Extreme Flow Metering

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Extreme Flow Metering From Mountains to Muskeg Under Ice to Flood Flows History • 1968 – 1976 –WSC – Calgary Region ‐ Hydrometric Technician –Metering, Flow Computations and Snow Surveys • 1977 – 2002 –AENV –Southern Alberta ‐ Technologist/Manager –Hydrometrics, Snow Surveys, Telemetry, Flow Forecasting, Hydrology, Etc. • 2002 ‐ ???? – 1511639 –Alberta Ltd. ‐ Compliance Monitoring –Ski Areas, Pipe Flows, Oil Companies, Alberta Environment, Hydraulic Fracturing Extractions, Various Hydrology Studies, Inspections and Reports for the Alberta Disaster Recovery Program since 2010. Open Water Flow Metering • Methods Wading, Bridges, Cableways • Difficulties ‐Weeds, Beaver Dams, Uneven Channels, Etc. ‐ Site selections and Access, Etc. 622AA Price Meter Wading with Price AA • Forty Mile Creek at Mt. Norquay Find the Creek –or River! Liard River near the NWT Border Tsea River ‐Defined Channel ‐ May Same Channel ‐ June Try to meter flow here! ‐ July Or Here! On top of an old beaver dam! Deep Channel – Medium Risk! After Runoff –Low Risk Spring Runoff –High Risk! Ideal Conditions! Bridge Frame and A‐Reel Bow River @ Calgary –Peak 2013 ‐ June 21 – 07:00 Bow @ Calgary –After Peak 2013 – June 26 @ 15:00 Elbow River U/S Hwy #22 – June 20, 2013 ‐ Peak Elbow River D/S Hwy 22 – June 20, 2013 ‐ Peak Standing Waves Flood debris –metering hazard! Sunshine Parking Lot – June 21, 2013 Healy Creek –Old Channel Bridge Measurements ‐ Miscellaneous Cableways • Most accurate and efficient –next to wading. • Safety issues and litigation. • Specs have been beefed up. • Safety checked yearly • Used by both WSC and USGS North Milk River at Western Crossing Cableway vs. Bridge Bow River @ Carseland ‐ 2005 Cattle Rub Ice Measurements • Not always “under ice” – thus the heading! • Always safety issues – requires training –and common sense. • Rescue • Equipment • Technique • Dynamics –temperature and depth. 6240AA Price Ice Meter Under Ice Flow Metering –High Risk! Channel jamming and filling! Anchor Ice – Channel full –Flow Abating A dam of ice is building upstream…. The wading section D/S an hour later ‐ No ice to chop! Usual wading site –Forty‐Mile Creek near Banff Just Upstream! 100 meters upstream –close to release! Logger water level data Snow Surveying –Nigel Creek below Parker Ridge ‐ 1984 Other Hazards! Bear Tracks Wolf Tracks Helicopters Various incidents –Before OH&S near miss reporting No report necessary to document –just a lasting memory! • Bridge –South Sask. @ Medicine Hat – 1995 Flood • Cableway –Red Deer below below Burnt Timber ‐ 1974 • Cableway‐ McLeod River near Wolf Creek – June 1972 • On Ice – McLeod River near Wolf Creek –April 1972 • Cableway –North Sask. Near Rocky Mtn. House – 1969 • Snow Surveys –South Racehorse –March 30, 2002..

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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.
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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.
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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.
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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.
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Wild Lands Advocate Vol. 14, No. 5, October 2006
October 2 006 • Vol. 14, No. Vol. 006 • 5 AWA The White Goat Wilderness — H. Unger THE QUIET URBANIZATION OF THE BACKCOUNTRY / 4 GOVERNMENT HOG-TIES COMMITTEE FOR CARIBOU RECOVERY / 12 EASTERN SLOPES CUMULATIVE EFFECTS STUDY FILLS GAP / 13 ALL ROADS MUST LEAD TO ALBERTAʼS MECCA / 15 Editorial Board: UPDATES Shirley Bray, Ph.D. COCTOBERONTENTS 2006 • VOL. 14, NO. 5 Andy Marshall 24 GLENBOW RANCH A WELCOME ADDITION TO PARKS SYSTEM Joyce Hildebrand OUT FRONT 24 OIL SANDS MULTI-STAKEHOLDER Printing by: PANEL HEARS FROM THE PUBLIC 4 THE QUIET URBANIZATION OF THE Colour printing and process is BACKCOUNTRY: PART 4 25 GHOST-WAIPAROUS: IS THERE LIFE sponsored by Topline Printing AFTER GAMP? 10 PETER SHERRINGTON: LINKING PEOPLE TO RAPTORS AND 25 CHEVIOT MINE BACK UNDER NATURAL WORLD UNITED NATIONS’ SPOTLIGHT ALBERTA WILDERNESS WATCH PROFILE 12 GOVERNMENT HOG-TIES 26 GRACE BUZIK: ARTIST’S COMMITTEE FOR CARIBOU ATTENTION TO DETAIL BRINGS RECOVERY WILDLIFE IMAGES TO LIFE 13 CUMULATIVE EFFECTS STUDY Graphic Design: LETTTERS TO THE EDITOR FILLS GAP IN SOUTH EASTERN Ball Creative SLOPES PLANNING 29 BACKPACKERS SHARE MANY GIFTS 15 ALL ROADS MUST LEAD TO OF WHITE GOAT WILDERNESS Wild Lands Advocate is ALBERTA’S MECCA: LAKELAND published bimonthly, 6 times 29 CROWSNEST PASS: THE GOOD, THE PARK HIGHWAY PROPOSAL BAD AND THE UGLY a year, by Alberta Wilderness RESURRECTED Association. The opinions 17 STUDY SHOWS CHRONIC WASTING ASSOCIATION NEWS expressed by the authors DISEASE SPREADS THROUGH in this publication are not SALIVA, BLOOD 27 STEWARDSHIP ETHIC MARKS necessarily those of AWA. ASSOCIATION’S WORK 18 PUBLIC INTEREST GROUPS PREPARE The editors reserve the right FOR HEARINGS ON ENCANA’S 31 AWA WILD WEST GALA 2006 to edit, reject or withdraw SUFFIELD DRILLING PROJECT articles and letters submitted.
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Snow Survey Stations Within Or Bordering the Province of Alberta
Snow Survey Stations Within or Bordering the Province of Alberta Andrew Lake Charles Lake Bistcho Lake Slave River · FORT NELSON A ^_ Margaret Lake Lake Athabasca SWEETGRASS ^_ Zama Lake Baril Lake ^_ FORT CHIPEWYAN ASSUMPTION ^_ Mamawi Lake Lake Claire HIGH LEVEL ^_ FORT VERMILION ^_ Richardson Lake ^_ EMBARRAS PORT Peace River KEG RIVER ^_ PINK MOUNTAIN ^_ Wabasca River ^_ NORTH STAR Clearwater River GORDON LAKE LO !( EUREKA RIVER Peerless Lake ^_ Gordon Lake FORT ST. JOHN A ^_ BULLHEAD MOUNTAIN Cardinal Lake ^_ FAIRVIEW ^_ North Wabasca Lake South Wabasca Lake Utikuma Lake GIROUXVILLE RYCROFT ^_ ^_ PINE PASS ^_ Winefred Lake SEXSMITH ^_ HYTHE HIGH PRAIRIE Lesser Slave Lake ^_ ^_ BEZANSON West Prairie River ^_ ^_ KINUSO Calling Lake SAULTEAUX RIVER Driftpile River ^_ STURGEON HEIGHTS East Prairie River Swan River Smoky River Wapiti River ^_ HOUSE MOUNTAIN LO !( SPRING CREEK#1 ^_ MOKAMAM CREEK ^_ GRASSLANDLac la Biche ^_ LITTLE SMOKY MOUNT SHEBA ^_ FLATBUSH ^_ ^_ Athabasca River Cold Lake BONNYVILLE Cutbank River ^_ PERRYVALE Simonette River KNUDSEN LAKE ^_ ^_ BARRHEAD NORTH _ ^ WASKATENAU Muriel Lake ^_ BARRHEAD WEST ^_ BELLIS ^_ ST. PAUL ^_ WHITECOURT TWIN LAKES ^_!( ^_ ^_ ^_ WESTLOCK Frog Lake REVOLUTION CREEK Muskeg River MEADOWVIEW ^_ MORINVILLE PADDLE RIVER HEADWATERS ^_!( ^_ ^_ TWO HILLS MAYERTHORPE ONOWAY ^_ Ste. Anne, Lac ^_ Chip Lake CLANDONALD EDSON #2 ELK ISLAND PARK ^_ HINTON OBED McLeod River ^_ ^_ ^_ ^_ LODGEPOLE Wabamun Lake ^_ Beaverhill Lake HOLMES RIVER ^_ BRUCE S.PBirch Lake North Saskatchewan River LEDUC ^_ ^_ MANNVILLE ^_ BRAZEAU RES.
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ICEFIELDS PARKWAY Driving Guide
ICEFIELDS PARKWAY driving guide an eBook from Parkways of the Canadian Rockies, the region’s original and most comprehensive driving guide | by Brian Patton CONTENTS 2 Herbert Lake .................................................................................................................. 4 Crowfoot Glacier ....................................................................................................... 6 Bow Lake ........................................................................................................................... 7 Peyto Lake ........................................................................................................................ 9 Upper Waterfowl Lake ........................................................................................ 11 Lower Waterfowl Lake ........................................................................................ 11 Mistaya Canyon ........................................................................................................... 12 David Thompson Highway ............................................................................... 14 Rampart Creek ............................................................................................................. 15 Graveyard Flats ............................................................................................................ 15 Weeping Wall ............................................................................................................... 16 Big Bend ............................................................................................................................
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HIGHWAY North America, but Certainly One of the Most Access WHY ARE GLACIERS RECEDING ? to Support a Tremendous Weight
THE COLUMBIA ICE-FIELD mass of ice in the valley reaches lower altitudes CARRYING POWER ATHABASCA GLACIER melting takes place during the summer months, CANADA'S The Columbia Ice-field, centre of the greatest One of the most interesting characteristics of a forming glacial streams. The Athabasca Glacier has been receding rapidly CANADA'S ICE-FIELD known accumulation of ice in the Rocky Mountains, glacier is its carrying power. Although it is in motion in recent years. Records of the Water Resources is not only one of the most interesting ice-fields in like a plastic substance, it is solid and strong enough Division of the Engineering and Water Resources HIGHWAY North America, but certainly one of the most access WHY ARE GLACIERS RECEDING ? to support a tremendous weight. Debris torn from Branch, Department of Northern Affairs and National ible. Near the Highway, it lies astride the British the mountainside obscures its edge, so that often The present glaciers are the remnants of the con Resources, show that the average yearly recession Columbia-Alberta boundary and at the dividing line one may walk 50 yards out before the ice can be tinental ice-cap which once covered a large part of (1945-1949) has been 102 feet. It has well-defined between Banff and Jasper National Parks. seen. This fringe of broken rock carried on the edge HI-FI ELD the northern half of this continent. In earlier times and apparently recently formed terminal and mar Scenic beyond adequate description, this spectac of the glacier is called a marginal moraine.
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The Icefields Parkway
Parks Pares Because the Icefields Parkway is not a through-road The Life (Hardisty), mountaineers (Stutfield), explorers (Hector) Columbia Icefield Area Canada Canada like the Trans-Canada, all vehicles travelling it must or packers (Peyto). Others, such as Tangle Ridge, Cirque As the parkway climbs high passes and plunges into The largest of the chain of icefields along the Great 188f3—1985:100 Years of Heritage Conservation have a national park motor vehicle licence. Lake and the Weeping Wall, are simply descriptive. valleys, you will pass through three different life zones Divide is the Columbia Icefield. This 325 km2 accumu and will have a good chance of seeing wildlife, espe lation of ice feeds eight large glaciers, three of which cially at dawn and dusk. The map on the reverse side Stops of Interest — the Athabasca, the Dome, and the Stutfield — can indicates some good places to see moose, wapiti, goats, be seen from the parkway. Better yet, you can actually In the Shadow of the Great Divide ... and sheep. Black bears and deer are also seen from Bow Summit touch a glacier. A short side trip from the parkway time to time. Please slow down and drive with extra takes you to the toe of the Athabasca Glacier. care when you see animals beside the road. The highest point on the parkway is Bow Summit, 2088 m above sea level and 40 km north of Lake A visit to the Columbia Icefield Centre (easily visible Some of these animals may appear tame, but they can Louise. Here, the road crosses alpine meadows near beside the parkway) will help you discover what there The Icefields all be dangerous.
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Jasper Totale Km Percorsi in Auto
Jasper INFO Clima Totale Km percorsi in Auto : ___________ 8 Tempo di percorrenza senza soste : 3h30’ Jasper Alba : 06:22 Tramonto : 21:33 AGOSTO Stato : Alberta Temperature : 8°/22° 07.30 – 08.40 Banff/Bow Lake – 95Km – 1h 10’ (senza soste) Trasferimento a Bow Lake, percorrere il primo tratto della Icefields Parkway fino al lago, prendere il sentiero n°52, Bow Glacier Falls, 4,6Km sola andata, 155m di dislivello, 3 ore stimate. 11.40 – 11.50 Bow Lake/Peyto Lake – 7Km – 10’ Trasferimento a Peyto Lake, è possible percorrere brevi sentieri che portano a punti panoramici sul lago. 12.30 – 13.00 Peyto Lake/Saskatchewan River Crossing – 35Km – 30’ (senza soste) Percorrere la Icefields Parkway ad andatura “turistica” fermandosi in prossimità dei laghi Mistaya Lake, Cirque Lake e Chephren Lake che offrono dei bei punti panoramici, prima del ponte che attraversa il Saskatchewan River, sulla sinistra si trovano vari affacci sul Mistaya Canyon da non perdere, arrivo alla località Saskatchewan River Crossing dove è possible fermarsi a mangiare e rifornirsi. 14.00 – 14.40 Saskatchewan River Crossing/Icefield Centre – 50Km – 40’ (senza soste) Lasciando la località Saskatchewan River Crossing, dopo circa 15Km sulla destra si trova “The Weeping Wall”, una parete rocciosa dove scorrono centinaia di cascate che si trasformano in vapore acqueo. Raggiunto l’icefield Centre, prenotarsi per l’escursione sul ghiacciaio con i “snocoach”, degli autobus con ruote giganti che portano fino al cuore del ghiacciaio Athabasca. La visita costa 49CAD$ a testa, dura 1h 30’ e parte circa ogni 15/20 minuti. 17.00 – 18.30 Icefield Centre /Jasper – 104Km – 1h 30’ (senza soste) Percorrere l’ultimo tratto della Icefields Parkway, dopo circa 70Km intercettare uscire dalla statale 93 e prendere al 93-A, strada più panoramica per jasper, poco dopo l’imbocco si possono visitare anche le Athabasca Falls, possibilità di avvistamento animali.
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S Icefield Parkway S Mosquito Creek L Übernachten J Wandern
dies ist der zweithöchste Pass Kanadas, (ohne Service) am Columbia Icefield. Diese über den eine Straße führt. Südlich vom Co- Plätze sind früher bzw. länger geöffnet. lumbia Icefield überquert der Highway den 2.035 Meter hohen Sunwapta Pass. Bevor Leider sind die Abfahrten zu den man von Süden kommend den Sunwapta ! Highlights des Parkway nur spärlich Pass erreicht, geht es über eine weit ausla- beschildert bzw. fehlen. Wir raten daher, dende Kurve "Big Bend", traditionell auch sich an der in der Parkbroschüre vorhan- BIS JASPER CALGARY "Big Hill" genannt, mehrere Kilometer und denen Karte zu orientieren oder die Kar- 425 Höhenmeter nach oben. Nordwärts te mit dem folgenden Link runterzuladen: Fahrende sollten unbedingt oberhalb der l www.albertawow.com/layout_maps/ Kurve auf dem Aussichtspunkt einen kur- Icefields parkway area map.pdf zen Fotostopp einlegen, der Blick zurück ist phänomenal. Absoluter Höhepunkt ist das CALGARY BIS JASPER CALGARY Columbia Icefield, das etwa in der Mitte der Es gibt keine Mobilfunkverbindung Strecke mit seiner gigantischen Gletscher- ! entlang des Parkway und im Winter Unterwegs auf dem Icefield Parkway zunge des Athabasca Glacier Besucher keine Tankmöglichkeit. anlockt. Wer Kosten und Zeit nicht scheut, Bevor Sie ab Lake Louise nach Norden auf- kann sich bequem per Gruppentour auf brechen, ein Tipp: Wenn es Ihr Zeitplan er- S ICEFIELD PARKWAY den Gletscher fahren lassen oder auch eine laubt, warten Sie möglichst auf klares Wet- schwierige (geführte) Gletschertour wagen. S MOSQUITO CREEK ter für die Fahrt über den Icefield Parkway. Der Highway ist ganzjährig geöffnet, Was sich Ihnen landschaftlich bis Jasper Der Icefield Parkway (Highway 93) beginnt Höchstgeschwindigkeit ist 90 km/h.
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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.
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