Climate Change Impacts on Streamflow in the Upper North Saskatchewan River Basin, Alberta

Total Page:16

File Type:pdf, Size:1020Kb

Climate Change Impacts on Streamflow in the Upper North Saskatchewan River Basin, Alberta CLIMATE CHANGE IMPACTS ON STREAMFLOW IN THE UPPER NORTH SASKATCHEWAN RIVER BASIN, ALBERTA MICHAEL W. NEMETH B.Sc., University of Lethbridge 2008 A Thesis Submitted to the School of Graduate Studies of the University of Lethbridge in Partial Fulfillment of the Requirements for the Degree MASTER OF SCIENCE Department of Geography University of Lethbridge LETHBRIDGE, ALBERTA, CANADA © Michael Wayne Nemeth, 2010 Abstract This research focuses on the estimation of the impacts of climate change on water yield, streamflow extremes, and the streamflow regimes in the Cline River Watershed, and consequently, water availability for hydropower generation in this area. The Cline River Watershed comprises the flow into Lake Abraham, the reservoir for Bighorn Dam, is part of the upper North Saskatchewan River basin (UNSRB). This objective was achieved by parameterizing the ACRU agro-hydrological modelling system. After parameterization was complete, ACRU output was calibrated and verified against available observed data, including temperature, snow water equivalent, glacier mass balance, potential evapotranspiration, and streamflow data. After ACRU was properly verified, five selected climate change scenarios to estimate impacts of climate change in this area. Overall water yields are projected to increase over time. A large shift in seasonality is likely the biggest impact climate change will have on water resources in the Cline River Watershed. iii Acknowledgements First and foremost I would like to thank my family; my wife, my daughter, and my parents who have always supported me in my undergraduate and graduate studies; thank you as this wouldn‟t have been possible without your support. This research was support by grants held by Dr. Stefan Kienzle from EPCOR and NSERC. Other financial support was provided by the University of Lethbridge. I would like to thank my supervisor Dr. Stefan Kienzle for all of his time and support on this project and patience with me, which truly made the difference to my learning and progress with this research. I would also like to thank my committee members; Dr. Jim Byrne for all his time and guidance with undergraduate and graduate work, Dr. Larry Flanagan for all his time and thoughts that helped me with several vegetation inputs and thesis improvements. As the external examiner, thank you to Dr. Greg Kiker for his thoughts and input which also helped improve this thesis. I would also like to thank everyone in the Department of Geography that made both my degrees from the University of Lethbridge a success in many ways. Thank you to Ryan MacDonald and Mark Mueller for their help during this project on all the data processing and collection that was done in all the different stages of this project. A special thanks to Ken Perl, Hester Jiskoot, and Craig Coburn for their advice and continued support, and Margaret Cook and Dana Andrei for their administrative support. Thank you to the School of Graduate Studies for their support through the entire length of my program. Thank you to Alison Buckingham from Parks Canada, Mike Seneka, Jon Pedlar, Rick Pickering, Ernst Kerkhoven, and Randy Sweeny from Alberta Environment, Craig Smith from Environment Canada with the data acquisition. iv Table of Contents Abstract ........................................................................................................................................... iii Acknowledgements ......................................................................................................................... iv Table of Contents ............................................................................................................................. v List of Figures .................................................................................................................................. x List of Tables ................................................................................................................................. xii Chapter 1: Thesis Introduction .................................................................................................... 1 1.1 Introduction ................................................................................................................................ 1 1.2 Research Objectives ................................................................................................................... 3 1.3 Thesis Structure ......................................................................................................................... 4 Chapter 2: Literature Review ....................................................................................................... 5 2.1 Introduction ................................................................................................................................ 5 2.2 Climate Change .......................................................................................................................... 5 2.2.1 Water Balance Equation ............................................................................................ 5 2.2.2 Global Climate Change and the Hydrological Cycle ................................................. 6 2.2.3 Climate Change and the Regional Hydrological Balance .......................................... 7 2.3 Observations of Climate and Hydrology in Western Canada .................................................... 8 2.3.1 Temperature ............................................................................................................... 8 2.3.2 Precipitation ............................................................................................................... 8 2.3.3 Evapotranspiration and Soil Moisture........................................................................ 9 2.3.4 Streamflow ............................................................................................................... 10 2.4 Future Trends in Climate and Potential Regional Effects ........................................................ 11 2.4.1 Physiological Response of Vegetation ..................................................................... 11 2.4.2 Affects of Forest Harvesting in UNSRB ................................................................. 12 2.4.3 Affects on Hydroelectric Power ............................................................................... 13 2.4.4 Glaciers .................................................................................................................... 14 2.4.5 Potential Impacts for Water Availability ................................................................. 15 2.5 Hydrological Modelling ........................................................................................................... 15 2.5.1 Classification of Hydrological Models .................................................................... 16 2.5.1.1 Conceptual Models .................................................................................. 16 2.5.1.2 Empirical Models ..................................................................................... 16 v 2.5.1.3 Physically Based Models ......................................................................... 17 2.6 Spatial Representation of Hydrological Processes ................................................................... 17 2.7 Spatial Climatic Data ............................................................................................................... 18 2.7.1 ANUSPLIN .............................................................................................................. 18 2.7.2 PRISM ..................................................................................................................... 18 2.8 The ACRU Agro-hydrological Modelling System .................................................................. 19 2.8.1 Theoretical Principles of ACRU .............................................................................. 19 2.8.2 Physical Processes of the ACRU Model .................................................................. 20 2.8.3 ACRU and Climate Change ..................................................................................... 22 2.9 Climate Scenario Development ............................................................................................... 23 2.9.1 Climate Scenarios .................................................................................................... 23 2.9.2 General Circulation Model Scenarios ...................................................................... 23 2.9.3 Regionalization Techniques ..................................................................................... 24 2.9.3.1 Statistical and Dynamic Downscaling ..................................................... 25 2.9.3.2 The Delta Change Method ....................................................................... 25 2.10 Summary ................................................................................................................................ 26 CHAPTER 3: Parameterization of the ACRU agro-hydrological modelling system and verification of hydrological processes for simulating potential climate change impacts in the upper North Saskatchewan River basin, Alberta, Canada. ..................................................... 27 3.1 Introduction .............................................................................................................................. 27 3.2 Study Area ..............................................................................................................................
Recommended publications
  • THE COLUMBIA ICE FIELDS by A
    30 CANADIAN SKI ANNUAL for the different kinds of snow which you to the end. The one who lagged behind will meet. believed that the other had some secret for I may have conveyed the impression that waxing, .but I am convinced it was simply the matter is more complicated than it that his ski were better and in better con­ really is in practice. My experience is that dition, so that the damp did not penetrate you cannot say, for instance, that if you and there was less strain on the wax. Also put on four layers of different wax the last he had laid a good foundation-coating so as layer will apply for the first hundred metres thoroughly to impregnate the ski. Moreover, and so on. he had certainly applied the wax on the day For a descent over varying kinds of snow before the run, rubbing it in well with his all that is necessary is to ensure that the hand. This makes an enormous difference. wax shall not be absolutely unfitted for the It is also a good thing to add a little various kinds of snow you meet, so thatyou paraffin as the last layer, especially if the do not, for instance, run into powder snow snow is wet, or if the temperatUl'e is at with fresh Klister, for in that case you will zero, or if snow is falling. This may prevent stop dead. In other words, you want a small bits of ice from forming under the ski. wax which does not directly conflict with the If you really want to wax conscientiously, quality of the snow and which will last to vou should not omit to wax the sides of the the end of the run.
    [Show full text]
  • Information Package Watercourse
    Information Package Watercourse Crossing Management Directive June 2019 Disclaimer The information contained in this information package is provided for general information only and is in no way legal advice. It is not a substitute for knowing the AER requirements contained in the applicable legislation, including directives and manuals and how they apply in your particular situation. You should consider obtaining independent legal and other professional advice to properly understand your options and obligations. Despite the care taken in preparing this information package, the AER makes no warranty, expressed or implied, and does not assume any legal liability or responsibility for the accuracy or completeness of the information provided. For the most up-to-date versions of the documents contained in the appendices, use the links provided throughout this document. Printed versions are uncontrolled. Revision History Name Date Changes Made Jody Foster enter a date. Finalized document. enter a date. enter a date. enter a date. enter a date. Alberta Energy Regulator | Information Package 1 Alberta Energy Regulator Content Watercourse Crossing Remediation Directive ......................................................................................... 4 Overview ................................................................................................................................................. 4 How the Program Works .......................................................................................................................
    [Show full text]
  • Upper North Saskatchewan River and Abraham Lake Bull Trout Study, 2002 - 2003
    Upper North Saskatchewan River and Abraham Lake Bull Trout Study, 2002 - 2003 CONSERVATION REPORT SERIES The Alberta Conservation Association is a Delegated Administrative Organization under Alberta’s Wildlife Act. CCONSERVATIONONSERVATION RREPORTEPORT SSERIESERIES 25% Post Consumer Fibre When separated, both the binding and paper in this document are recyclable Upper North Saskatchewan River and Abraham Lake Bull Trout Study, 2002 – 2003 Marco Fontana1, Kevin Gardiner2 and Mike Rodtka2 1 Alberta Conservation Association 113 ‐ 1 Street Cochrane, Alberta, Canada T4C 1B4 2 Alberta Conservation Association 4919 – 51 Street Rocky Mountain House, Alberta, Canada T4T 1B3 Report Series Editor PETER AKU KELLEY J. KISSNER Alberta Conservation Association 59 Hidden Green NW #101, 9 Chippewa Rd Calgary, AB T3A 5K6 Sherwood Park, AB T8A 6J7 Conservation Report Series Type Data, Technical ISBN printed: 978‐0‐7785‐6573‐4 ISBN online: 978‐0‐7785‐6574‐1 Publication No.: T/165 Disclaimer: This document is an independent report prepared by the Alberta Conservation Association. The authors are solely responsible for the interpretations of data and statements made within this report. Reproduction and Availability: This report and its contents may be reproduced in whole, or in part, provided that this title page is included with such reproduction and/or appropriate acknowledgements are provided to the authors and sponsors of this project. Suggested Citation: Fontana, M., K. Gardiner, and M. Rodtka. 2006. Upper North Saskatchewan River and Abraham Lake Bull
    [Show full text]
  • Bighorn Backcountry Public Land Use Zones 2019
    Edson 16 EDMONTON Hinton 47 22 Jasper 39 734 Bighorn Backcountry PLUZs 2 22 National Bighorn The Bighorn Backcountry is managed to ensure the Backcountry Park protection of the environment, while allowing responsible 11 and sustainable recreational use. The area includes more than Rocky 11 5,000 square kilometres (1.2 million acres) of public lands east Mountain House 54 of Banff and Jasper National Parks. 734 27 The Bighorn Backcountry hosts a large variety of recreational Banff National 22 activities including camping, OHV and snow vehicle use, hiking, shing, Park hunting and cycling. CALGARY 1 It is your responsibility to become familiar with the rules and activities allowed in this area before you visit and to be informed of any trail closures. Please refer to the map and chart in this pamphlet for further details. Visitors who do not follow the rules could be ned or charged under provincial legislation. If you have any concerns about the condition of the trails and campsites or their appropriate use, please call Alberta Environment and Parks at the Rocky Mountain House Ofce, 403-845-8250. (Dial 310-0000 for toll-free service.) For current trail conditions and information kiosk locations, please visit the Bighorn Backcountry website at www.alberta.ca Definitions for the Bighorn Backcountry Motorized User ✑ recreational user of both off-highway vehicles and snow vehicles. Equestrian User or ✑ recreational user of both horses and/or mules, used for trail riding, pack Equine horse, buggy/cart, covered wagon or horse-drawn sleigh. Non-Motorized User ✑ recreational user which is non-motorized except equestrian user or equine where specified or restricted.
    [Show full text]
  • This Work Is Licensed Under the Creative Commons Attribution-Noncommercial-Share Alike 3.0 United States License
    This work is licensed under the Creative Commons Attribution-Noncommercial-Share Alike 3.0 United States License. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc-sa/3.0/us/ or send a letter to Creative Commons, 171 Second Street, Suite 300, San Francisco, California, 94105, USA. THE TIGER BEETLES OF ALBERTA (COLEOPTERA: CARABIDAE, CICINDELINI)' Gerald J. Hilchie Department of Entomology University of Alberta Edmonton, Alberta T6G 2E3. Quaestiones Entomologicae 21:319-347 1985 ABSTRACT In Alberta there are 19 species of tiger beetles {Cicindela). These are found in a wide variety of habitats from sand dunes and riverbanks to construction sites. Each species has a unique distribution resulting from complex interactions of adult site selection, life history, competition, predation and historical factors. Post-pleistocene dispersal of tiger beetles into Alberta came predominantly from the south with a few species entering Alberta from the north and west. INTRODUCTION Wallis (1961) recognized 26 species of Cicindela in Canada, of which 19 occur in Alberta. Most species of tiger beetle in North America are polytypic but, in Alberta most are represented by a single subspecies. Two species are represented each by two subspecies and two others hybridize and might better be described as a single species with distinct subspecies. When a single subspecies is present in the province morphs normally attributed to other subspecies may also be present, in which case the most common morph (over 80% of a population) is used for subspecies designation. Tiger beetles have always been popular with collectors. Bright colours and quick flight make these beetles a sporting and delightful challenge to collect.
    [Show full text]
  • HDP 2006 05 Report 1
    Report #1 1998 CWS Air Surveys In response to a general lack of knowledge on the abundance and distribution of the Harlequin Duck within Alberta, the Canadian Wildlife Service in cooperation with Alberta Environment undertook helicopter surveys of the eastern slopes of Alberta in 1998 and 1999. In 1998 the survey area encompassed streams along the eastern slopes of Alberta between the communities of Grande Cache and Nordegg. Ground truthing was provided by foot surveys on the McLeod River conducted by Bighorn Wildlife Technologies Ltd. Local area biologists helped with selection of blocks of streams to be surveyed where harlequins were most likely to occur and assisted in the helicopter surveys. Helicopter survey methods are detailed in Gregoire et al. (1999). Global Positioning Coordinates (GPS) were recorded for all sightings as well as survey start and end points. The Universal Transverse Mercator (UTM) coordinate system was used for recording sightings of Harlequin Duck and other wildlife. Survey start and end points were recorded in Latitude and Longitude. Five digit numbers hand written in the field survey reports represent the BSOD (now WHIMIS) ID number for that observation. What this document contains. - A summary of the 1998 surveys (Gregoire et al. 1999. Canadian Wildlife Service Technical Report Series No. 329), - The field results for the helicopter survey conducted between the Brazeau and North Saskatchewan Rivers - The results of a foot survey on the Blackstone River. , · Harlequin L?.uck ·surveys in the Centr~I - .Eastern Slopes o.f Albert9: . ·Spring 1998. T - • ~ Paul Gr~goire, Jeff Kneteman and Jim Allen . .-"• r, ~ ~-. Prairie and Northern Region 1999 .1;._-, - 1 ,~ .Canadian Wildlife Service '' ,· ~: ,.
    [Show full text]
  • Day Hikes in Jasper National Park
    Parks Pares Canada Canada All around you are the natural wonders of Jasper National around to the starting point, and the one to the right leads to Park. To explore some of its valleys and mountainsides, the Valley of the Five Lakes. National Parks Centenaire des hike the trails described in this folder. Ranging from short, 1985 Centennial parcs nationaux easy walks to longer uphill treks, these hikes all take a day Pyramid Lake or less. The trail descriptions include trail length, access • LEGEND and an outline of the terrain and features. DAY HIKES IN Length — 17.4 km Highway Overnight hikes are also available in the park. Before Trailheads — If you are on foot, you may start from the Secondary Road heading into the backcountry on overnight trips, ask for townsite at the parking lot opposite the swimming pool. As JASPER information and your park use permit at the trail office in well, there are numerous access points along Pyramid Fire Road Jasper townsite or at the Icefields Centre. Lake Road: the parking lot at Cottonwood Slough, the Hiking Trail NATIONAL PARK riding stables, Pyramid Lake Motel and the Pyramid Lake Self-guiding Trail An exciting possibility on any hike is seeing some of the Island picnic area. wildlife native to the park. Never forget that these animals Picnic Area are wild and can be dangerous if approached. Before This is actually a number of trails joined together which Campground setting out, take time to read the "You Are in Bear wind over the Pyramid Bench, an escarpment above Jasper Riding Stable Country" folder available at most park offices and townsite.
    [Show full text]
  • Glaciers of the Canadian Rockies
    Glaciers of North America— GLACIERS OF CANADA GLACIERS OF THE CANADIAN ROCKIES By C. SIMON L. OMMANNEY SATELLITE IMAGE ATLAS OF GLACIERS OF THE WORLD Edited by RICHARD S. WILLIAMS, Jr., and JANE G. FERRIGNO U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1386–J–1 The Rocky Mountains of Canada include four distinct ranges from the U.S. border to northern British Columbia: Border, Continental, Hart, and Muskwa Ranges. They cover about 170,000 km2, are about 150 km wide, and have an estimated glacierized area of 38,613 km2. Mount Robson, at 3,954 m, is the highest peak. Glaciers range in size from ice fields, with major outlet glaciers, to glacierets. Small mountain-type glaciers in cirques, niches, and ice aprons are scattered throughout the ranges. Ice-cored moraines and rock glaciers are also common CONTENTS Page Abstract ---------------------------------------------------------------------------- J199 Introduction----------------------------------------------------------------------- 199 FIGURE 1. Mountain ranges of the southern Rocky Mountains------------ 201 2. Mountain ranges of the northern Rocky Mountains ------------ 202 3. Oblique aerial photograph of Mount Assiniboine, Banff National Park, Rocky Mountains----------------------------- 203 4. Sketch map showing glaciers of the Canadian Rocky Mountains -------------------------------------------- 204 5. Photograph of the Victoria Glacier, Rocky Mountains, Alberta, in August 1973 -------------------------------------- 209 TABLE 1. Named glaciers of the Rocky Mountains cited in the chapter
    [Show full text]
  • University of Alberta the Backcountry
    University of Alberta The Backcountry as Home: Park Wardens, Families, and Jasper National Park’s District Cabin System, 1952-1972 by Nicole Eckert-Lyngstad A thesis submitted to the Faculty of Graduate Studies and Research in partial fulfillment of the requirements for the degree of Master of Arts Anthropology ©Nicole Eckert-Lyngstad Spring 2013 Edmonton, Alberta Permission is hereby granted to the University of Alberta Libraries to reproduce single copies of this thesis and to lend or sell such copies for private, scholarly or scientific research purposes only. Where the thesis is converted to, or otherwise made available in digital form, the University of Alberta will advise potential users of the thesis of these terms. The author reserves all other publication and other rights in association with the copyright in the thesis and, except as herein before provided, neither the thesis nor any substantial portion thereof may be printed or otherwise reproduced in any material form whatsoever without the author's prior written permission. Abstract This research examines home life as experienced by single and married National Park Wardens, their partners and children who resided year-round in the backcountry of Jasper National Park (JNP) between 1952 and 1972. Since the establishment of JNP in 1907, park wardens were responsible for maintaining, monitoring and patrolling large backcountry districts, and used cabins as home bases and overnight shelters. Although the district system officially ended in 1969 and no wardens have lived year-round in the backcountry since 1972, these historic cabins remain in the park and are maintained for use by current park personnel.
    [Show full text]
  • Trails Parks, Provincial Recreations Areas and Events
    David Thompson PARKS The David Thompson Country Tourism Region Country encompasses the municipalities of Caroline, Clearwater County, and Rocky Mountain House. Crimson Lake Ram Falls Rocky Mountain House Landslide Hike Highlights of the area include Abraham Lake, Provincial Park Provincial Park National Historic Site Burnstick Lake, Cow Lake, Crimson Lake, Nordegg and Ya Ha Tinda. While the above parks are the most well-known, David Thompson Please visit our website for more information and Country has over twenty Provincial listings of hotels, restaurants, campgrounds, trails Parks, Provincial Recreations Areas and events. and Wilderness Areas for you to where explore. You can find them listed Alberta Parks Bighorn Backcountry at the link. Listing Link Trails link www.davidthompsoncountry.ca Clearwater River Horse Trails When in David Thompson Country you can find TRAILS more visitor information at: DTC has a variety of trails to explore, from multi use If you’re looking for motorized access for your ATV, Rocky Mountain House Visitor Information Centre trails to motorized and non-motorized specific trails. OHV, or Motorbike there are designated areas for you Monday – Friday, 9 AM – 5 PM Our hiking trails vary in difficulty from short walks to enjoy. One area to explore is the Clearwater Trails Ph: 403-845-5450 suitable for a soft adventure seeker to hikes that will Initiative west of Caroline and the Bighorn area also Toll Free: 1-800-565-3793 challenge the hard-core adventurer. has dedicated motorized trails as well. E-mail: [email protected] Mountain and trail biking are popular There are plenty of areas for horses activities as well, with Nordegg and and we have ranches and outfitters Village of Caroline Office Baseline Mountain being two popular offering guided trail rides if you have Tuesday – Friday, 9 AM – 4 PM destinations.
    [Show full text]
  • Indigenous Water Rights & Global Warming in Alberta
    University of Calgary PRISM: University of Calgary's Digital Repository University of Calgary Press University of Calgary Press Open Access Books 2018-05 Water Rites: Reimagining Water in the West University of Calgary Press Ellis, J. (Ed.). (2018). Water Rites: Reimagining Water in the West. Calgary, AB: University of Calgary Press. http://hdl.handle.net/1880/107767 book https://creativecommons.org/licenses/by-nc-nd/4.0 Attribution Non-Commercial No Derivatives 4.0 International Downloaded from PRISM: https://prism.ucalgary.ca WATER RITES: Reimagining Water in the West Edited by Jim Ellis ISBN 978-1-55238-998-0 THIS BOOK IS AN OPEN ACCESS E-BOOK. It is an electronic version of a book that can be purchased in physical form through any bookseller or on-line retailer, or from our distributors. Please support this open access publication by requesting that your university purchase a print copy of this book, or by purchasing a copy yourself. If you have any questions, please contact us at [email protected] Cover Art: The artwork on the cover of this book is not open access and falls under traditional copyright provisions; it cannot be reproduced in any way without written permission of the artists and their agents. The cover can be displayed as a complete cover image for the purposes of publicizing this work, but the artwork cannot be extracted from the context of the cover of this specific work without breaching the artist’s copyright. COPYRIGHT NOTICE: This open-access work is published under a Creative Commons licence. This means that you are free to copy, distribute, display or perform the work as long as you clearly attribute the work to its authors and publisher, that you do not use this work for any commercial gain in any form, and that you in no way alter, transform, or build on the work outside of its use in normal academic scholarship without our express permission.
    [Show full text]
  • Northern Rockies
    TransCanada Ecotours® TransCanada “This book wonderfully Let the Northern Rockies Ecotour set your compass Discover the secrets of a spectacular interlaces the physical, for a remarkable journey of discovery through the Canadian landscape with the biological and historical northern part of the Canadian Rocky Mountain qualities of one of Parks World Heritage site. 265 photos, 22 maps and TransCanada Ecotours® Canada’s iconic regions. 133 Ecopoints present the region’s rich First Nations An entertaining but highly history, exploits of early fur-traders, artists, mission- aries, tourists, and scientists, and the ongoing inter- educational account that Northern play of people, wildlife and their inspiring mountain will captivate all who ecosystem. The authors draw on current research traverse the Northern to discuss key environmental issues such as climate Rockies be it by bike, car, Rockies change and biodiversity conservation. train or vicariously from their living room.” You will explore the eastern foothills (Chapter One) Highway Guide ending in historic Grande Cache, then travel west on NIK LOPOUKHINE CHAIR IUCN WORLD COMMISSION the Yellowhead Highway (Chapter Two) following ON PROTECTED AREAS major rivers across the continental divide from Hinton Guide Northern Rockies Highway to Valemount, British Columbia. In the concluding Chapter Three, the Ecotour turns southwards from Jasper along the spectacular Icefields Parkway through the Rockies, ending near Lake Louise. See the full route map on page 5 INSTITUTE RESEARCH FOOTHILLS $24.95 P.O. Box 6330 A lavishly illustrated driving guide 133 points of interest, 265 photos, 1176 Switzer Drive to the landscapes, geology, ecology, 22 maps that include: Hinton, Alberta T7V 1X6 culture, people and history of the Hinton – Cadomin – Grande Cache – Canada Northern Rockies Region of Alberta Jasper – Valemount – and the and British Columbia.
    [Show full text]