Mid-Columbia Ecosystem Enhancement Project Catalogue
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British Columbia Ministry of Natural Resource Operations Regional
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The Revelstoke Dam: a Case Study of the Selection, Licensing and Implementation of a Large Scale Hydroelectric Project in British Columbia
THE REVELSTOKE DAM: A CASE STUDY OF THE SELECTION, LICENSING AND IMPLEMENTATION OF A LARGE SCALE HYDROELECTRIC PROJECT IN BRITISH COLUMBIA By HEIDI ERIKA MISSLER B.A., The University of British Columbia, 1984 A THESIS SUBMITTED IN PARTIAL FULFILLMENT OF THE REQUIREMENT FOR THE DEGREE OF MASTER OF ARTS i n THE FACULTY OF GRADUATE STUDIES (Department of Geography) We accept this thesis as conforming to the required standard THE UNIVERSITY OF BRITISH COLUMBIA September 1988 QHeidi Erika Missler, 1988 In presenting this thesis in partial fulfilment of the requirements for an advanced degree at the University of British Columbia, I agree that the Library shall make it freely available for reference and study. I further agree that permission for extensive copying of this thesis for scholarly purposes may be granted by the head of my department or by his or her representatives. It is understood that copying or publication of this thesis for financial gain shall not be allowed without my written permission. Department The University of British Columbia 1956 Main Mall Vancouver, Canada V6T 1Y3 Date DE-6G/81) ABSTRACT Procedures for the selection, licensing and implementation of large scale energy projects must evolve with the escalating complexity of such projects and. the changing public value system. Government appeared unresponsive to rapidly changing conditions in the 1960s and 1970s. Consequently, approval of major hydroelectric development projects in British Columbia under the Water Act became increasingly more contentious. This led, in 1980, to the introduction of new procedures—the Energy Project Review Process (EPRP)— under the B.C. Utilities Commission Act. -
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. -
The Columbia Basin Tribes and First Nations Jointly Developed This Paper To
Agenda Item E.2 Attachment 1 (Electronic Only) March 2021 a | EXECUTIVE SUMMARY he Columbia Basin tribes and First Nations jointly developed this paper to Tinform the U.S. and Canadian Entities, federal governments, and other re- gional sovereigns and stakeholders on how anadromous salmon and resident fish can be reintroduced into the upper Columbia River Basin. Reintroduction and res- toration of fish passage could be achieved through a variety of mechanisms, includ- ing the current effort to modernize the Columbia River Treaty (Treaty). Restoring fish passage and reintroducing anadromous fish should be investigated and imple- mented as a key element of integrating ecosystem-based function into the Treaty. Anadromous fish reintroduction is critical to restoring native peoples’ cultural, harvest, spiritual values, and First Foods taken through bilateral river development for power and flood risk management. Reintroduction is also an important facet of ecosystem adaptation to climate change as updated research indicates that only the Canadian portion of the basin may be snowmelt-dominated in the future, making it a critical refugium for fish as the Columbia River warms over time. This transboundary reintroduction proposal focuses on adult and juvenile fish pas- sage at Chief Joseph and Grand Coulee dams in the U.S. and at Hugh Keenleyside, Brilliant, Waneta and Seven Mile dams in Canada. Reintroduction would occur incrementally, beginning with a series of preliminary planning, research, and ex- perimental pilot studies designed to inform subsequent reintroduction and passage strategies. Long-term elements of salmon reintroduction would be adaptable and include permanent passage facilities, complemented by habitat improvement, ar- tificial propagation, monitoring, and evaluation. -
Dams and Hydroelectricity in the Columbia
COLUMBIA RIVER BASIN: DAMS AND HYDROELECTRICITY The power of falling water can be converted to hydroelectricity A Powerful River Major mountain ranges and large volumes of river flows into the Pacific—make the Columbia precipitation are the foundation for the Columbia one of the most powerful rivers in North America. River Basin. The large volumes of annual runoff, The entire Columbia River on both sides of combined with changes in elevation—from the the border is one of the most hydroelectrically river’s headwaters at Canal Flats in BC’s Rocky developed river systems in the world, with more Mountain Trench, to Astoria, Oregon, where the than 470 dams on the main stem and tributaries. Two Countries: One River Changing Water Levels Most dams on the Columbia River system were built between Deciding how to release and store water in the Canadian the 1940s and 1980s. They are part of a coordinated water Columbia River system is a complex process. Decision-makers management system guided by the 1964 Columbia River Treaty must balance obligations under the CRT (flood control and (CRT) between Canada and the United States. The CRT: power generation) with regional and provincial concerns such as ecosystems, recreation and cultural values. 1. coordinates flood control 2. optimizes hydroelectricity generation on both sides of the STORING AND RELEASING WATER border. The ability to store water in reservoirs behind dams means water can be released when it’s needed for fisheries, flood control, hydroelectricity, irrigation, recreation and transportation. Managing the River Releasing water to meet these needs influences water levels throughout the year and explains why water levels The Columbia River system includes creeks, glaciers, lakes, change frequently. -
Revelstoke Generating Station Unit 6 Project Factsheet-December 2018
Revelstoke Generating Station Unit 6 Project Factsheet-December 2018 This project would install a sixth generating unit into an empty four units were installed when the facility was constructed. bay at Revelstoke Generating Station. Revelstoke Unit 6 would The fifth generating unit was recently added and began add approximately 500 megawatts of capacity to our system service in 2010. and provide a significant amount of electricity when our Revelstoke Generating Station produces, on average, about customers need it most – during dark cold winter days 7,817 gigawatt hours or roughly 15 per cent of the electricity when furnaces, appliances and lights are all in use. BC Hydro generates each year. With the five generating units, Revelstoke Generating Station has a combined capacity of REVELSTOKE DAM AND GENERATING STATION 2,480 megawatts. Electricity generated by the plant is Revelstoke Dam and Generating Station are located on the delivered to the grid by two parallel 500 kilovolt transmission Columbia River, 5 kilometers upstream from the City of lines that run from Revelstoke Generating Station to the Revelstoke. The facilities are part of our Columbia system Ashton Creek substation near Kamloops. with Revelstoke Reservoir and Mica Dam located upstream and the Hugh L. Keenleyside Dam and Arrow Lakes Reservoir downstream. The Revelstoke Generating Station, completed in 1984, was designed to hold six generating units but only Project Timing We do not have a timeline for construction. Revelstoke 6 is an important contingency project in case demand grows faster than we expect. 1 Revelstoke Revelstoke Dam Reservoir Hwy 23 BRITISH COLUMBIA Hwy 1 Hwy 1 Hwy 23 Revelstoke Revelstoke Generating Station PROJECT BENEFITS AND OPPORTUNITIES The work to install the sixth generating unit at Revelstoke Generating Station would be very similar to the Revelstoke ○ Jobs . -
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). -
Geography of British Columbia People and Landscapes in Transition 4Th Edition
Geography of British Columbia People and Landscapes in Transition 4th Edition Brett McGillivray Contents Preface / ix Introduction / 3 PART 1: GEOGRAPHICAL FOUNDATIONS 1 British Columbia, a Region of Regions / 11 2 Physical Processes and Human Implications / 29 3 Geophysical Hazards and Their Risks / 51 4 Resource Development and Management / 71 PART 2: THE ECONOMIC GEOGRAPHY OF BRITISH COLUMBIA 5 “Discovering” Indigenous Lands and Shaping a Colonial Landscape / 85 6 Boom and Bust from Confederation to the Early 1900s / 103 7 Resource Dependency and Racism in an Era of Global Chaos / 117 8 Changing Values during the Postwar Boom / 137 9 Resource Uncertainty in the Late Twentieth Century / 153 10 The Twenty-First-Century Liberal Landscape / 177 Conclusion / 201 Acknowledgments / 214 Glossary / 215 Further Readings / 224 Photo Credits / 228 Index / 229 Introduction he geography of British Columbia is in constant place on it the features you consider important. This flux. Between 2014 and 2017 alone, the following cognitive mapping exercise reveals individual land- T events occurred, transforming the landscape and scape experiences (which can be shared with others) and the way people engage with it: demonstrates the importance of location. Using maps to answer “where” questions is the easiest aspect of geo- • Heat waves shattered temperature records, and wild- graphical study. fires devasted parts of the province, causing thousands Answering the question “Why are things where they to flee their homes. are?” is more complicated. “Why” questions are far more • Fracking triggered large quakes in the oil and gas difficult than “where” questions and may ultimately verge patch. on the metaphysical. -
The Columbia River Treaty
The Columbia River Treaty John Shurts General Counsel Northwest Power and Conservation Council Portland, Oregon CREW May 2014 Northwest Power and slide 1 Conservation Council Columbia River Treaty (1961/64) 15 maf of storage in Canada (Mica, Duncan, Keenleyside/Arrow) Downstream flood control and power generation benefits Sharing of downstream benefits – incl. Canadian Entitlement to ½ of downstream Northwest Power and Conservation power benefits Council Columbia River Treaty (cont’d) US authorized to build Libby Dam on Kootenai River – no sharing of benefits – operations coordinated Entities designated to implement Treaty are BC Hydro in BC; Bonneville Admin and Corps Div Commander Northwest in US Power and Conservation Council Canadian Outflows for Power and Flood Control on Planning Basis Arrow+Duncan Treaty Outflows (60-yr Avg.) 140000 120000 Unregulated 100000 04AOP Regulated 80000 60000 40000 20000 Arrow+Duncan Outflow in cfs in Outflow Arrow+Duncan 0 SEP FEB JAN DEC OCT NOV MAR MAY JULY NorthwestJUNE 15-Apr 30-Apr 31-Aug 15-Aug Power and slide 5 Conservation Council Columbia River: average regulated flows average flows at The Dalles -- natural and regulated 500000 400000 Natural Regulated 300000 200000 Cubic Feet per SecondFeet Cubic per 100000 0 Northwest Power and slide 6 Conservation Council Bonneville Dam 1948 Northwest Power and 1996 Conservation Council Kinbasket Lake (Mica Dam) slide 9 AVERAGE ANNUAL RUNOFF AND USABLE RESERVOIR STORAGE MAJOR WESTERN RIVER BASINS 250 240 230 220 210 200 190 180 170 160 Average Annual Runoff 150 Usable Reservoir Storage 140 130 120 110 100 90 MILLIONS OF ACRE FEETACRE MILLIONS OF 80 70 60 50 40 30 20 10 0 Columbia Colorado Missouri Northwest RIVER BASINS Power and Conservation Council Northwest Power and Conservation Council U . -
Downie Slide Very Large Rockslide Stabilization Project
Canadian Geotechnical Society Canadian Geotechnical Achievements 2017 Downie Slide Very Large Rockslide Stabilization Project Geographical location Key References Imrie, AS, Moore, DP and Enegren, EG. Along west side of Revelstoke Reservoir; 65 km north of 1991. Performance and maintenance of Revelstoke, British Columbia. the drainage system at Downie Slide. In Landslides, D Bell (editor), Balkema, Rotterdam. When it began or was completed Kalenchuk, KS, Hutchison, DJ and Downie Slide was identified in 1956; investigations and initial Diederichs, MS. 2009. Downie Slide - drainage works began in 1974; the main drainage system was Interpretations of complex slope installed between 1977 and 1981; monitoring, assessment and mechanics in a massive, slow moving, maintenance continues. translational landslide. Proceedings, Canadian Geotechnical Conference Halifax, NS, pp 367-374. Why a Canadian geotechnical achievement? Photographs Downie Slide is located on the Columbia River within BC Hydro’s Revelstoke Reservoir. The slide is in mica schist/gneiss bedrock with multiple water levels. At nearly 10 km2 in area, 250 m deep and approximately 1.5 billion m3 in volume, this is the world’s largest known landslide stabilization project. Construction of the Revelstoke Dam was contingent on the stabilization of Downie Slide. Key safety issues were the potential for reservoir blockage, a landslide-generated wave, and upstream flooding of Mica Dam, approximately 70 km to the north. After a thorough site investigation by BC Hydro and many consultants, and an extensive public consultation, drainage was selected as the appropriate method for stabilization Aerial view of Downie Slide (outlined in red) looking up the Revelstoke Reservoir and Columbia The drainage included 2,450 m of adits, primarily located in the River valley. -
BC Hydro's Dam Safety Program and Risk Management Processes
BC Hydro’s Dam Safety Program and Risk Management Processes Stephen Rigbey Director, Dam Safety, BC Hydro BC Hydro Overview COMPLEX INFRASTRUCTURE . 80 dams at 41 sites . 31 hydroelectric facilities . ~ 9500MW installed currently . 1100 MW started construction . 3 thermal generating plants . Off-grid diesel stations . 18,500 kilometers of transmission lines Provincial ownership, but international implications 2 Concrete Gravity Dam BC Hydro has 19 Major Concrete Gravity Dams: Aberfeldie Buntzen, Clayton Falls Clowhom Comox Eko Elliott Falls River Ladore Peace Canyon Puntledge Diversion Quinsam Diversion Quinsam Storage Ruskin Seton Seven Mile Spillimacheen Stave Falls & Whatshan Large Embankment Dams WAC Bennett 183 m high; 2 km crest length Volume = 44 million m3 Large by height ; volume Mica 243m high 4 Consequences – Extreme category Columbia River : breach at Mica Dam - flood reaches US border in 22 hrs - peaks at 48m above river bank the next day Flooding all the way to Portland >>> 10,000 people US Nuclear Plant Fraser River : breach at La Joie, Terzhagi still about 10,000 people at risk All BC rail and road transportation routes All Power interconnects 5 Issues Database and Vulnerability Index Deficiencies Actual – known to exist, measureable Potential – require further investigation Normal Conditions Unusual Conditions flood seismic 6 Vulnerability Index- VulnerabilityRisk = Probability Index (Actual of- Dam) Failure = (Concern x Consequence Rating(AD)) x (Frequency of Demand Scaling Factor), or, 3 Vulnerability Index (AD) = 10x -
Lake Revelstoke Reservoir Creel and Visitor Use Survey 2000
Lake Revelstoke Reservoir Creel and Visitor Use Survey 2000 by: K. Bray and M. Campbell Columbia Basin Fish and Wildlife Compensation Program Revelstoke, B.C. January 2001 Executive Summary From May 5 to September 4, 2000, an access point creel survey was conducted on Lake Revelstoke. The principal objectives were to assess the sport fishery on Lake Revelstoke, collect biological data on fish species in the reservoir, and provide a baseline against which future change can be measured. A visitor use survey was conducted concurrently with the creel survey to gauge visitor opinions and perceptions about Lake Revelstoke and to determine how people were using the reservoir. The number of partners involved in this project presents a good example of both the challenges of managing a complex project and the success when many parties work together. Random sampling was stratified by day type (weekend/holidays and weekdays), site location, and time of day. Seven major access point sites were identified and assigned selection probabilities based on previous surveys and current conditions. Aerial survey counts of boats and campers and ground counts of campers were conducted at informal sites to help estimate the proportion of effort missed. 536 angler interviews were conducted with anglers from B.C. comprising 91.6% of those surveyed and Albertans 6.9%. Residents of Revelstoke accounted for half (50.2%) of the interviews and Okanagan anglers for 30.4%. The average trip length was 2.81 ± 0.16 hours with an average of 2.29 anglers and 2.13 rods per boat. Most fishing on Lake Revelstoke was done from a boat (96%) with lures used during almost all recorded fishing trips.