KR/KL Burbot Conservation Strategy
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Kootenay System Operations
Columbia River Treaty Review – Technical Studies Appendix C Kootenay System Operations Operation of the Kootenay River system is complicated as it is administered by several different jurisdictions and the hydroelectric facilities are owned by different agencies/companies. As shown in Figure 1, the Kootenay River originates in the Rocky Mountains not far from Field, BC. The river flows south, within a few km of the source of the Columbia River at Canal Flats, and then continues south into Koocanusa Reservoir, formed behind Libby Dam in Montana, United States. From Libby, the Kootenay River turns west and north, and re-enters British Columbia near the community of Creston, flowing into the south arm of Kootenay Lake. In the northern part of the Kootenay basin, the Duncan River is joined by the Lardeau River just downstream from Duncan Dam, and then flows into the north arm of Kootenay Lake. Water from the north and south arms of Kootenay Lake then flows through the west arm of the lake and past the Corra Linn Dam near Nelson (as well as other dams) en route to the Columbia–Kootenay confluence at Castlegar. The components of this system and various agreements/orders that regulate flows are described in this Appendix. November 29, 2013 1 Columbia River Treaty Review – Technical Studies Figure 1: Kootenay and Columbia Region November 29, 2013 2 Columbia River Treaty Review – Technical Studies 1.0 Coordination of Libby Operations Background Under the terms of the Columbia River Treaty, Canada permitted the U.S. to build the Libby Dam on the Kootenai River (U.S. -
Ethnohistory of the Kootenai Indians
University of Montana ScholarWorks at University of Montana Graduate Student Theses, Dissertations, & Professional Papers Graduate School 1983 Ethnohistory of the Kootenai Indians Cynthia J. Manning The University of Montana Follow this and additional works at: https://scholarworks.umt.edu/etd Let us know how access to this document benefits ou.y Recommended Citation Manning, Cynthia J., "Ethnohistory of the Kootenai Indians" (1983). Graduate Student Theses, Dissertations, & Professional Papers. 5855. https://scholarworks.umt.edu/etd/5855 This Thesis is brought to you for free and open access by the Graduate School at ScholarWorks at University of Montana. It has been accepted for inclusion in Graduate Student Theses, Dissertations, & Professional Papers by an authorized administrator of ScholarWorks at University of Montana. For more information, please contact [email protected]. COPYRIGHT ACT OF 1976 Th is is an unpublished m a n u s c r ip t in w h ic h c o p y r ig h t su b s i s t s . Any further r e p r in t in g of it s c o n ten ts must be a ppro ved BY THE AUTHOR. MANSFIELD L ib r a r y Un iv e r s it y of Montana D a te : 1 9 8 3 AN ETHNOHISTORY OF THE KOOTENAI INDIANS By Cynthia J. Manning B.A., University of Pittsburgh, 1978 Presented in partial fu lfillm en t of the requirements for the degree of Master of Arts UNIVERSITY OF MONTANA 1983 Approved by: Chair, Board of Examiners Fan, Graduate Sch __________^ ^ c Z 3 ^ ^ 3 Date UMI Number: EP36656 All rights reserved INFORMATION TO ALL USERS The quality of this reproduction is dependent upon the quality of the copy submitted. -
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~ .......... ~ ~ - - -- .. ~~ -- .... ..... .., - .. - ... ...., .... IX. ADYNAMIC HESEHV01H SIMULATION MODEL-DYHESM:5 i\ 311 c. transverse and longitUdinal direction playa secondary role and only the variations) ." I in the vertical enter lhe first order balances of mass, momentum and energy. 1/ I Departures from this Stilte of horizontalisopyc'nalsare possible, but these \ tI l A DYNAMIC RESERVOIR SIl\olULATION MODEL enter only as isolated events or as \I/eak pe.!lurbatiQ.D.S. In both cases the.•net eJJ;cJ,J CI DYRESM: 5 is e~plured wi(h a parame!efizalion of their inp,ut (0 the vertical s(rUelure"iiild , ) I comparison of the model prediction and field data must thus be confined to ~ ~ .....of.............,.calm when the structure is truly one-dimensional. lorg 1mberger and John C.. Pattetsun .. ~ ,. The constraints imposed by ~uch a one-dimer.:Jional model may best be University of Western Australia quantified by defining a series of non-dimensional llUmbers. The value of the Nedlands, Western Australia Wedderburn number :) LV =.i.!!.. h (.J" I I '( 14.2 • L- '7 y(l .. n, (I) , \ ..,' I / 1. INTRODUCTION where g' is an effective reoufed gravity across the thermocline, h the depth of the mixed layer, L the basin scale, and u· the surface shear velocity, is a measure of """·".',j<}·,t-·;~·'",,,"~~,'ti The dynamic reservoir simulation model, DYRESM, is a one-dimensional the activity within the mixed layer. Spigel and Imberger (I980) have shown thah, numerical model for the prediction of temperature and salinity in small to medium for W > 00) the departure fmm one-dimensionality is minimal and for I ':I sized reservoirs and Jakes. -
Columbia River Treaty Review Technical Studies Report
Columbia River Treaty Review Technical Studies Prepared by BC Hydro and Power Authority November 29, 2013 Table of Contents Chapter 1: Introduction ........................................................................................................................................ 5 1.1 Background ......................................................................................................................................... 5 1.2 Approach to Treaty Strategic Decision ............................................................................................... 5 1.3 Process and Scope of Analysis ............................................................................................................ 7 1.3.1 Environmental Advisory Committee and Fish and Wildlife Technical Committee ............. 7 1.3.2 Water Use Plan and Structured Decision Making Process ................................................... 8 Chapter 2: Columbia and Kootenay Hydroelectric System Summary ............................................................. 9 2.1 Operations on the Columbia River - Relationship between Columbia River Treaty, Non Treaty Storage Agreement, and Water Use Plans ............................................................................................... 10 2.2 Operations on the Kootenay River - Relationship between Columbia River Treaty, Duncan Water Use Plan, International Joint Commission Order, and Canal Plant Agreement ...................................... 12 Chapter 3: Selection of Alternatives to Model ................................................................................................. -
Lake Koocanusa, High Level Assessment of a Proposed
BGC ENGINEERING INC. AN APPLIED EARTH SCIENCES COMPANY MINISTRY OF ENERGY, MINES AND PETROLEUM RESOURCES LAKE KOOCANUSA HIGH LEVEL ASSESSMENT OF A PROPOSED DAM FINAL DRAFT PROJECT NO.: 0466001 DATE: November 19, 2020 BGC ENGINEERING INC. AN APPLIED EARTH SCIENCES COMPANY Suite 500 - 980 Howe Street Vancouver, BC Canada V6Z 0C8 Telephone (604) 684-5900 Fax (604) 684-5909 November 19, 2020 Project No.: 0466001 Kathy Eichenberger, Executive Director Ministry of Energy, Mines and Petroleum Resources PO Box 9314, Stn Prov Govt Victoria, BC V8W 9N1 Dear Kathy, Re: Lake Koocanusa, High Level Assessment of a Proposed Dam – FINAL DRAFT BGC is pleased to provide the Ministry of Mines, Energy and Petroleum Resources with the following FINAL DRAFT report. The report details an assessment of a proposed dam on Lake Koocanusa, in southeastern British Columbia. If you have any questions or comments, please contact the undersigned at 604-629-3850. Yours sincerely, BGC ENGINEERING INC. per: Hamish Weatherly, M.Sc., P.Geo. Principal Hydrologist Ministry of Energy, Mines and Petroleum Resources, Lake Koocanusa November 19, 2020 High Level Assessment of a Proposed Dam – FINAL DRAFT Project No.: 0466001 EXECUTIVE SUMMARY The Libby Dam is a 129 m high concrete gravity dam located on the Kootenay River near Libby, Montana. The dam was completed in 1973 and was first filled in 1974, inundating the Kootenay River valley to form the 145 km long Koocanusa Reservoir (Lake Koocanusa). Canadian residents and water users are affected by changes in the Libby Dam operations that affect reservoir water levels, as nearly half (70 km) of the reservoir extends into southeastern British Columbia. -
Mitochondrial DNA Analysis of Burbot Stocks in the Kootenai River Basin of British Columbia, Montana, and Idaho
Transactions of the American Fisheries Society 128:868-874, 1999 © Copyright by the American Fisheries Society 1999 Mitochondrial DNA Analysis of Burbot Stocks in the Kootenai River Basin of British Columbia, Montana, and Idaho VAUGHN L. PARAGAMIAN Idaho Department of Fish and Game, 2750 Kathleen Avenue, Coeur d'Alene, Idaho 83815, USA MADISON S. POWELL* AND JOYCE C. FALER Aquaculture Research Institute, University of Idaho, Moscow, Idaho 83844-2260, USA Abstract.-Differences in mitochondrial haplotype frequency were examined among burbot Lota lota collected from four areas within the Kootenai River Basin of British Columbia, Montana and Idaho. The polymerase chain reaction (PCR) was used to amplify three gene regions of the mi- tochondria) genome: NADH dehydrogenase subunit 1 (ND1), NADH dehydrogenase subunit 2 (ND2), and NADH dehydrogenase subunits 5 and 6 combined (ND5,6). Amplified DNA was screened for restriction fragment length polymorphisms (RFLPs). Simple haplotypes resulting from RFLPs in a single gene region were combined into composite haplotypes. The distribution of composite haplotypes and their frequencies correspond to areas of the Kootenay River basin above and below a presumptive geographic barrier, Kootenai Falls, Montana, and suggest spatially seg- regated populations. A test of geographic heterogeneity among haplotype frequency distributions was highly significant (P < 0.001) when a Monte Carlo simulation was used to approximate a X2 test. Two populations, one above and one below Kootenai Falls emerged when a neighbor-joining method was used to infer a phylogenetic tree based on estimates of nucleotide divergence between all pairs of sample locations. These analyses indicate that burbot below Kootenai Falls form a separate genetic group from burbot above the falls and further suggests that Libby Dam, which created Lake Koocanusa, is not an effective barrier segregating burbot above Kootenai Falls. -
Lake Koocanusa Official Community Plan Bylaw No
LAKE KOOCANUSA OFFICIAL COMMUNITY PLAN BYLAW NO. 2432, 2013 CONSOLIDATION This is a consolidation of the Lake Koocanusa Official Community Plan and adopted bylaw amendments. The amendments have been combined with the original Bylaw for convenience only. This consolidation is not a legal document. October 30, 2020 Lake Koocanusa Official Community Plan Bylaw No. 2432, 2013 This is a consolidation of the Official Community Plan. This consolidated version is for convenience only and has no legal sanction. April 5, 2013 Lake Koocanusa Official Community Plan Endorsement Regional District of East Kootenay “Rob Gay” April 5, 2013 Rob Gay, Board Chair Date “Heath Slee” April 5, 2013 Heath Slee, Electoral Area B Director Date Ktunaxa Nation Council “Ray Warden” March 28, 2013 Ray Warden, Director of Ktunaxa Lands and Resources Agency Date Forest, Lands and Natural Resources Operations “Tony Wideski” March 15, 2013 Tony Wideski, Regional Executive Director – Kootenay Date BYLAW AMENDMENTS Bylaw Amend / Adopted Short Citing Legal / Zone Yr 2539 01/2014 Oct. 3/14 Medical Marihuana Text Amendment /RDEK 2771 02/2017 Aug. 4/17 Koocanusa West / Designation of Part of Wentzell Lot 1, DL 11493, Plan 16032 RR to CR 2921 03/2019 Jun. 7/19 Sweetwater / KV Part of Lot 2, DL Properties Inc. 10348, KD, Plan EPP14443 C to R-SF 2973 04/2019 Jul. 3/20 Sweetwater / KV Part of Lot 2, DL Properties Inc. 10348, KD, Plan EPP14443 C to R-SF REGIONAL DISTRICT OF EAST KOOTENAY BYLAW NO. 2432 A bylaw to adopt an Official Community Plan for the Lake Koocanusa area. WHEREAS the Board of the Regional District of East Kootenay deems it necessary to adopt an official community plan in order to ensure orderly development of the Lake Koocanusa area; NOW THEREFORE, the Board of the Regional District of East Kootenay, in open meeting assembled, enacts as follows: Title 1. -
Benton City Blaine Bremerton Brewster
KUJ-F CHR KCED Hot AC* Benton City 99.1 52000w 1263ft DA 91.3 1000w -72ft +New Northwest Broadcasters, LLC Centralia Community College KMMG Regional Mexican [Repeats: KDYK 1020] Sister to: KALE, KEGX, KIOK, KKSR, KTCR 360-736-9391 96.7 820w 889ft 509-783-0783 fax: 509-735-8627 600 Centralia College Blvd, 98531 +Bustos Media Corporation 830 N Columbia Center Blvd Ste B2 GM Wade Fisher Sister to: KDYK, KDYM, KZML, KZTA, KZTB Kennewick 99336 Centralia/Chehalis Market 509-457-1000 fax: 509-452-0541 GM Kurt Luchs SM Ken Olsen PO Box 2888, Yakima 98907 PD A.J. Brewster CE Mike Powers KNBQ Country 706 Butterfield Rd, Yakima 98901 www.power991fm.com 102.9 70000w 2192ft GM Ricky Tatum SM Ruben Muniz Richland/Kennewick/Pasco Arbitron 7.2 Shr 1700AQH -Clear Channel Communications PD Jesus Rosales CE Dewey Trostell 2nd market Walla Walla 206494-2000 fax: 206-286-2376 www.radlolagrande.com/yakima/ 351 Elliott Ave W Ste 300, Seattle 98119 Richland/KennewickPasco Arbitron 3.0 Shr 700 AQH GM Michele Grosenick SM Alison Hesse Burien PD Jay Kelly CE Ken Broeffle Blaine www.qcountry1029.com KGNW Religious Teaching Centralia/Chehalis Market 820 50000/5000 DA-2 KARI Religious Teaching 2nd market Seattle/Tacoma/Everett +Salem Communications Corp. 550 5000/2500 DA-2 3rd market Olympia Sister to: KKMO, KKOL, KLFE, KNTS -^Multicultural Radio Broadcasting 206443-8200 fax:206-777-1133 Sister to: KVRI 2201 6th Ave Ste 1500, Seattle 98121 Centralia-Chehalis 360-371-5500 fax:360-371-7617 GM Andrew Adams SM Chad Gammage Box 75150, White Rock BC V4B 5 PD Dave Drui CE Monte Passmore KITI Oldies 4840 Lincoln Rd, Blaine 98230 www.kgnw.com 1420 500015000 DA-2 GM/SM/PD Gary Nawman CE Mike Gilbert Seattle/Tacoma/EvereH Arbitron 0.3 Shr 38,100 Cume +Premier Broadcasters, Inc. -
Columbia River Treaty History and 2014/2024 Review
U.S. Army Corps of Engineers • Bonneville Power Administration Columbia River Treaty History and 2014/2024 Review 1 he Columbia River Treaty History of the Treaty T between the United States and The Columbia River, the fourth largest river on the continent as measured by average annual fl ow, Canada has served as a model of generates more power than any other river in North America. While its headwaters originate in British international cooperation since 1964, Columbia, only about 15 percent of the 259,500 square miles of the Columbia River Basin is actually bringing signifi cant fl ood control and located in Canada. Yet the Canadian waters account for about 38 percent of the average annual volume, power generation benefi ts to both and up to 50 percent of the peak fl ood waters, that fl ow by The Dalles Dam on the Columbia River countries. Either Canada or the United between Oregon and Washington. In the 1940s, offi cials from the United States and States can terminate most of the Canada began a long process to seek a joint solution to the fl ooding caused by the unregulated Columbia provisions of the Treaty any time on or River and to the postwar demand for greater energy resources. That effort culminated in the Columbia River after Sept.16, 2024, with a minimum Treaty, an international agreement between Canada and the United States for the cooperative development 10 years’ written advance notice. The of water resources regulation in the upper Columbia River U.S. Army Corps of Engineers and the Basin. -
Main Arm Kootenay Lake FIM 2011
Foreshore Inventory and 3Mapping KKOOOOTTEENNAAYY LLAAKKEE MMAAIINN AARRMM Prepared For: Regional District of Central Kootenay Prepared By: Ecoscape Environmental Consultants Ltd. September, 2010 File No.: 09-513 #102 – 450 Neave Court Kelowna, BC V1V 2M2 Phone: 250.491.7337 Fax: 250.491.7772 Email: [email protected] FORESHORE INVENTORY AND MAPPING Regional District of Central Kootenay Kootenay Lake Main Arm Prepared For: Regional District of Central Kootenay Box 590, 202 Lakeside Dr. Nelson, BC V1L 5R4 Prepared By: ECOSCAPE ENVIRONMENTAL CONSULTANTS LTD. #102 – 450 Neave Court Kelowna, B.C. V1W 3A1 January 2011 File No. 09-513 #102 – 450 Neave Ct. Kelowna BC. V1V 2M2 ph: 250.491.7337 fax: 250.491.7772 [email protected] 09-513 i January 2011 ACKNOWLEDGEMENTS This project was made possible through collaboration between the Regional District of Central Kootenay and Fisheries and Oceans Canada. The following parties carried out or organized fieldwork for this assessment: Fisheries and Oceans Canada: Bruce MacDonald, Sheldon Romaine, Brian Ferguson, Kristin Murphy, and Darryl Hussey The author of this report was: Jason Schleppe, M.Sc., R.P.Bio. (Ecoscape) The report was reviewed by: Kyle Hawes, B.Sc., R.P.Bio. (Ecoscape) Geographical Information Systems (GIS) mapping and analysis was prepared by: Robert Wagner, B.Sc. (Ecoscape) Recommended Citation: Schleppe, J., 2009. Kootenay Lake Foreshore Inventory and Mapping. Ecoscape Environmental Consultants Ltd.. Project File: 09-513. September, 2010. Prepared for: Regional District Central Kootenay. #102 – 450 Neave Ct. Kelowna BC. V1V 2M2 ph: 250.491.7337 fax: 250.491.7772 [email protected] 09-513 ii January 2011 EXECUTIVE SUMMARY This report has been prepared based upon the belief that it is possible to manage our watersheds and their natural surroundings in a sustainable manner. -
KRPI AM Radio Transmitter Site Supplemental Master Project Narrative
KRPI AM Radio Transmitter Site Supplemental Master Project Narrative KRPI Supplemental Project Narrative Table of Contents I. REVISED LOCATION OF ANTENNA ARRAY ................................................................. 1 II. OTHER REVISIONS AND CORRECTIONS TO APPLICATION MATERIALS.............. 2 III. COMMON PROJECT CONCERNS RAISED IN PUBLIC COMMENTS ...................... 4 A. Radio Frequency Interference ............................................................................................. 4 B. Health Effects of Radiofrequency Emissions ..................................................................... 6 C. Visual and Character Impacts ........................................................................................... 11 D. Impacts to Canadians ........................................................................................................ 14 E. Public Benefit.................................................................................................................... 16 F. Avian Impacts ................................................................................................................... 17 G. Impacts to Property Values ............................................................................................... 19 H. Notice ................................................................................................................................ 19 I. Height Limits ................................................................................................................... -
BC Hydro Climate Change Assessment Report 2012
POTENTIAL IMPACTS OF CLIMATE CHANGE ON BC HYDRO’S WATER RESOURCES Georg Jost: Ph.D., Senior Hydrologic Modeller, BC Hydro Frank Weber; M.Sc., P. Geo., Lead, Runoff Forecasting, BC Hydro 1 EXecutiVE Summary Global climate change is upon us. Both natural cycles and anthropogenic greenhouse gas emissions influence climate in British Columbia and the river flows that supply the vast majority of power that BC Hydro generates. BC Hydro’s climate action strategy addresses both the mitigation of climate change through reducing our greenhouse gas emissions, and adaptation to climate change by understanding the risks and magnitude of potential climatic changes to our business today and in the future. As part of its climate change adaptation strategy, BC Hydro has undertaken internal studies and worked with some of the world’s leading scientists in climatology, glaciology, and hydrology to determine how climate change affects water supply and the seasonal timing of reservoir inflows, and what we can expect in the future. While many questions remain unanswered, some trends are evident, which we will explore in this document. 2 IMPACTS OF CLIMATE CHANGE ON BC HYDRO-MANAGED WATER RESOURCES W HAT we haVE seen so far » Over the last century, all regions of British Columbia »F all and winter inflows have shown an increase in became warmer by an average of about 1.2°C. almost all regions, and there is weaker evidence »A nnual precipitation in British Columbia increased by for a modest decline in late-summer flows for those about 20 per cent over the last century (across Canada basins driven primarily by melt of glacial ice and/or the increases ranged from 5 to 35 per cent).