Bow River Recreational Access Ghost Dam to Bearspaw Reservoirs. Introduction
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RURAL ECONOMY Ciecnmiiuationofsiishiaig Activity Uthern All
RURAL ECONOMY ciEcnmiIuationofsIishiaig Activity uthern All W Adamowicz, P. BoxaIl, D. Watson and T PLtcrs I I Project Report 92-01 PROJECT REPORT Departmnt of Rural [conom F It R \ ,r u1tur o A Socio-Economic Evaluation of Sportsfishing Activity in Southern Alberta W. Adamowicz, P. Boxall, D. Watson and T. Peters Project Report 92-01 The authors are Associate Professor, Department of Rural Economy, University of Alberta, Edmonton; Forest Economist, Forestry Canada, Edmonton; Research Associate, Department of Rural Economy, University of Alberta, Edmonton and Research Associate, Department of Rural Economy, University of Alberta, Edmonton. A Socio-Economic Evaluation of Sportsfishing Activity in Southern Alberta Interim Project Report INTROI)UCTION Recreational fishing is one of the most important recreational activities in Alberta. The report on Sports Fishing in Alberta, 1985, states that over 340,000 angling licences were purchased in the province and the total population of anglers exceeded 430,000. Approximately 5.4 million angler days were spent in Alberta and over $130 million was spent on fishing related activities. Clearly, sportsfishing is an important recreational activity and the fishery resource is the source of significant social benefits. A National Angler Survey is conducted every five years. However, the results of this survey are broad and aggregate in nature insofar that they do not address issues about specific sites. It is the purpose of this study to examine in detail the characteristics of anglers, and angling site choices, in the Southern region of Alberta. Fish and Wildlife agencies have collected considerable amounts of bio-physical information on fish habitat, water quality, biology and ecology. -
CANADIAN ROCKIES North America | Calgary, Banff, Lake Louise
CANADIAN ROCKIES North America | Calgary, Banff, Lake Louise Canadian Rockies NORTH AMERICA | Calgary, Banff, Lake Louise Season: 2021 Standard 7 DAYS 14 MEALS 17 SITES Roam the Rockies on this Canadian adventure where you’ll explore glacial cliffs, gleaming lakes and churning rapids as you journey deep into this breathtaking area, teeming with nature’s rugged beauty and majesty. CANADIAN ROCKIES North America | Calgary, Banff, Lake Louise Trip Overview 7 DAYS / 6 NIGHTS ACCOMMODATIONS 3 LOCATIONS Fairmont Palliser Calgary, Banff, Lake Louise Fairmont Banff Springs Fairmont Chateau Lake Louise AGES FLIGHT INFORMATION 14 MEALS Minimum Age: 4 Arrive: Calgary Airport (YYC) 6 Breakfasts, 4 Lunch, 4 Dinners Suggested Age: 8+ Return: Calgary Airport (YYC) Adult Exclusive: Ages 18+ CANADIAN ROCKIES North America | Calgary, Banff, Lake Louise DAY 1 CALGARY, ALBERTA Activities Highlights: Dinner Included Arrive in Calgary, Welcome Dinner at the Hotel Fairmont Palliser Arrive in Calgary Land at Calgary Airport (YYC) and be greeted by Adventures by Disney representatives who will help you with your luggage and direct you to your transportation to the hotel. Morning And/Or Afternoon On Your Own in Calgary Spend the morning and/or afternoon—depending on your arrival time—getting to know this cosmopolitan city that still holds on to its ropin’ and ridin’ cowboy roots. Your Adventure Guides will be happy to give recommendations for things to do and see in this gorgeous city in the province of Alberta. Check-In to Hotel Allow your Adventure Guides to check you in while you take time to explore this premiere hotel located in downtown Calgary. -
Water Storage Opportunities in the South Saskatchewan River Basin in Alberta
Water Storage Opportunities in the South Saskatchewan River Basin in Alberta Submitted to: Submitted by: SSRB Water Storage Opportunities AMEC Environment & Infrastructure, Steering Committee a Division of AMEC Americas Limited Lethbridge, Alberta Lethbridge, Alberta 2014 amec.com WATER STORAGE OPPORTUNITIES IN THE SOUTH SASKATCHEWAN RIVER BASIN IN ALBERTA Submitted to: SSRB Water Storage Opportunities Steering Committee Lethbridge, Alberta Submitted by: AMEC Environment & Infrastructure Lethbridge, Alberta July 2014 CW2154 SSRB Water Storage Opportunities Steering Committee Water Storage Opportunities in the South Saskatchewan River Basin Lethbridge, Alberta July 2014 Executive Summary Water supply in the South Saskatchewan River Basin (SSRB) in Alberta is naturally subject to highly variable flows. Capture and controlled release of surface water runoff is critical in the management of the available water supply. In addition to supply constraints, expanding population, accelerating economic growth and climate change impacts add additional challenges to managing our limited water supply. The South Saskatchewan River Basin in Alberta Water Supply Study (AMEC, 2009) identified re-management of existing reservoirs and the development of additional water storage sites as potential solutions to reduce the risk of water shortages for junior license holders and the aquatic environment. Modelling done as part of that study indicated that surplus water may be available and storage development may reduce deficits. This study is a follow up on the major conclusions of the South Saskatchewan River Basin in Alberta Water Supply Study (AMEC, 2009). It addresses the provincial Water for Life goal of “reliable, quality water supplies for a sustainable economy” while respecting interprovincial and international apportionment agreements and other legislative requirements. -
Bow River Basin State of the Watershed Summary 2010 Bow River Basin Council Calgary Water Centre Mail Code #333 P.O
30% SW-COC-002397 Bow River Basin State of the Watershed Summary 2010 Bow River Basin Council Calgary Water Centre Mail Code #333 P.O. Box 2100 Station M Calgary, AB Canada T2P 2M5 Street Address: 625 - 25th Ave S.E. Bow River Basin Council Mark Bennett, B.Sc., MPA Executive Director tel: 403.268.4596 fax: 403.254.6931 email: [email protected] Mike Murray, B.Sc. Program Manager tel: 403.268.4597 fax: 403.268.6931 email: [email protected] www.brbc.ab.ca Table of Contents INTRODUCTION 2 Overview 4 Basin History 6 What is a Watershed? 7 Flora and Fauna 10 State of the Watershed OUR SUB-BASINS 12 Upper Bow River 14 Kananaskis River 16 Ghost River 18 Seebe to Bearspaw 20 Jumpingpound Creek 22 Bearspaw to WID 24 Elbow River 26 Nose Creek 28 WID to Highwood 30 Fish Creek 32 Highwood to Carseland 34 Highwood River 36 Sheep River 38 Carseland to Bassano 40 Bassano to Oldman River CONCLUSION 42 Summary 44 Acknowledgements 1 Overview WELCOME! This State of the Watershed: Summary Booklet OVERVIEW OF THE BOW RIVER BASIN LET’S TAKE A CLOSER LOOK... THE WATER TOWERS was created by the Bow River Basin Council as a companion to The mountainous headwaters of the Bow our new Web-based State of the Watershed (WSOW) tool. This Comprising about 25,000 square kilometres, the Bow River basin The Bow River is approximately 645 kilometres in length. It begins at Bow Lake, at an River basin are often described as the booklet and the WSOW tool is intended to help water managers covers more than 4% of Alberta, and about 23% of the South elevation of 1,920 metres above sea level, then drops 1,180 metres before joining with the water towers of the watershed. -
Exploring the Vastness of Banff National Park
Exploring the Vastness of Banff National Park By Claire Walter o borrow on old Ttravelogue cliché, Alberta’s Banff National Park is study in contrast. Its 2,586 square miles comprise both wilderness and civilization. There are high mountains, deep valleys, endless forests and abundant wildlife. Even though much of it feels and looks remote, it is just 70 miles from Calgary – and the Trans-Canada Highway runs right through it. It contains one large town (Banff), one smaller town (Lake Louise Village), two palatial hotels (the Fairmont Banff Springs and Fairmont Chateau Lake Louise) and three significant downhill ski areas (Ski Lake Louise, Sunshine and Norquay). It is a park among parks, with Kootenay National Park just to the south, Yoho National Park to the west (and in another province) and Jasper National Park to the north. It is Canada’s oldest national park and also the one with phenomenal snowshoe opportunities. It’s a great destination for a snowshoe getaway or a multi-activity winter vacation with snowshoeing among the options. There’s skiing (Alpine and Nordic), wildlife viewing, spa- hopping and enjoying the shops, galleries, restaurants and nightspots in Banff or quieter Lake 1 Go FartherTM Model: ARTICA™ BACKCOUNTRY q Two-Piece Articulating Frame q Virtual Pivot Traction Cam q Quick-Cinch™ One-Pull Binding q 80% Recyclable Materials, No PVC’s eastonmountainproducts.com ©2010 easton mountain products Louise Village. As a bonus, winter is low season in Banff, so lodging is a bargain and the shops offer incredible values. Snowshoeing Options The most straightforward snowshoeing is practically from the doorstep of the Chateau Lake Louise. -
South Saskatchewan River Basin Adaptation to Climate Variability Project
South Saskatchewan River Basin Adaptation to Climate Variability Project Climate Variability and Change in the Bow River Basin Final Report June 2013 This study was commissioned for discussion purposes only and does not necessarily reflect the official position of the Climate Change Emissions Management Corporation, which is funding the South Saskatchewan River Basin Adaptation to Climate Variability Project. The report is published jointly by Alberta Innovates – Energy and Environment Solutions and WaterSMART Solutions Ltd. This report is available and may be freely downloaded from the Alberta WaterPortal website at www.albertawater.com. Disclaimer Information in this report is provided solely for the user’s information and, while thought to be accurate, is provided strictly “as is” and without warranty of any kind. The Crown, its agents, employees or contractors will not be liable to you for any damages, direct or indirect, or lost profits arising out of your use of information provided in this report. Alberta Innovates – Energy and Environment Solutions (AI-EES) and Her Majesty the Queen in right of Alberta make no warranty, express or implied, nor assume any legal liability or responsibility for the accuracy, completeness, or usefulness of any information contained in this publication, nor that use thereof infringe on privately owned rights. The views and opinions of the author expressed herein do not necessarily reflect those of AI-EES or Her Majesty the Queen in right of Alberta. The directors, officers, employees, agents and consultants of AI-EES and the Government of Alberta are exempted, excluded and absolved from all liability for damage or injury, howsoever caused, to any person in connection with or arising out of the use by that person for any purpose of this publication or its contents. -
The 2013 Flood Event in the Bow and Oldman River Basins; Causes, Assessment, and Damages
The 2013 flood event in the Bow and Oldman River basins; causes, assessment, and damages John Pomeroy1, Ronald E. Stewart2, and Paul H. Whitfield1,3,4 1Centre for Hydrology, University of Saskatchewan, Saskatoon, SK, S7N 5C8. Phone: (306) 966-1426, Email: [email protected] 2Department of Environment and Geography, University of Manitoba, Winnipeg, MB, R3T 2N2 3Department of Earth Science, Simon Fraser University, Burnaby, BC, V5A 1S6 4Environment Canada, Vancouver, BC, V6C 3S5 Event summary In late June 2013, heavy rainfall and rapidly melting alpine snow triggered flooding throughout much of the southern half of Alberta. Heavy rainfall commenced on June 19th and continued for three days. When the event was over, more than 200 mm and as much as 350 mm of precipitation fell over the Front Ranges of the Canadian Rocky Mountains. Tributaries to the Bow River including the Ghost, Kananaskis, Elbow, Sheep, Highwood, and many of their tributaries all reached flood levels. The storm had a large spatial extent causing flooding to the north and south in the Red Deer and Oldman Basins, and also to the west in the Elk River in British Columbia. Convergence of the nearly synchronous floodwaters downstream in the Saskatchewan River system caused record high releases from Lake Diefenbaker through Gardiner Dam. Dam releases in Alberta and Saskatchewan attenuated the downstream flood peak such that only moderate flooding occurred in Saskatchewan and Manitoba. More than a dozen municipalities declared local states of emergency; numerous communities were placed under evacuation order in Alberta and Saskatchewan. More than 100,000 people needed to evacuate their homes, and five people died. -
Hydrology Study, Bow and Elbow River Updated Hydraulic Model Project, Rev
March 2010 HYDROLOGY STUDY, BOW AND ELBOW RIVER UPDATED HYDRAULIC MODEL PROJECT, REV. A Submitted to: Alberta Environment REPORT Report Number: 09-1326-1040 HYDROLOGY STUDY, BOW AND ELBOW RIVER UPDATED HYDRAULIC MODEL PROJECT Executive Summary Golder Associates Ltd. (Golder) was commissioned by Alberta Environment (AENV) to conduct a hydrology study for the “Bow and Elbow River Updated Hydraulic Model” project. The City of Calgary (the City), in partnership with Alberta Environment (AENV), plans to create a HEC-RAS (Hydraulic Engineering Center River Analysis System) hydraulic model of the Bow and Elbow Rivers through the City. The model implementation is primarily for supporting emergency response planning and operations through flood inundation mapping. It will provide additional perspective on current flood hazard area management and will provide a basis for increased understanding of fish habitat, river morphology and erosion, water quality and storm water runoff impacts. The scope of work for the hydrology study included: 1) Generation of naturalized daily flow series at the major storage facilities on the Bow River above Bearspaw Dam and on the Elbow River at Glenmore Reservoir; 2) Estimation of naturalized and regulated 1:2 to 1:1,000 year flood flows based on flood frequency analysis of naturalized and/or recorded peak flow series at relevant locations along the Bow River and its tributaries (including the Elbow River); 3) Development of synthetic inflow flood hydrographs for tributaries to the Bow River with hydropower developments and at the Water Survey of Canada (WSC) Bow River at Banff station; 4) Routing of the synthetic flood hydrographs through all major storage reservoirs along the Bow River above Bearspaw Dam and through the Glenmore Reservoir; 5) Commentary on the effects of climate change and the impact of stormwater runoff on flood estimates as well as on the seasonality of flood peaks; and 6) Comparison of the new flood flow estimates with those of AENV’s 1983 Calgary Floodplain Study (the 1983 study). -
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. -
Aquatic Ecosystems: the Elbow River an Educational Field Study for Biology-20 Students Acknowledgements
Aquatic Ecosystems: The Elbow River An Educational Field Study for Biology-20 Students Acknowledgements The development of this field study program was made possible through a partnership between Alberta Tourism, Parks and Recreation, the Friends of Kananaskis Country, and the Elbow River Watershed Partnership. The program was written and compiled by the Environmental Education Program in Kananaskis Country and the field study equipment and programming staff were made possible through the Friends of Kananaskis Country with financial support from the Elbow River Watershed Partnership, Alberta Ecotrust, the City of Calgary, and Lafarge Canada. The Elbow River Watershed Partnership also provided technical support and expertise. These materials are copyrighted and are the property of Alberta Tourism, Parks and Recreation. They have been developed for educational purposes. Reproduction of student handouts by school and other non-profit organizations is encouraged with acknowledgement of their sources when they are used in conjunction with this field study program. Otherwise, written permission is required for the reproduction or use of anything contained in this document. For further information contact the Environmental Education Program in Kananaskis Country. Committee responsible for implementing the program include: Monique Dietrich Elbow River Watershed Partnership, Calgary, Alberta Jennifer Janzen Springbank High School, Springbank, Alberta Mike Tyler Woodman Junior High School, Calgary, Alberta Janice Poleschuk St. Jean Brebeuf Junior -
Calgary's Water Supply
3/20/2021 Calgary's water supply Caution | State of local emergency renewed until May 24, 2021 Get Coronavirus (COVID-19) updates and information on closures, cancellations and service changes. Coronavirus (COVID-19) updates View our closures and service changes Calgary's water supply Where does our water come from? Print guide for Calgary's watershed Our water comes from the Rocky Mountains west of the city from a basin-like landform called a watershed. See our Homeowner Water Guide for Calgary's watershed. It is water collected from rain fall and snow melt which channels through creeks and streams making its way into larger rivers. Translations Are you a student? Find more water facts and information about Calgary's water Arabic systems at Water Education Resources. Chinese - Simplied Chinese - Traditional Hindi How the City of Calgary protects our water supply Punjabi Urdu Water is a limited resource and our water supply is changing due to climate change and a growing population. Find out how we're protecting our source water and what actions we're taking to ensure we have reliable water supply for generations to come. The Elbow River Watershed The Elbow River is the source for approximately 40 per cent of Calgary's water supply. The Elbow Valley watershed covers an area of 1,227 square kilometres and drains into the Glenmore Reservoir. It is 120 kilometres long and passes through four sub-climates before it enters the Glenmore Reservoir. The Elbow River is the source of water for the Glenmore Water Treatment Plant. We draw water from the Glenmore Reservoir in order to provide treated water to citizens, but we also play an important role in ood control for this region. -
Bow River Live Simulation
Bow River Live Simulation Summary Report December 2011 This report was prepared by WaterSMART Solutions Ltd. (WaterSMART) and Alberta Innovates – Energy and Environment Solutions. It may be freely downloaded from the Alberta WaterPortal at: http://www.albertawater.com. Alberta Environment and Water has provided to Alberta WaterSMART a licence to use the data required to prepare this report for the purpose of conducting research and public dissemination on a non-commercial basis. Alberta Environment and Water data is co-mingled with other data and, as a result, it is not possible to separate Alberta Environment and Water data from other data. Therefore, Alberta Environment and Water requires the following copyright and disclaimer as it relates to its data contained herein. The statements below apply only to the data provided by Alberta Environment and Water to prepare this report, not to other aspects of the report. Copyright and Terms of Use This material, including copyright and marks under the Trade-marks Act (Canada), is owned by the Government of Alberta and protected by law. Permission Statement This material may be used, reproduced, stored or transmitted for non-commercial purposes. However, Crown copyright is to be acknowledged. We ask that: Users exercise due diligence in ensuring the accuracy of the materials reproduced; Alberta Environment and Water be identified as the source; and The reproduction is not represented as an official version of the materials reproduced, nor as having been made, in affiliation with or with the endorsement of Alberta Environment and Water. If it is to be used, reproduced, stored or transmitted for commercial purposes, arrange first for consent by contacting: Alberta Environment and Water: Environmental Modeling Team Leader at (403) 297-6565 Disclaimer Information in this report is provided solely for the user’s information and, while thought to be accurate, is provided strictly “as is” and without warranty of any kind.