Spring Runoff Advisory

Total Page：16

File Type：pdf, Size：1020Kb

Spring Runoff Advisory Issued at:11:30 AM, April 28, 2003 Issued by: River Forecast Centre Spring Runoff Advisory for South and Central Alberta A Spring Runoff Advisory has been issued for small streams, creeks and rivers originating in foothills and plains regions of the Bow, Red Deer and North Saskatchewan basins, and the northern part of the Oldman basin. The region is between Edmonton and Calgary west of Highway 36 and between Calgary and Fort Macleod, west of Highway 2. Over the weekend, up to 150 mm of precipitation fell in these regions, with the heaviest precipitation falling west of Highway 2. Although much of this fell as snow, the early stages of the storm were marked by rainfall, which wetted the soils, increasing runoff production when the snow melts. With a return to warmer temperatures forecast for the rest of this week, runoff from the snowmelt will cause increases in streamflows and there is potential that some streams in these areas may experience high water levels. No major flooding is expected. However, localized flooding in some low-lying areas is likely as meltwater makes its way into the drainage system. A Spring Runoff Advisory means that stream levels are rising or expected to rise due to snowmelt and no major flooding is expected. Minor flooding in low-lying areas is possible. Anyone situated close to the streams affected (property owners and the general public) is advised to be cautious of the rising levels. The High Streamflow Advisory remains in effect for the following streams and their tributaries: In the North Saskatchewan River Basin: · Ram River · Clearwater River In the Red Deer River Basin: · Red Deer River · James River In the Bow River Basin: · Highwood River · Sheep River · Elbow River · Kananaskis River Although these streams have peaked in response to the rainfall over the weekend, they will be experiencing additional rises due to melt of the snow which fell in the same event. Alberta Environment is monitoring river levels closely for streams throughout Alberta. This advisory will be updated if the situation changes. Media Contact: Communications Division, Alberta Environment Phone: (780) 427-6267 Pager: (780) 671-0549 (24 hours) Fax: (780) 427-1874 .

Copy Link

Recommended publications

NYU Radiology CME in Banff MONDAY, August 3 TUESDAY
NYU Radiology CME in Banff OPTIONAL ACTIVITIES The activities below have been arranged by TPI on an exclusive basis for NYU attendees so as not to conflict with the meeting agenda. *TPI reserves the right to cancel or re-price any tours that do not meet the minimum requirements. MONDAY, August 3 Welcome to Banff Sightseeing Tour – 1:30 to 6:30pm Adult -- $105Child (6-15) -- $87 Children under 6 – Free Feel the power of Bow Falls and the beauty that surrounds it just below Banff Springs Hotel. Continue exploring from some of the best views in town – Surprise Corner on Tunnel Mountain Drive, the Hoodoos (oddly shaped pillars of glacial rock), Mount Norquay’s winding road and Sulphur Mountain’s Peak. Take the gondola up to the 7,500 ft. summit of Sulphur Mountain and enjoy the panoramic view of the entire Bow Valley. Free time for refreshments in the restaurant or to explore the many trails that wind atop the mountain. Includes: round trip transportation aboard deluxe motorcoach, escort, gondola ride, admission fees, tax, and driver gratuity. Minimum 20 persons. TUESDAY, August 4 Kananaskis River Whitewater Rafting 1:30 to 6:30pm Adult -- $154; Child (5-15) -- $139 Enjoy the perfect mix of mountains, scenery, fun and a little action on an exciting whitewater paddle raft adventure on the scenic Kananaskis River. The river tour is rated a Grade 2 to 3. Once suited up in full rafting gear, begin a scenic float that gradually builds into an unforgettable whitewater thrill! A skilled rafting guide will ensure your safety and amusement.
[Show full text]
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.
[Show full text]
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.
[Show full text]
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).
[Show full text]
Ca 1978 ISSS Tours 8+16E Report.Pdf
11th CONGRESS I NT ERNA TI ONAL I OF SOIL SCIENCE EDMONTON, CANADA JUNE 1978 GUIDEBOOK FOR A SOILS LAND USE TOUR IN BANFF AND JASPER NATIONAL PARKS TOURS 8 AND 16 L.J. KNAPIK Soils Division, Al Research Council, Edmonton G.M. COEN Research Branch, culture Canada, Edmonton Alberta Research Council Contribution Series 809 ture Canada Soil Research Institute tribution 654 Guidebook itors D.F. Acton and L.S. Crosson Saskatchewan Institute of Pedology Saskatoon, Saskatchewan ~-"-J'~',r--- --\' "' ~\>(\ '<:-q, ,v ~ *'I> co'"' ~ (/) ~ AlBERTA \._____ ) / ~or th '(<.\ ~ e r ...... e1Bowden QJ' - Q"' Olds• Y.T. I N.W.T. _...,_.. ' h./? 1 ...._~ ~ll"O"W I ,-,- B.C. / U.S.A. ' '-----"'/' FIG. 1 GENERAL ROUTE MAP i; i TABLE OF CONTENTS Page ACKNOWLEDGEMENTS ...............•..................................... vi INTRODUCTION ........................................................ 1 GENERAL ITINERARY ................................................... 2 REGIONAL OVERVIEW ..•................................................. 6 The Alberta Plain .................................................. 6 15 The Rocky Mountain Foothills ........................................ The Rocky Mountains ................................................ 17 DAY 1: EDMONTON TO BANFF . • . 27 Road Log No. 1: Edmonton to Calgary.......................... 27 The Lacombe Research Station................................. 32 Road Log No. 2: Calgary to Banff............................ 38 Kananaskis Site: Orthic Eutric Brunisol.... .. ...... ... ....... 41 DAY 2: BANFF AND
[Show full text]
Canadian Rockies
TOP ADVENTURE DESTINATIONS: Canadian Rockies Are your student game for a breathtaking hike to the Takakkaw Falls, spot wildlife in Jasper, or take in stunning views with a trip up a Banff Gondola? If your students are ready to kayak on Moraine Lake, hike Lake O’Hara, and then relax in the Banff Upper Hot Springs, Educational Destinations can make your Canadian Rockies adventure trip rewarding and memorable. ADVENTURE OPPORTUNITIES: • View the highest peak in the Rocky Mountains • Take a Gondola Ride to Sulphur Mountain • Dare to Step Out on the Columbia Icefield Skywalk, a in the heart of the Canadian Rockies Glass-Floor Observation Deck Overlooking Sunwapta • Experience a Mind-Blowing Helicopter Ride Valley and a Walk to Twin Falls • Enjoy a Safari tour through teh River in Grizzly Bear • Take a Soak in the Popular Lussier Hot Springs Valley • Summit A Mountain Right In The Town Of Banff • Travel on a Gigantic Ice Explorer to a location where • Journey Through Johnston Canyon and See the Students can Walk on the Athabasca Glacier Waterfalls, Bridges, and Blue ‘Ink Pot’ Spring Pools • Experience a Tour by Horseback along the Bow River • See Iconic Wildlife on a Wagon Ride at the • Explore the Life of the Active Athabasca Glacier Boundary Ranch • Take a Tranquil Canoe Excursion on Pyramid Lake • Challenge the Rapids of the Kananaskis River • Visit Spirit Island...which is not an Island...Most of the • Experience Thrilling Treetop Adventures Time • Zipline Through Picturesque Landscapes • View the Blue Emerald Waters of Alpine • Explore
[Show full text]
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.
[Show full text]
Management of a River Recreation Resource: Understanding the Inputs To
Management of a River Recreation Resource: Understanding the Inputs to Management of Outdoor Recreational Resources by Kimberley Rae A thesis presented to the University of Waterloo in fulfillment of the thesis requirements for the degree of Master of Arts in Recreation and Leisure Studies Waterloo, Ontario, Canada, 2007 © Kimberley Rae, 2007 AUTHOR’S DECLARATION I hereby declare that I am the sole author of this thesis. This is a true copy of the thesis, including any final revisions, as accepted by my examiners. I understand that a copy of my thesis may be made available electronically to the public. ii Abstract Research into the use of natural resources and protected areas for the pursuit of outdoor recreational opportunities has been examined by a number of researchers. One activity with growth in recent years is river recreation, the use of rivers for rafting, kayaking, canoeing and instructional purposes. These many uses involve different groups of individuals, creating management complexity. Understanding the various inputs is critical for effective management The Lower Kananaskis River, located in Kananaskis Country in Southwestern Alberta, was area chosen to develop an understanding the inputs necessary for effective management. Specifically, this study explored the recreational use of the river in an effort to create recommendations on how to more effectively manage use of the Lower Kananaskis River and associated day-use facilities in the future. Kananaskis Country is a 4,250 km2 multi-use recreation area located in the Canadian Rocky Mountains on the western border of Alberta. Since its designation, the purpose of the area, has been to protect the natural features of the area while providing quality facilities that would complement recreational opportunities available in the area.
[Show full text]
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.
[Show full text]
Movement and Summer Habitat of Brown Trout (Salmo Trutta) Below a Pulsed Discharge Hydroelectric Generating Station
REGULATED RIVERS: RESEARCH & MANAGEMENT Regul. Ri6ers: Res. Mgmt. 15: 395–403 (1999) MOVEMENT AND SUMMER HABITAT OF BROWN TROUT (SALMO TRUTTA) BELOW A PULSED DISCHARGE HYDROELECTRIC GENERATING STATION CHRISTOPHER M. BUNTa,*, STEVEN J. COOKEa, C. KATOPODISb AND R. SCOTT McKINLEYa a Waterloo Biotelemetry Institute, Department of Biology, Uni6ersity of Waterloo, Waterloo, Ontario, Canada, N2L 3G1 b Department of Fisheries and Oceans, Freshwater Institute, 501 Uni6ersity Crescent, Winnipeg, Manitoba, Canada, R3T 2N6 ABSTRACT Radiotelemetry was used to investigate detailed movement and summer habitat of brown trout Salmo trutta (size range 157–488 mm TL, n=18) in the Kananaskis River, Alberta. Flows in the Kananaskis River respond to pulsed daily discharge from an upstream hydroelectric generating facility (range 0.15–25 m3 s−1). Wetted area available for brown trout doubled during periods of high flow. Fluctuating river levels did not appear to influence the degree to which brown trout moved within the study site. However, there was evidence that brown trout used cover and pools more as discharge increased. During high flow conditions, brown trout used similar depths (63 cm), and significantly lower surface water velocities than during low flow conditions. Brown trout also moved closer to shore into interstitial spaces among woody debris and root complexes during high flow. Pool habitats were used most often compared with all other habitat types combined. Pools with large woody debris accounted for 75% of all habitat observations. Woody debris was used more often than all other cover types. Results of the study indicate that the effects of river regulation on brown trout appear to have been moderated by woody debris in pools and along river banks, which provided refuge from high water velocities during periods of high flow.
[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]
050623 1115 Flood Warning for Southern Alberta Noncore
Flood Warning Update Issued at: 11:15 AM, June 23, 2005 Issued by: River Forecast Centre, Flow Forecasting Flood Warning Update A Flood Warning remains in effect for the following streams and rivers and their tributaries in the Red Deer River basin: · Red Deer River downstream of Dickson Dam The Red Deer River peaked at Drumheller at about 1400 m3/s (a rise of 3.9 metres) on June 21 and the river level has since fallen by 2 metres. The Red Deer River at the Alberta/Saskatchewan border has started to peak this morning at a flow of 1040 m3/s with a total rise of about 1.3 metres. Flood Watch Update A Flood Warning has been downgraded to a Flood Watch for the following streams and their tributaries in the North Saskatchewan River and Red Deer River basins: · North Saskatchewan River downstream of the City of Edmonton including the Alberta/Saskatchewan border · Red Deer River upstream of Dickson Dam · Little Red Deer River The North Saskatchewan River at Edmonton peaked at a flow near 2600 m3/s (a rise of 4.4 metres) on June 21 and the river level has since fallen by 3 metres. The North Saskatchewan River at the Alberta/Saskatchewan border peaked at 7 pm yesterday (June 22) at a flow of 2770 m3/s with a total rise of 2.5 metres. Alberta Environment is monitoring water levels of these rivers very closely. A Flood Watch remains in effect for the following streams and rivers and their tributaries in the Bow River and North Saskatchewan River basins: · Bow River (including the City of Calgary) · Nordegg, Ram, Clearwater Rivers and tributaries of the North Saskatchewan River upstream of Lodgepole.
[Show full text]