Cumulative Effects Assessment of the North Saskatchewan River Watershed Using ALCES
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Fisheries Barriers in Native Trout Drainages
Alberta Conservation Association 2018/19 Project Summary Report Project Name: Fisheries Barriers in Native Trout Drainages Fisheries Program Manager: Peter Aku Project Leader: Scott Seward Primary ACA Staff on Project: Jason Blackburn, David Jackson, and Scott Seward Partnerships Alberta Environment and Parks Environment and Climate Change Canada Key Findings • We compiled existing barrier location information within the Peace River, Athabasca River, North Saskatchewan River, and Red Deer River basins into a centralized database. • We catalogued fish habitat and community data for the Narraway River watershed for use in a population restoration feasibility framework. • We identified 107 potential barrier locations within the Narraway River watershed, using Google Earth ©, which will be refined using valley confinement modeling and validated with ground truthing in 2019. Introduction Invasive species pose one of the greatest threats to Alberta native trout species, through hybridization, competition, and displacement. These threats are partially mediated by the presence of natural headwater fish-passage barriers, namely waterfalls, that impede upstream 1 invasions. In Alberta, several sub-populations of native trout remain genetically pure primarily because of waterfalls. Identification and inventory of waterfalls in the Peace River, Athabasca River, North Saskatchewan River, and Red Deer River basins isolating pure populations and their habitats is critical to inform population recovery and build implementation strategies on a stream by stream basis. For example, historical stocking of non-native trout to the Narraway River watershed may be endangering native bull trout and Arctic grayling. Non-native cutthroat trout, rainbow trout, and brook trout have been stocked in the Torrens River, Stetson Creek, and Two Lakes, all of which have connectivity to the Narraway River. -
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 ....................................................................................................................... -
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 -
Land Use, Climate Change and Ecological Responses in the Upper
Land use, climate change and ecological responses in the Upper North 1 Saskatchewan and Red Deer River Basins: A scientific assessment Land use, climate change and ecological responses in the Upper North Saskatchewan and Red Deer River Basins: A scientific assessment Dan Farr, Colleen Mortimer, Faye Wyatt, Andrew Braid, Charlie Loewen, Craig Emmerton, Simon Slater Cover photo: Wayne Crocker This publication can be found at: open.alberta.ca/publications/9781460140697. Comments, questions, or suggestions regarding the content of this document may be directed to: Ministry of Environment and Parks, Environmental Monitoring and Science Division 10th Floor, 9888 Jasper Avenue NW, Edmonton, Alberta, T5J 5C6 Tel: 780-229-7200 Toll Free: 1-844-323-6372 Fax: 780-702-0169 Email: [email protected] Media Inquiries: [email protected] Website: environmentalmonitoring.alberta.ca Recommended citation: Farr. D., Mortimer, C., Wyatt, F., Braid, A., Loewen, C., Emmerton, C., and Slater, S. 2018. Land use, climate change and ecological responses in the Upper North Saskatchewan and Red Deer River Basins: A scientific assessment. Government of Alberta, Ministry of Environment and Parks. ISBN 978-1-4601-4069-7. Available at: open.alberta.ca/publications/9781460140697. © Her Majesty the Queen in Right of Alberta, as represented by the Minister of Alberta Environment and Parks, 2018. This publication is issued under the Open Government Licence - Alberta open.alberta.ca/licence. Published September 2018 ISBN 978-1-4601-4069-7 Land use, climate change and ecological responses in the Upper North 2 Saskatchewan and Red Deer River Basins: A scientific assessment Acknowledgements The authors are grateful to the external reviewers for providing their technical reviews and feedback, which have enhanced this work. -
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. -
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. -
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. -
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 '' ,· ~: ,. -
North Saskatchewan River Drainage, Fish Sustainability Index Data Gaps Project, 2015
North Saskatchewan River Drainage, Fish Sustainability Index Data Gaps Project, 2015 The Alberta Conservation Association is a Delegated Administrative Organization under Alberta’s Wildlife Act. North Saskatchewan River Drainage, Fish Sustainability Index Data Gaps Project, 2015 Mike Rodtka, Chad Judd and Andrew Clough Alberta Conservation Association 101 – 9 Chippewa Road Sherwood Park, Alberta, Canada T8A 6J7 Report Editors PETER AKU KELLEY KISSNER Alberta Conservation Association 50 Tuscany Meadows Cr. NW 101 – 9 Chippewa Rd. Calgary, AB T3L 2T9 Sherwood Park, AB T8A 6J7 Conservation Report Series Type Data ISBN: 978-0-9949118-3-4 Disclaimer: This document is an independent report prepared by 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: Rodtka, M., C. Judd, and A. Clough. 2016. North Saskatchewan River drainage, Fish Sustainability Index data gaps project, 2015. Data Report, D-2016-105, produced by Alberta Conservation Association, Sherwood Park, Alberta, Canada. 17 pp + App. Cover photo credit: David Fairless Digital copies of conservation reports can be obtained from: Alberta Conservation Association 101 – 9 Chippewa Rd. Sherwood Park, AB T8A 6J7 Toll Free: 1-877-969-9091 Tel: (780) 410-1998 Fax: (780) 464-0990 Email: [email protected] Website: www.ab-conservation.com i EXECUTIVE SUMMARY Alberta Environment and Parks Fish Sustainability Index is a standardized process of assessment that provides a landscape-level overview of fish sustainability within the province and enables broad-scale evaluation of management actions and land-use planning. -
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. -
Northern Leopard Frog Recovery Program
Northern Leopard Frog Recovery Program Year 5 (2003) Kris Kendell In cooperation with: Northern Leopard Frog Recovery Program Year 5 (2003) This publication may be cited as: Kendell, K. 2004. Northern leopard frog recovery program: Year 5 (2003). Unpublished report, Alberta Conservation Association, Edmonton, AB. 14 pp. ii TABLE OF CONTENTS ACKNOWLEDGEMENTS....................................................................................................... iv EXECUTIVE SUMMARY ........................................................................................................ v 1.0 INTRODUCTION .................................................................................................................... 1 2.0 STUDY AREA ......................................................................................................................... 2 2.1 Egg mass collection and frog release sites........................................................................ 2 2.2 Captive rearing site ........................................................................................................... 2 3.0 METHODS ............................................................................................................................... 3 3.1 Captive rearing.................................................................................................................. 3 3.2 Marking............................................................................................................................. 3 3.3 Release (2003) ................................................................................................................. -
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