong>Reclamation</strong>’s discretion are removed from<br />

the hydrological setting under a No-Project scenario.<br />

In 2007, <strong>Reclamation</strong> provided NMFS and USFWS a No-Project hydrology that included critical<br />

assumptions given a hypothetical scenario in which <strong>Reclamation</strong> would no longer deliver water<br />

to the Klamath Project. Key assumptions included: (1) UKL will be a level pool and not<br />

affected by wind; and (2) the reef at Link River dam would be reconstructed, recreating the<br />

original reef elevation stage-discharge relationship (NMFS 2010a).<br />

Prior to completing <strong>Reclamation</strong>’s 2012 BA, the Services and <strong>Reclamation</strong> discussed the<br />

potential <strong>of</strong> developing a No-Project hydrology for this consultation. NMFS, USFWS, and<br />

<strong>Reclamation</strong> mutually agreed, during informal consultation, that developing a No-Project<br />

hydrology for the purpose <strong>of</strong> analyzing the effects <strong>of</strong> <strong>Reclamation</strong>’s proposed action on listed<br />

species was not prudent because the agencies were not able to find consensus on approaches to<br />

address critical assumptions necessary to define a No-Project condition. Concerns with the<br />

above-described assumptions, combined with the Services’ determination that their analytical<br />

approach was not dependent on a No-Project hydrology led <strong>Reclamation</strong> to not model a No-<br />

Project hydrology. NMFS determined on January 8, 2013, it had sufficient information to<br />

initiate formal consultation based on the biological assessment, and NMFS and USFWS have<br />

since proceeded with formal consultation and drafting the joint BiOps based on the biological<br />

assessment and critical assumptions described in this BiOp.<br />

On April 8, 2013, the Hoopa Valley Tribe submitted to NMFS, model output from a No-Project<br />

hydrological scenario and associated flow/habitat relationship data, analyzing habitat availability<br />

under a No-Project hydrology. NMFS has not had sufficient resources to do more than a cursory<br />

evaluation <strong>of</strong> the model structure and assumptions supporting the No-Project hydrological<br />

scenario, nor has it had sufficient resources to evaluate it with USFWS and <strong>Reclamation</strong>, while<br />

also proceeding with drafting the BiOp as required under the ESA and implementing regulations.<br />

While NMFS is appreciative <strong>of</strong> the Tribe’s efforts to advance our understanding <strong>of</strong> the effects <strong>of</strong><br />

the Proposed Action, NMFS has identified some potential problems with the model structure and<br />

assumptions in NMFS’ cursory review <strong>of</strong> it, and NMFS is cautious <strong>of</strong> using hydrological data in<br />

which the critical assumptions <strong>of</strong> water routing have not been evaluated by <strong>Reclamation</strong>,<br />

USFWS, and NMFS. However, NMFS will further evaluate the No-Project hydrological<br />

scenario in coordination with <strong>Reclamation</strong> and USFWS to determine whether it is a reasonable<br />

representation <strong>of</strong> no-project flows and reveals effects <strong>of</strong> the action that may affect listed species<br />

or critical habitat in a manner or to an extent not previously considered. If so, reinitiation <strong>of</strong><br />

formal consultation will be required under 50 CFR 402.16.<br />

Therefore, NMFS does not use a modeled No-Project flow to quantitatively compare the flow<br />

effects <strong>of</strong> the proposed action for this consultation. However, NMFS can reasonably assume the<br />

proposed action reduces mainstem flow volume in the Klamath River throughout most <strong>of</strong> the<br />

year because the Project diverts water during the spring and summer (and fall and winter to a<br />

lesser degree) and stores water in UKL in the fall and winter. Using Hardy’s (2012) coho<br />

salmon fry and Hardy et al.’s (2006) juvenile data, NMFS identified the range <strong>of</strong> flows for the<br />

mainstem reaches downstream <strong>of</strong> IGD where there is a positive correlation between flow and<br />

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