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The UKL Reserve is defined as the usable storage volume (above an elevation of 4,136.00 ft [1260.65 m]) in UKL on September 30 of each water year. Similar to the Project Supply and EWA, the UKL Reserve is initially determined on March 1. Note that although the water volumes for each of the Project Supply and EWA are for March 1 through September 30, these supplies of water are not required to be fully used by September 30, and may be used through November of the following water year. The KBPM is a critical tool for evaluation of possible water management. However, not all of the processes built into the model can be implemented during operations exactly as they were simulated. For example, the model uses patterns of irrigation water distribution on a monthly basis to simulate delivery of water to the Project. The distribution patterns were developed by analyzing historical irrigation demand and calculating an average percent distribution for each month during water years ranging from substantially drier than average to substantially wetter than average. Real-time implementation of the proposed action will not result in the same irrigation delivery distribution patterns. Similarly, the UKL Reserve and distribution of the EWA will be different operationally than simulated. However, the results of actual operations are anticipated to be within the upper and lower bounds of the simulated results (e.g., Klamath River flows at IGD, UKL elevations, and Project Supply), assuming that climate and hydrologic conditions occurring during the life of the proposed action are within the range of conditions observed in the POR used for modeling the proposed action. A detailed description of WRIMS model study 2L_MW_7_O is included in Appendix 4A-1, Model Documentation of Reclamation’s Biological Assessment (Reclamation 2012). 4.2.3.1 Fall/Winter Operations Water management from October through February will follow a formulaic approach focused on meeting the needs of coho salmon in the Klamath River while increasing water storage in UKL and providing fall/winter water deliveries to the Project and Lower Klamath NWR. This approach attempts to ensure adequate water storage and sucker habitat in UKL while providing variable river flows that mimic natural hydrology, based on real-time hydrologic conditions in the upper Klamath Basin. The fall/winter Klamath Project operational procedure distributes the available UKL inflows as described below. Additional details are included in Reclamation’s BA (Reclamation 2012). The primary goals of fall/winter water management are to: Increase the UKL elevation to meet listed species habitat needs and increase storage for spring/summer EWA releases and irrigation deliveries. Release sufficient flow from Link River Dam to meet listed species needs in the Klamath River. 17
Provide Project irrigation deliveries to: • Klamath Drainage District (Area A2 from North Canal and Ady Canal) • Lease Lands in Area K (Area A2 from Ady Canal) • Lower Klamath National Wildlife Refuge (from Ady Canal) To satisfy these goals for fall/winter water management, Reclamation will determine a flow release target from Link River Dam in real-time, using the series of steps and equations described below. The flow release target from Link River Dam combined with accretions downstream from Link River Dam is intended to provide at least minimum daily target flows below IGD, and flows greater than minimums when hydrologic conditions allow. IGD proposed average daily minimum target flows are 1,000 cfs (28.3 m 3 /sec) in October and November, and 950 cfs (26.9 m 3 /sec) in December, January, and February. In several water years during the POR, the model simulates a number of daily flows at IGD that are less than the minimum daily average target flows. This is because the model simulates a oneday time lag between flow releases at Link River Dam and flow at IGD. The one-day time lag combined with variability in accretions results in simulated flows lower than the minimum targets. Real-time implementation of the proposed action will result in increased releases from Link River Dam to ensure that flows meet or exceed the daily minimum average target flows at IGD. In addition, to allow flexibility for the possibility of operator error and uncertainties associated with flow releases at IGD, Reclamation proposes a maximum of a 5 percent reduction in flows below the minimum daily average flows at IGD, for up to a 72-hour duration. If such a flow reduction occurs, Reclamation proposes that the resulting average flow for the month will meet or exceed the associated minimum daily average flow (Reclamation 2013b). Flow in the Williamson River is the primary hydrologic indicator used to calculate a release target for Link River Dam. As described in more detail below, the initial calculated Link River Dam release target is modified based on several factors, including (1) magnitude of Williamson River flow, (2) rate at which UKL is filling, (3) accretions to the Klamath River below Link River Dam, and (4) any EWA carried over from the previous water year. Williamson River flows used in the modeling environment and during real-time operations are based on daily average flow at the U.S. Geological Survey (USGS) gage number 11512500 (Williamson River below Sprague River, near Chiloquin, Oregon). 4.2.3.1.1 Williamson River Proportion The previous day’s Williamson River average flow is multiplied by the appropriate proportion to calculate an initial Link River Dam flow release. The proportion of the Williamson River flow used to calculate the daily Link River Dam target release is adjusted based on the magnitude of the current Williamson River flow and the month. Higher Williamson River flow results in a greater proportion of inflow released at Link River Dam and lower Williamson River flow results in a lower proportion released. The flow proportion multipliers corresponding to specific Williamson River flows are presented in Table 4.2. Intermediate flow proportion multipliers are obtained by linear interpolation. 18
Page 1 and 2: National Marine Fisheries Service U
Page 3 and 4: 7.4.5 LRS and SNS Population Dynami
Page 5 and 6: 11.1.5 Critical Assumptions .......
Page 7 and 8: 16 APPENDICIES ....................
Page 9 and 10: Table 8.2 UKL end-of-month elevatio
Page 11 and 12: LIST OF FIGURES Figure 3.1. The act
Page 13 and 14: Figure 11.17. Coho salmon fry habit
Page 15 and 16: ABBREVIATIONS AND ACRONYMS Abbrevia
Page 17 and 18: Abbreviation/Acronym YTEP WDFW WRIM
Page 19 and 20: In 2001, the Services issued BiOps
Page 21 and 22: Findings of Fact and Order of Deter
Page 23 and 24: proposed changes to the vegetation
Page 25 and 26: Figure 3.1. The action area for Rec
Page 27 and 28: 4 PROPOSED ACTION Reclamation propo
Page 29 and 30: 4.2 Element Two Operate the Project
Page 31 and 32: October 1 and March 1. The proposed
Page 33: Reclamation incorporated the 1981 t
Page 37 and 38: Table 4.3. UKL fill rate adjustment
Page 39 and 40: Table 4.5. Calculation of fall/wint
Page 41 and 42: Flows below IGD are ultimately the
Page 43 and 44: The EWA, Project Supply, and UKL Re
Page 45 and 46: Table 4.8. Environmental Water Acco
Page 47 and 48: eleases somewhat on the ascending l
Page 49 and 50: fish disease, die off, entrainment,
Page 51 and 52: acre-feet when the Project Supply c
Page 53 and 54: Table 4.11. Monthly maximum Lower K
Page 55 and 56: 4.2.4 Ramp-Down Rates at Iron Gate
Page 57 and 58: progresses and EWA volumes are upda
Page 59 and 60: O&M activities are carried out eith
Page 61 and 62: 1. The A Canal has six headgates th
Page 63 and 64: Therefore, Reclamation proposes to
Page 65 and 66: coordinate with the NMFS to develop
Page 67 and 68: the confluence with Omogar Creek at
Page 69 and 70: though several major improvements t
Page 71 and 72: Sucker larvae transform into age-0
Page 73 and 74: units: (1) Clear Lake; (2) Tule Lak
Page 75 and 76: Figure 7.2. Adult spawning populati
Page 77 and 78: Table 7.1. Estimated LRS and SNS ad
Page 79 and 80: 1905, Ch. 567, 33 Stat. 714). The P
Page 81 and 82: Figure 7.4 Modeled April through No
Page 83 and 84: 7.9.2 Klamath Basin The Oregon Clim
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A change in mean precipitation rang
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Table 7.2 Impaired water bodies wit
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Table 7.3 Seasonal comparisons of p
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ammonia that is lethal to 50 percen
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Table 7.4 Estimated external phosph
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examination of juvenile suckers fro
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Evaluation of baseline hydrology in
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2012 1931 through 2012 12.6% 0.24 5
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The overall water year trend (Table
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Figure 7.7 Sprague River trends, wa
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Figure 7.9 Sprague River trends, wa
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Figure 7.12 Williamson River trends
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Figure 7.14 UKL trends, water years
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Figure 7.17 UKL: net inflow departu
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7.10.3.3 Competition and Predation
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By late July, surviving larval suck
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Threat Nature of Threat Life Stage
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2011) and increased adult spawning
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Based on the best available informa
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contrast, water levels began 1.5 ft
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evaporation and seepage estimated a
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prolonged low oxygen conditions if
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The April through September 4,034.6
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8 EFFECTS OF THE ACTION ON LOST RIV
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Although the volume of Project wate
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than 1 m), and fitting one or more
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Figure 8.3. UKL elevations at the e
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Services and Reclamation will deter
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For cumulative net inflow values be
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Figure 8.8. UKL elevations at the e
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Figure 8.10. UKL elevations at the
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Figure 8.12. UKL elevations at the
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natural and man-caused changes in i
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Table 8.1 UKL end-of-month surface
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UKL. Based on best available inform
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larvae in UKL. Annual production of
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Table 8.5 UKL end-of-month elevatio
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Based on our review of the literatu
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into the Pelican Bay water quality
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We assume that UKL surface elevatio
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vary by several orders of magnitude
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survival rates, we know that some o
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populations, and contains the large
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8.3.5.1 Effects to Adult Sucker Spa
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Table 8.8 Clear Lake surface elevat
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occur, especially in the west lobe.
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Table 8.9 End of the month surface
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8.3.7.4 Effects of Entrainment Loss
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The source of the sediment is unkno
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period when they migrate upstream t
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limited LRS and SNS persistence in
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term and localized and because fish
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8.5.1 Canal Salvage Reclamation pro
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high predation rates and failure of
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include the Klamath Basin Rangeland
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Figure 9.1 Designated CHUs for the
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These are discussed in greater deta
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The proposed action will have no ef
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No other spawning habitat exists be
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consulted on. Current monitoring da
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proposed action and this PCE suppor
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Because of a multi-decade lack of r
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Adverse effects of the proposed act
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that juvenile survival is most like
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elocation effort in Lake Ewauna to
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LRS and SNS population resiliency o
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stratum 4 (Interior Klamath) in whi
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Pacific salmonids Oncorhynchus spp.
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scenario, actions and elements of t
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flow prescriptions should mimic pro
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11.2.1 Current Condition of Critica
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11.2.2 Factors Affecting SONCC Coho
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e disoriented or displaced downstre
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enhancement, and rehabilitative act
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Water Temperature Sedimentation Org
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Figure 11.1 Longitudinal and season
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functioning floodplains that fail t
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downstream of IGD, (2) enhance coho
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few local ranchers and water distri
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in some tributaries, access to and
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11.3.7 Summary of Critical Habitat
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these two time periods, the effects
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consists of approximately 29,000 ac
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The PacifiCorp habitat conservation
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IGD, or used in constructed habitat
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estoration, watershed planning, sal
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Table 11.4. Modeled suspended sedim
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parasites Ceratomyxa shasta (causes
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that become infected is estimated t
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where snow water equivalent is proj
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minimizing disease risks, the detai
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Figure 11.4. Proposed action, histo
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Figure 11.6. Proposed action weekly
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Figure 11.9. Regression between EWA
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Figure 11.11. Proposed action and o
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Figure 11.12. Number of days per wa
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Figure 11.14. Monthly coefficient o
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IGD. The proposed action modeled da
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The results from Table 11.7 indicat
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likely to increase the quantity of
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habitat decreases between the Shast
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Table 11.9. Daily average mainstem
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Table 11.10. Daily average mainstem
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5% 3336 13176 27664 26168 30946 237
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The proposed action results in agri
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Figure 11.21. Monthly mean of daily
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Riparian restoration projects will
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expected to be typical riparian spe
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Table 11.13. Annual percent of proj
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esource needs as they grow, and 3)
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11.5.2 Klamath River Basin Adjudica
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coho salmon within the Klamath Rive
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aspects of a natural flow regime th
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element of coho salmon critical hab
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12.1.1.1 Risk Analyses for Endanger
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ESU DIVERSITY STRATA POPULATIONS IN
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eproduction, and distribution. The
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Figure 12.2. Historic population st
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the average ratio of IP-km to total
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Although long-term data on coho sal
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1980 1981 1982 1983 1984 1985 1986
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maintain viable abundances in many
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12.2.5.5 Viability Summary Though p
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coastal currents and upwelling, kno
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12.2.6.2 Marine Derived Nutrients M
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fisheries south of Cape Falcon, Ore
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12.3 Environmental Baseline of Coho
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water temperatures up to 19 ºC in
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some coho salmon smolts may stop mi
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threshold, all Klamath River coho s
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abundance threshold (Table 12.3). T
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mainstem Klamath and Trinity rivers
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Although there are risks to Klamath
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activities are generally beneficial
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12.4 Effects to Individuals The pro
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12.4.1.2 Response 12.4.1.2.1 Adults
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(2012) believes is representative o
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genotype II density of 5 spores/L w
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flows provide a limit to the increa
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polychaete and sediment disturbance
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which will likely result in a relat
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etween Trees of Heaven (RM 172) and
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action. Reclamation estimated that
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Based on literature, increased comp
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Table 12.6. Summary of risks result
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most juveniles. Stream flow diversi
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at most fish relocation sites, base
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higher, the minimally increased sed
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Small pulses of moderately turbid w
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Boulder faces in the deflector stru
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conditions may fail if those condit
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Adverse effects of the proposed act
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Potential Stressor Habitat Reductio
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Potential Stressor Elevated water t
Page 393 and 394:
12.6.2 Effects of fitness consequen
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13 INCIDENTAL TAKE STATEMENT Sectio
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Table 13.1 Summary of maximum annua
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in fewer larvae and juveniles, and
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Table 13.2 Estimated annual maximum
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1.2.1.8. Incidental Take Caused by
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characteristics of aquatic species,
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Table 13.5 Expected annual Environm
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Cause of Incidental Take Habitat Re
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Clear Lake, Gerber Reservoir, and T
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This term and condition is requirin
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13.4 Mandatory Monitoring and Repor
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Required hydrologic monitoring incl
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Table 13.7. Summary of LRS and SNS
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T&C or Mandatory Monitoring Mandato
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Table 13.9 Summary of reporting and
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Table 13.10 Summary of meetings req
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the above QA/QC procedures describe
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Barry, P.M., E.C. Janney, D.A. Hewi
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Burdick, S.M. and J. Rasmussen. 201
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Dunsmoor, L., L. Basdekas, B. Wood,
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Garen, D. 2011, Upper Klamath Basin
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Janney, E.C., B.S. Hayes, D.A. Hewi
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Laenen, A., and A.P. LeTourneau. 19
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Miller, R.R., and G.R. Smith. 1981.
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Perkins, D.L., and G.G. Scoppettone
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(Deltistes luxatus) in Tule and Cle
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Terwilliger, M. 2006. Physical habi
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USBR [U.S. Bureau of Reclamation].
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Williams, J.E. 2000. Chapter 13. Th
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Arthington, A.H., S.E. Bunn, N.L. P
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Beeman, J., S. Juhnke, G. Stutzer a
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Brommer, J.E. 2000. The evolution o
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Department of the Army Regional Gen
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Chilcote, M. W. 2003. Relationship
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Dunsmoor LK, and Huntington CW. 200
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Foott, J.S., R. Stone, E. Wiseman,
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Habera, J.W., R.J. Strange, B.D. Ca
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Hemstreet, T. 2013. Electronic mail
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Jordan, M. S. 2012. Hydraulic predi
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Kostow, K. E., A. R. Marshall and S
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MacFarlane, R. B., S. Hayes, and B.
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Moyle, P. B. 2002. Inland Fishes of
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PacifiCorp Klamath Hydroelectric Pr
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Oregon Department of Environmental
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Puckridge, J. T., F. Sheldon, K. F.
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Ring, T.E. and B. Watson. 1999. Eff
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Sommer, T. R., M. L. Nobriga, W. C.
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Taylor, R. 1991. A review of local
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USFWS [U. S. Fish and Wildlife Serv
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Ward G, and Armstrong N. 2010. Asse
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Winker, K., J. H. Rappole, and M. A
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77 FR 476. National Marine Fisherie
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UKL Elevation (feet) Active Storage
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16.2 Appendix B: Elevation Flow Dat
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490
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Week of Water Year 1981 1982 1983 1
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Water Year October November Decembe
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16.3 Appendix C: Description of Res
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4. Removal of Small Dams (permanent
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Information regarding consideration
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9. Piping Ditches a. Project Descri
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. Site-Specific Restrictions Restri
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6. Protection Measures The followin
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to enter or be placed where they co
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shall be distributed throughout the
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weed free straw, silt fences) are i
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the project is located, and compris
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2. Post Construction Monitoring and
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Median Seasonal Flow (acre-feet) Me
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Median Seasonal Net Inflow (acre-fe
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16.5 Appendix E: Observed and Model
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Observed and modeled proposed actio
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Observed and modeled proposed actio
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16.6 Appendix F: Analyzing the rela
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Table 1. Paired comparison of the c
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Table 3. The difference in the mean
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