Developing a New Reservoir Operating Plan for Lake Diefenbaker: Questionnaire Summary
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SASKATCHEWAN RV PARKS & CAMPGROUNDS RECOMMENDED BY THE NRVOA TABLE OF CONTENTS Assiniboia Assiniboia Regional Park & Golf Course Battleford Eiling Kramer Campground Bengough Bengough Campground Big Beaver Big Beaver Campground Blaine Lake Martins Lake Regional Park Bulyea Rowans Ravine Candle Lake Sandy Bay Campground Canora Canora Campground Carlyle Moose Mountain Carrot River Carrot River Overnite Park Chelan Fishermans Cove Christopher Lake Anderson Point Campground Churchbridge Churchbridge Campground Christopher Lake Murray Point Campground Cochin The Battlefords Provincial Park Craik Craik & District Regional Park Cut Bank Danielson Campground Canada | NRVOA Recommended RV Parks & Campgrounds: 2019 Return To Table of Contents 2 Cut Knife Tomahawk Campground Davidson Davidson Campground Dinsmore Dinsmore Campground Dorintosh Flotten Lake North Dorintosh Flotten Lake South Dorintosh Greig Lake Dorintosh Kimball Lake Dorintosh Matheson Campground Dorintosh Mistohay Campground Dorintosh Murray Doell Campground Dundurn Blackstrap Campground Eastend Eastend Town Park Eston Eston Riverside Regional Park Elbow Douglas Campground Fishing Lake Fishing Lake Regional Park Glaslyn Little Loon Regional Park Govan Last Mountain Regional Park Grenfell Crooked Lake Campground Grenfell Grenfell Recreational Park Canada | NRVOA Recommended RV Parks & Campgrounds: 2019 Return To Table of Contents 3 Gull Lake Antelope Lake Campground Gull Lake Gull Lake Campground Harris Crystal Beach Regional Park Humboldt Waldsea Lake Regional Park Kamsack Duck Mountain -
Campground Access to of Sustainable Living Craik Hospital
MileByMile.com Personal Road Trip Guide Saskatchewan Highway #11 "Highway 11" Miles ITEM SUMMARY 0.0 Welcome to city of Regina, Winnipeg Street. Access to Royal Saskatchewan Museum. Junction of SK; Hwy #1 West to Moose Jaw, SK. Swift Current, SK. and AB/SK border. East to Moosomin, SK, Virden, SK. - The Royal Saskatchewan Museum was established in Regina as the Provincial Museum in 1906. It was the first museum in Saskatchewan, and the first provincial museum in the three Prairie Provinces. - Attractions in REgina, SK: - Royal Saskatchewan Museum, R C M P Museum, Access to Highway #11 north to Saskatoon. - Attractions in and around Regina, SK. - RCMP Heritage Centre, Regina Plains Museum, - Saskatchewan Sports Hall of Fame & Museum, - RCMP Training Academy, - Regina Floral Conservatory, - MacKenzie Art Gallery, - Sask. Government House Museum and Heritage Property, - Wascana Place, - Saskatchewan War Memorial Project, - Dieppe Memorial. 1.0 Albert St Exit Junction of city of Regina, SK, Ring Road. Highway #11 overlaps Highway #6 at this point. Highway #6 North to communities of Earl Grey Southey adn Serath, South to Corinne, Parry. 1.9 Photo View from highway Highway #6 leaves Highway #11 at this point. 2.4 Photo View from highway Highway is named 'The Louis Riel Trail'. - Highway #11 in - The Louis Riel Trail Saskatchewan, Canada connects the province's three largest cities: highway sign Regina, SK., Saskatoon, SK, and Prince Albert, SK. It is which is approximately 395 kilometers (244 mi.) long. It is also known as the Louis Riel Trail after the 19th century Metis leader. It runs from Highway #6 north of Regina, SK until Highway 2 south of Prince Albert, SK. -
Thermal Alteration and Macroinvertebrate Response Below a Large Northern Great Plains Reservoir
Journal of Great Lakes Research 41 Supplement 2 (2015) 155–163 Contents lists available at ScienceDirect Journal of Great Lakes Research journal homepage: www.elsevier.com/locate/jglr Thermal alteration and macroinvertebrate response below a large Northern Great Plains reservoir Iain D. Phillips a,b,⁎, Michael S. Pollock a, Michelle F. Bowman c,D.GlenMcMaster d, Douglas P. Chivers b a Water Quality and Habitat Assessment Services, Water Security Agency, 101-108 Research Drive, Saskatoon, Saskatchewan, S7N 3R3, Canada b Department of Biology, University of Saskatchewan, 112 Science Place, Saskatoon, Saskatchewan S7N 5E2, Canada c Forensecology, 70 Swift Crescent, Guelph, Ontario N1E 7J1, Canada d Water Quality and Habitat Assessment Services, Water Security Agency, 420-2365 Albert Street, Regina, Saskatchewan, S4P 4K1, Canada article info abstract Article history: Large hydroelectric dams directly alter the abiotic condition of rivers by releasing water with large differences in Received 26 June 2014 temperature relative to natural conditions. These alterations in the thermal regime along with alterations in flow Accepted 3 July 2015 often result in altered ecosystems downstream. For sustainable management of this aquatic resource, there is a Available online 23 July 2015 need to balance services a reservoir provides with ecosystem protection. Here we conduct a high-resolution study on the thermal regime and associated aquatic macroinvertebrate community downstream of a hydroelec- Communicated by Jeff Hudson tric dam on a large-order Northern Great Plains River and analyze these findings with a non-central hypothesis fi Keywords: test model, Test Site Analysis. Speci cally, we monitor the temperature regime of this tailwater environment, and Lake Diefenbaker compare the annual change in temperature downstream to reference sites unaffected by the dam. -
Reactive Silicon Dynamics in a Large Prairie Reservoir (Lake Diefenbaker, Saskatchewan)
Journal of Great Lakes Research 41 Supplement 2 (2015) 100–109 Contents lists available at ScienceDirect Journal of Great Lakes Research journal homepage: www.elsevier.com/locate/jglr Reactive silicon dynamics in a large prairie reservoir (Lake Diefenbaker, Saskatchewan) Taylor Maavara a,⁎, Jennifer L.A. Hood a, Rebecca L. North b, Lorne E. Doig c, Christopher T. Parsons a, Jessica Johansson b, Karsten Liber c,JeffJ.Hudsonb, Brett T. Lucas c, David M. Vandergucht b, Philippe Van Cappellen a a Ecohydrology Research Group, Water Institute and Department of Earth and Environmental Sciences, University of Waterloo, Waterloo, ON N2L 3G1, Canada b Department of Biology, University of Saskatchewan, Saskatoon, SK S7N 5E2, Canada c Toxicology Centre, University of Saskatchewan, Saskatoon, SK S7N 5B3, Canada article info abstract Article history: There is an up-coming global surge in dam construction. River damming impacts nutrient cycling in watersheds Received 4 July 2014 through transformation and retention in the reservoirs. The bioavailability of silicon (Si) relative to nitrogen Accepted 9 March 2015 (N) and phosphorus (P) concentrations, in combination with light environment, controls diatom growth and Available online 4 June 2015 therefore influences phytoplankton community compositions in most freshwater aquatic ecosystems. In this study, we quantified reactive Si cycling and annual Si retention in Lake Diefenbaker, a 394 km2 prairie reservoir Communicated by John-Mark Davies in Saskatchewan, Canada. Retention estimates were derived from 7 sediment cores combined with high- Index words: resolution spatiotemporal sampling of water column dissolved Si (DSi). Current annual DSi retention in the res- 8 −1 Reactive silicon ervoir is approximately 28% of the influx, or 2.5 × 10 mol yr . -
Upper Qu'appelle Water Supply Project
Upper Qu’Appelle Water Supply Project Water Scarcity, Water Supply, Water Security A Long Term Investment in Saskatchewan’s Future An Economic Impact & Sensitivity Analysis Water security has always been important for Saskatchewan. Prior to settlement, First Nations moved with the droughts and wintered in the river valleys. Droughts of the 1930s created a human and environmental tragedy that lasted for generations. It set November 2012 South Central Enterprise Region the foundation, however, for visionary water planning with the formation of a secure water supply in Lake Diefenbaker and a distributional opportunity for all regions of the province. The water investments in the 1940s, 1950s and 1960s are still benefiting Upper Qu’Appelle Regional Water Conveyance generations of Saskatchewan residents. Over 100,000 acres has been irrigated around the Lake, clean hydro electric power is generated from turbines at Coteau Creek, tourism has grown around the water source and wildlife have thrived in the healthy man made aquatic environment. In 1980, Regina and Moose Jaw requested the federal and provincial governments complete a comprehensive water supply study that concluded municipal requirements for raw water could be met from Buffalo Pound Lake via the existing Qu’Appelle River channel to 2030, with the addition of granular activated carbon treatment. At the time, water quality rather than water supply issues were paramount and central to the evaluation. At the time a multi-purpose canal via several routes through the Qu’Appelle and Thunder Creek as far as the Souris was identified. In the thirty years since there have been major changes in the levels of development and scope of opportunities available to the area. -
Gardiner Dam's Historic Movement and Ongoing Stability Evaluation
10/18/2018 10/18/2018 Gardiner Dam’s Historic Movement and Ongoing Stability Evaluation Jody Scammell, M.Sc., P. Eng. Director, Dam Safety and Major Structures 1 10/18/2018 2 10/18/2018 Outline • South Saskatchewan River Project Introduction • Lake Diefenbaker Reservoir • Gardiner Dam – Foundation Conditions – Major Components – Movements – Previous Stability Evaluations • Grant Devine Dam Stability Evaluation • Expected Results – Not expected results 3 10/18/2018 SSRP Introduction Gardiner Dam Qu’Appelle River Dam 4 10/18/2018 SSRP Introduction • 1894 first consideration for large irrigation • 1968 completed • Total cost $120 million (1968 value) • Replacement value $2.41 Billion • Owned and operated by Water Security Agency • Operation, maintenance and monitoring complete by 8 onsite staff 5 10/18/2018 Lake Diefenbaker Reservoir 6 10/18/2018 Reservoir Drainage Basin • Three Regions • Effective Distribution – Eastern Rockies 50% Area / 80% Flow – Foothills – Prairies 50% Area / 20% Flow • 60% Snowmelt • 38% Rainfall runoff • 2% Glacier melt 7 10/18/2018 Reservoir Operation • Runoff patterns – Low winter flow – Spring peak, April – Summer peak, May/June – Recession, Aug/Sept 8 10/18/2018 Reservoir • Lake Diefenbaker • 225 km long (near Eston, SK) • 760 km shoreline • Volume 9.25x109 m3 • Usable Storage 3.95x109 m3 • Up to 58 m deep 9 10/18/2018 2013 Release • Largest flow released • 1600 m3/s spillway • 2000 m3/s total 6000 558 Lake Diefenbaker April 1, 2013 to March 31, 2014 5000 556 4000 554 3000 552 Inflow Flow (m3/s) Flow Outflow -
Lake Diefenbaker: the Prairie Jewel
Journal of Great Lakes Research 41 Supplement 2 (2015) 1–7 Contents lists available at ScienceDirect Journal of Great Lakes Research journal homepage: www.elsevier.com/locate/jglr Lake Diefenbaker: The prairie jewel Introduction with intakes that are 34 m below FSL. The proportion of inflowing water that flows out of Gardiner Dam varies from ~70% in low flow years (e.g., 2001 average flow was 84 m3 s−1)toover97%inhigh fl 3 −1 Fighting drought with a dam: Lake Diefenbaker, the reservoir of ow years (e.g., 2005; 374 m s ; Hudson and Vandergucht, 2015) fl life-giving water.CBC's Norman DePoe. with a median proportional out ow of ~94%. Additional water losses in- clude net evaporation, which can represent over 10% in dry years, irriga- On the broad expanse of flat land of the northern Great Plains of tion, and direct use from the reservoir. From the Qu'Appelle Dam, Lake Canada lies a large, narrow, river-valley reservoir, Lake Diefenbaker. Diefenbaker water is transferred out of the natural catchment and re- The reservoir was developed for multiple benefits including the irriga- leased down the Qu'Appelle River to supply southern regions of the tion of ~2000 km2 of land in Central Saskatchewan, the generation of province. With a mean depth of 22 m, the water residence time, though hydroelectricity, a source of drinking water, flood control, water for in- variable, is typically just over a year (Donald et al., 2015; Hudson and dustry and livestock, and recreation. This semi-arid region has an aver- Vandergucht, 2015). -
Water Quality in the South SK River Basin
Water Quality in the South SK River Basin I AN INTRODUCTION TO THE SOUTH SASKATCHEWAN RIVER BASIN I.1 The Saskatchewan River Basin The South Saskatchewan River joins the North Saskatchewan River to form one of the largest river systems in western Canada, the Saskatchewan River System, which flows from the headwater regions along the Rocky Mountains of south-west Alberta and across the prairie provinces of Canada (Alberta, Saskatchewan, and Manitoba). The Prairie physiographic region is characterized by rich soils, thick glacial drift and extensive aquifer systems, and a consistent topography of broad rolling hills and low gradients which create isolated surface wetlands. In contrast, the headwater region of the Saskatchewan River (the Western Cordillera physiographic region) is dominated by thin mineral soils and steep topography, with highly connected surface drainage systems and intermittent groundwater contributions to surface water systems. As a result, the Saskatchewan River transforms gradually in its course across the provinces: from its oxygen-rich, fast flowing and highly turbid tributaries in Alberta to a meandering, nutrient-rich and biologically diverse prairie river in Saskatchewan. There are approximately 3 million people who live and work in the Saskatchewan River Basin and countless industries which operate in the basin as well, including pulp and paper mills, forestry, oil and gas extraction, mining (coal, potash, gravel, etc.), and agriculture. As the fourth longest river system in North America, the South Saskatchewan River Basin covers an incredibly large area, draining a surface of approximately 405 860 km² (Partners FOR the Saskatchewan River Basin, 2009). Most of the water that flows in the Saskatchewan River originates in the Rocky Mountains of the Western Cordillera, although some recharge occurs in the prairie regions of Alberta and Saskatchewan through year-round groundwater contributions, spring snow melt in March or April, and summer rainfall in May and early July (J.W. -
State of Lake Diefenbaker Report
State of Lake Diefenbaker Prepared for: Consultation Meeting on May 30, 2012. Document was edited and revised on October 19, 2012 Executive Summary The purpose of this report is to provide the stakeholders with some context of the South Saskatchewan River project, the management issues associated with the operation of the Gardiner and Qu’Appelle River Dams, and the health of Lake Diefenbaker and the Lake Diefenbaker Watershed. This report summarizes the management activities associated with the operation of the South Saskatchewan River Project and the potential outcomes related to these management activities. Information within this report provides a basis for evaluating the management objectives and setting priorities for the operation of the Project. Table 1 outlines the various reservoir management activities and the resulting consequences of these activities. The South Saskatchewan River Project, of which Lake Diefenbaker and the Gardiner and Qu’Appelle River Dams are the primary components, is a critical water resource for the province of Saskatchewan. The South Saskatchewan River Project is currently owned and managed by the Water Security Agency of Saskatchewan for multiple services, including irrigation, municipal and industrial water supply, hydroelectric power generation, recreation, aquatic and wildlife habitat, and downstream flood control. The services provided by the Project are fundamental to the province’s economic, social and environmental well being. Lake Diefenbaker construction started after an agreement between the province of Saskatchewan and the Government of Canada, which was signed in 1958. The initial purpose of the project was to form a reservoir that could provide source water to irrigate approximately 200,000 hectares of farmland in central Saskatchewan and the Qu’Appelle Valley. -
Our Greatest Resource: a Look at Irrigation in Saskatchewan in 2015
OUR GREATEST RESOURCE A look at irrigation in Saskatchewan by Cassi Smith A fully-diversified irrigation economy will create returns to farmers and society and make significant contributions to provincial output (GDP) as well as increase household and rural farm incomes and employment. It will create a foundation for even higher value-added SIPA food production, increase tourism development and Saskatchewan Irrigation Projects stabilize rural populations. Association Inc. Photo: Ron Garnett / AirScapes.ca September 2015 Saskatchewan Business Magazine 41 “Water is the lifeblood of agriculture, and irrigation and water development projects have the potential to provide security for ag processing as well as production. In the right circumstances, they can be a fundamental enabler for one of Saskatchewan’s most significant economic sectors.” Ron Kehrig, Sector Manager for Life Sciences and Biomass with Saskatchewan’s Ministry of the Economy Saskatchewan has only ever scratched the surface environmental and agricultural benefits of completing the of its irrigation potential. With the construction of province’s proposed water infrastructure projects are vast and Gardiner Dam and the Qu’Appelle Dam and the subsequent Saskatchewan has everything we need to turn the sleeping creation of Lake Diefenbaker, the province’s water-holding potential of irrigation into a province-wide success story. capacity is huge and has been for many years. Investing in our province’s future is a lot like farming. One In 1957, the federal government, through Prairie Farm year the weather cooperates, yields are high and bills are paid, Rehabilitation Administration (PFRA), began construction of while the next, a series of setbacks can put everyone in a dan- the Gardiner and Qu’Appelle River dams to impound water in gerous position. -
Saskatchewan 2011 | 2012 PROVINCIAL PARKS GUIDE
parks Saskatchewan 2011 | 2012 PROVINCIAL PARKS GUIDE Saskatchewan Ministry of Tourism, Parks, Culture and Sport saskparks.net 1 Lac La Ronge Provincial Park (Nistowiak Falls) Lac La Ronge Provincial Now, our 34 provincial parks, This is an exciting time for our eight historic sites, 130 recreation provincial parks. We are working sites and 24 protected areas have to ensure future generations will a total land area of 1.4 million be able to continue to explore, hectares and contain some of relax and enjoy the many in Saskatchewan’s the province’s most unique, outdoor recreation opportunities provincial parks! biologically-diverse and beautiful and natural and cultural areas natural and cultural landscapes. in our provincial parks. This year, the provincial This summer, be sure to take in Enjoy your visit to Saskatchewan’s park system turns 80 – a birthday celebrations at a park provincial parks! milestone that will be of your choice. You can find greeted by celebrations out what is being planned by right across the system. contacting the park or by visiting our website at www.saskparks.net. Saskatchewan’s first six provincial parks We are also continuing to improve Bill Hutchinson were established in our provincial parks by adding Minister of Tourism, Parks, 1931 – a year after the electrical service to campsites, Culture and Sport federal government transferred renewing or replacing service control of natural resources centres and replacing boat docks, to the province. One of those picnic tables and barbecues. original parks, Little Manitou, is currently a regional park. Cover image: Lake Diefenbaker (near Elbow Harbour Recreation Site) Contributing photography: Tourism Saskatchewan, Paul Austring Photography, Davin Andrie, Greg Huszar Photography, Saskatchewan Archives Board 4 Park Locator Map 6 Start Packing 8 Your Spot Awaits 10 Don't Forget 12 Celebrating our 80th Anniversary 14 Through The Years 16 Endless Possibilities 18 Southwest Cypress Hills, St. -
Hydroelectric Operations
SASKATCHEWAN RIVER BASIN Hydroelectric Operations Flick on a light, crank up the air conditioner, plug in the snow blower, and somewhere water turns a turbine to product the hydroelectric power that you need. Generating electricity is an important use of water in the Saskatchewan POWER FACTS... River Basin. • Electricity is measured More than three million people live, work and play in the Saskatchewan River in kilowatt hours Basin and many depend on hydroelectricity. In Manitoba, almost all of the (kwh). It takes one province’s electricity comes from hydroelectric dams. Approximately six percent kwh to light ten 100- of North America’s water fl ows through Manitoba and the rivers in Manitoba watt light bulbs for one that supply power have more than twice the hydroelectric potential of Niagara hour. Falls. To date, only 50% of this potential has been harnessed for electricity. • In a thermal station, Manitoba has 15 hydroelectric generating stations or dams. Most of Manitoba’s production of one kwh hydroelectric power is generation by fi ve dams on the Nelson River, which of electricity requiries receives 30 percent of its fl ow from the Saskatchewan River Basin. 140 litres of water, most of which returns Hydroelectric power produces about 20 percent of Saskatchewan’s electricity and to the river. Saskatchewan has seven hydroelectric generating stations or dams. Th e majority • In a hydroelectric of Alberta’s power is generated by fossil fuels, although there are 22 hydroelectric generating station, generating stations or dams in Alberta. Th e majority of the stations are small 8-12,000 litres of water power producers.