Water Quality Data for the Lower Nelson River System, Manitoba, 2009
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Power from the Nelson
the The plan to develop abundant, clean, self-renewing energy from Manitoba's own great river. MANITOBA HYDRO LONG SPRUCE KETTLE KE LS EY JENPEG MANITOBA'S WATER POWER ln terms of hVdro-electric po' tential, l\lanitoba's greatest water power resources are the Nelson, Churchill. Winn ipeg, and Saskat' chewan River, in that order. The Winnipeg River's 560,000 kilowatts was developed firsr be' cause of its prox im ity to the pro' GRAND RAPIDS vincial population centre. Next came the Saskatchewan and a 472,OOO kW station at Grand Rapids. Now the mighty Nelson and Churchill Rivers are being har- nessed. Together. the Nelson and Churchill can provide a total of a,270,OOO kW of self-renewing hydro power. I DEVE LOPED HYDRO SITE POTENTIAL HY DRO SIIE - The Electrical Province ln a world belatedly becoming aware that fuels such as oil, coal, and natural gas will one day be completely gone, the value of water power is appreciated more and more. Water power is self renewing. When the last ounce of mineral wealth is wrested from the ground, our water resources will be intact and worth more than ever. Manitobans have been enjoying the benefits of low-cost electricity generated from water power since the first all-weather hydro staiion was built on the Winnipeg River system in 1906. The Winnipeg River, only B0 miles away from the major population centre of Winnipeg, served the province's hydraulic generation needs for the next ha lf century. By 1955, with six hydro plants in service along its course,the Winnipeg River was fully developed (560,000 kilowatts) and power planners looked to the more northerly Saskatchewan River for more low cost power. -
The University of Manitoba the Author Reserves Other
TI{E T]VIPACT OF T'ORESTRY PFACTTCES oN MOosE (arces ar,cns) T}] NORTH - CENTRAL IVIANTTOBA by BARBA-RA E. SCATT'E A practícum submitted to the University of Manitoba an partial fulfillment of the requirements of the degree of MASTER OF NATURAL RESOT]RCE MANAGEMENT J drsao Permissi.on has been granted to the LTBRARy oF THE uNrvERsrry OF ì4ANITOBA to Lend or se,ll copies of this practicum, to the NATTONAL LTBRARY oF CANADA to mÍcrofilm this pracricum and to lend or sell copies of the film, and iJNrvERSrry I'frcROFrIìfs to publish an abstract of this practicum. The author reserves other publication rights, and neither the practicum nor extensive extracts from it uray be printed or otherwise reproduced vrithout the authorts r.¡ritten permission. -¡:l:i., i_l i'ì l ? i:: :,1 .,.-\ r.: .' .,; ' v.'j]-! I /-. ¡n r.-,r'lQ ':i ---i;t-- ABSTRÄ,CT The impact of forestry operations on moose (alces alces) in north - central Manitoba was determined through an examination of: (1) browse utilization by moose on forest cutovers, (2) spatial distribution of moose on forest cut- overs, and (3) hunter-kilI of moose in areas of pulpwood and timber extraction- An examination of the literature and the results of the browse and moose distribution surveys showed that forest har- vesting can be used to create moose habitat in Grass River provincial- Park. From these results, a series of guidelines regarding pulpwood and tj-mber extraction ín the study area were developed. The Provincial Park Lands Act provides Parks Branch with the legislation to regulate harvesting of trees in Grass River Provincial Park according to these guidelines. -
Petition to List US Populations of Lake Sturgeon (Acipenser Fulvescens)
Petition to List U.S. Populations of Lake Sturgeon (Acipenser fulvescens) as Endangered or Threatened under the Endangered Species Act May 14, 2018 NOTICE OF PETITION Submitted to U.S. Fish and Wildlife Service on May 14, 2018: Gary Frazer, USFWS Assistant Director, [email protected] Charles Traxler, Assistant Regional Director, Region 3, [email protected] Georgia Parham, Endangered Species, Region 3, [email protected] Mike Oetker, Deputy Regional Director, Region 4, [email protected] Allan Brown, Assistant Regional Director, Region 4, [email protected] Wendi Weber, Regional Director, Region 5, [email protected] Deborah Rocque, Deputy Regional Director, Region 5, [email protected] Noreen Walsh, Regional Director, Region 6, [email protected] Matt Hogan, Deputy Regional Director, Region 6, [email protected] Petitioner Center for Biological Diversity formally requests that the U.S. Fish and Wildlife Service (“USFWS”) list the lake sturgeon (Acipenser fulvescens) in the United States as a threatened species under the federal Endangered Species Act (“ESA”), 16 U.S.C. §§1531-1544. Alternatively, the Center requests that the USFWS define and list distinct population segments of lake sturgeon in the U.S. as threatened or endangered. Lake sturgeon populations in Minnesota, Lake Superior, Missouri River, Ohio River, Arkansas-White River and lower Mississippi River may warrant endangered status. Lake sturgeon populations in Lake Michigan and the upper Mississippi River basin may warrant threatened status. Lake sturgeon in the central and eastern Great Lakes (Lake Huron, Lake Erie, Lake Ontario and the St. Lawrence River basin) seem to be part of a larger population that is more widespread. -
Large Area Planning in the Nelson-Churchill River Basin (NCRB): Laying a Foundation in Northern Manitoba
Large Area Planning in the Nelson-Churchill River Basin (NCRB): Laying a foundation in northern Manitoba Karla Zubrycki Dimple Roy Hisham Osman Kimberly Lewtas Geoffrey Gunn Richard Grosshans © 2014 The International Institute for Sustainable Development © 2016 International Institute for Sustainable Development | IISD.org November 2016 Large Area Planning in the Nelson-Churchill River Basin (NCRB): Laying a foundation in northern Manitoba © 2016 International Institute for Sustainable Development Published by the International Institute for Sustainable Development International Institute for Sustainable Development The International Institute for Sustainable Development (IISD) is one Head Office of the world’s leading centres of research and innovation. The Institute provides practical solutions to the growing challenges and opportunities of 111 Lombard Avenue, Suite 325 integrating environmental and social priorities with economic development. Winnipeg, Manitoba We report on international negotiations and share knowledge gained Canada R3B 0T4 through collaborative projects, resulting in more rigorous research, stronger global networks, and better engagement among researchers, citizens, Tel: +1 (204) 958-7700 businesses and policy-makers. Website: www.iisd.org Twitter: @IISD_news IISD is registered as a charitable organization in Canada and has 501(c)(3) status in the United States. IISD receives core operating support from the Government of Canada, provided through the International Development Research Centre (IDRC) and from the Province -
Keeyask Generation Project: Aquatic Environment Supporting Volume
Keeyask Generation Project Environmental Impact Statement Supporting Volume Aquatic Environment June 2012 Morgan Bay100°W 95°W 90°W 60°N HUDSON Hudson Bay Settee Lake !( BAY Churchill ± Port Nelson Wei York !( r R Factory 55°N Thompson iver 55°N Deer Gillam Okaw Creek Island Island ER IV R N O S L E N 100°W 95°W 90°W Weir River Goose C Potential re e Conawapa G.S. k ÕÚ Lime Swift stone Riv er Creek VER Angling River RI S ! ÕÚ Limestone Fox Lake Cree Nation YE STEPHENS Fox Lake (Bird) G.S. Angling HA Kettle Lake ¾ÀPR 280 G.S. Proposed LAKE ÕÚ Keeyask G.S. ÕÚ Longspruce Clark ÕÚ Gillam! G.S. Fox Lake Cree Nation Lake NELSON RIVER A Kwis Ki Mahka Reserve Gull Lake ! Tataskweyak Cree Nation Tataskweyak (Split Lake) Assean Lake Burntwood River sonRiverEstuary_20120520.mxd SPLIT LAKE York Factory First Nation ! York Landing (Kawechiwasik) Kelsey G.S. Aiken River ! ÕÚ War Lake First Nation Ilford Fox River NELSON RIVER 0 25 50 Kilometres Projection: UTM Zone 15, NAD 83 Data Source: NTS base 1:500 000 Kelsey Generating Station to Nelson River Estuary 01020Miles File Location: G:\EIS\Keeyask\Publish_MXDs\SUPPORTING_VOLUME\REVISED_StillOldTemplate\Intro\AESV_1_KelseyGeneratingStationToNel Map 1-1 ke a L a ak w Mosw aio ak Wask ot rth o R N akot i v R osw er iver M h Sout 100°W 95°W 90°W 60°N Hudson Bay !( Churchill ± !( Thompson 55°N STEPHENS LAKE AREA 55°N S T E P Ferris H Bay 100°W 95°W 90°W E N S !( PR 280 ¾À LAKE Kettle G.S.ÚÕ Proposed KEEYASK AREA Keeyask G.S. -
Weekly Update #7 – February 21, 2020
Water Level & Flow Update for the Lower Nelson River Weekly Update # 7 February 21, 2020 Lower Nelson River (Split Lake to Hudson Bay) Water up and impoundment has not started at Keeyask (planned to begin in February). Flows on the Nelson River are high as heavy Fall rainfall in the southern parts of the watershed flows north on its way to Hudson Bay - this will continue all winter. Hydro system flows to Split Lake and the Lower Nelson River come from 2 sources – Lake Winnipeg (LW) outflows through Kelsey generating station (at 3115 cms or 110,000 cfs) and Churchill River Diversion (CRD), through Notigi control structure (960 cms or 33,900 cfs)-see map. These combined flows (of 4,075 cms or 143,900 cfs) have been relatively constant since early December. The Nelson’s flow downstream of Keeyask is 4,480 cms ( or 158,200 cfs) (measured at As of February 19, Lower Nelson River lake and Limestone GS). forebay levels are: • Split Lake 168.35 m (or 552.3 ft) Nelson River flow depends on Lake Winnipeg Water level: • Clark Lake 167.94 m (or 551.0 ft ) Lake Winnipeg outflows are largely controlled by the • Gull Lake 156.17 m (or 512.4 ft ) Jenpeg Generating Station (upstream of Kelsey Jenpeg• Stephens Lake 139.76 m (or 458.5 ft) Generating Station). These flows are maximized every • Long Spruce forebay 110.90 m (or 361.2 ft ) winter to allow as much water as possible to flow out of • Limestone forebay 85.07 m (or 279.1 ft) Lake Winnipeg to fuel generating stations on the Nelson River to meet heating demands by Manitobans. -
Appendix 4.3C
REGIONAL CUMULATIVE EFFECTS ASSESSMENT – PHASE II PHYSICAL ENVIRONMENT – WATER REGIME – APPENDIX 4.3C APPENDIX 4.3C: AN ASSESSMENT OF THE HYDRAULIC IMPACTS OF THE CHURCHILL RIVER DIVERSION ON THE RAT AND BURNTWOOD RIVERS ____ ANASSESSMENT OF THE HYDRAULIC IMPACTS Of THE CHURCHILL RIVER DIVERSION ON THE RA TAND BURNTWOOD RIVERS WaterResources EngineerIng PowerPlanning DivisIon PREPARED BY J. CRAwFORD, RENG. \Ak(Rk---’ CHECKED BY J. MALENCHAK, PH.D. P.ENG. J. WEsTMAc0TT, M.Sc. P. CHANEL, M.Sc. PENG. / P. RASMUSSEN, PH.D. P.ENG. ? CONSULTANT APPRovED BY E,TEKLEMARIAM, M.Sc. RENG. NOTED BY T.MILES, M.Sc. RENG. — i)iC DATE: NOVEMBER 6,2015 REPORT: PPD-1 5/10 1kManitoba Hydro 2 EXECUTIVE SUMMARY 1. The following is a report on simulated water levels and river flows for the Rat and Burntwood Rivers without the Churchill River Diversion. Simulated water levels and river flows are required to estimate the hydraulic impacts of the Churchill River Diversion for Regional Cumulative Effects Assessment and for other purposes including for operations and resource planning. 2. A hydraulic model was developed to simulate hydraulic conditions on the Rat and Burntwood River systems without the Churchill River Diversion. Model results were then compared against actual measured values to quantify the impacts of the Churchill River Diversion and verify the model was working correctly. Overall model performance results were good which confirmed the model is representative of conditions without the Churchill River Diversion. The following conclusion can be made from the model results: The Churchill River Diversion has impacted the Rat and Burntwood River systems. -
Document Control
~ ~ ""!1 fl ,_, "-""! ~ r'"' G""' o·~~ Ht1='\\l~~~~-t=-~, :~i~:.; Susitna Joint Venture Document Number 87;;.._____ _ PJeaso Return To DOCUMENT CONTROL The Destruction of ~·1anito1)il: ..,; Last Great Riv~.:r by: R. Xewbury & G. ~alaher '···"·· i: . .• ., tts;.,__... m ·ir'Cr a· •z ... NOTICE: This M~t~ri~ may be protected by copyright iaw (TitJa 17 U.S. Code)~ The Destruction of .I! i: i ~ -1 f Manitoba's Last·Great River .': ! ..I _i by R. NEWBURY and G. W. MALAHER ... water is an integral part aj the land, responsible to a large extent for its physical form and the life found in or near it - including man. The land and water are indivisible, and those who would treat a river as so much plumbing to be manipulated, and its water as a commodity to be bought and sold like carloads of wheat, have simply not comprehended this fundamental fact. Richard C. Backing -• I' Two great rivers, the Nelson and the Churchill, cut com in midsummer when normal high water would overtop the I I pletely through the Precambrian Shield of northern Mani proposed Missi Falls dam. The stopped-up waters of thf I' I! toba bringing water from the interior of Canada to Hudson Churchili would head southward through Notigi and Spli1 i ' l' Bay. \Vaters flowing to the Nelson begin their journey on Lakes toward the Nelson River some 200 miles to the south : the eastern slope of the Rockies, crossing the three Prairie The reservoir would raise lake levels from ten feet or ._,. J i' Provinces via the Saskatchewan River. -
Convergent Margin Magmatism in the Central Andes and Its Near Antipodes in Western Indonesia: Spatiotemporal and Geochemical Considerations
AN ABSTRACT OF THE DISSERTATION OF Morgan J. Salisbury for the degree of Doctor of Philosophy in Geology presented on June 3, 2011. Title: Convergent Margin Magmatism in the Central Andes and its Near Antipodes in Western Indonesia: Spatiotemporal and Geochemical Considerations Abstract approved: ________________________________________________________________________ Adam J.R. Kent This dissertation combines volcanological research of three convergent continental margins. Chapters 1 and 5 are general introductions and conclusions, respectively. Chapter 2 examines the spatiotemporal development of the Altiplano-Puna volcanic complex in the Lípez region of southwest Bolivia, a locus of a major Neogene ignimbrite flare- up, yet the least studied portion of the Altiplano-Puna volcanic complex of the Central Andes. New mapping and laser-fusion 40Ar/39Ar dating of sanidine and biotite from 56 locations, coupled with paleomagnetic data, refine the timing and volumes of ignimbrite emplacement in Bolivia and northern Chile to reveal that monotonous intermediate volcanism was prodigious and episodic throughout the complex. 40Ar/39Ar age determinations of 13 ignimbrites from northern Chile previously dated by the K-Ar method improve the overall temporal resolution of Altiplano-Puna volcanic complex development. Together with new and updated volume estimates, the new age determinations demonstrate a distinct onset of Altiplano-Puna volcanic complex ignimbrite volcanism with modest output rates beginning ~11 Ma, an episodic middle phase with the highest eruption rates between 8 and 3 Ma, followed by a general decline in volcanic output. The cyclic nature of individual caldera complexes and the spatiotemporal pattern of the volcanic field as a whole are consistent with both incremental construction of plutons as well as a composite Cordilleran batholith. -
A Freshwater Classification of the Mackenzie River Basin
A Freshwater Classification of the Mackenzie River Basin Mike Palmer, Jonathan Higgins and Evelyn Gah Abstract The NWT Protected Areas Strategy (NWT-PAS) aims to protect special natural and cultural areas and core representative areas within each ecoregion of the NWT to help protect the NWT’s biodiversity and cultural landscapes. To date the NWT-PAS has focused its efforts primarily on terrestrial biodiversity, and has identified areas, which capture only limited aspects of freshwater biodiversity and the ecological processes necessary to sustain it. However, freshwater is a critical ecological component and physical force in the NWT. To evaluate to what extent freshwater biodiversity is represented within protected areas, the NWT-PAS Science Team completed a spatially comprehensive freshwater classification to represent broad ecological and environmental patterns. In conservation science, the underlying idea of using ecosystems, often referred to as the coarse-filter, is that by protecting the environmental features and patterns that are representative of a region, most species and natural communities, and the ecological processes that support them, will also be protected. In areas such as the NWT where species data are sparse, the coarse-filter approach is the primary tool for representing biodiversity in regional conservation planning. The classification includes the Mackenzie River Basin and several watersheds in the adjacent Queen Elizabeth drainage basin so as to cover the ecoregions identified in the NWT-PAS Mackenzie Valley Five-Year Action Plan (NWT PAS Secretariat 2003). The approach taken is a simplified version of the hierarchical classification methods outlined by Higgins and others (2005) by using abiotic attributes to characterize the dominant regional environmental patterns that influence freshwater ecosystem characteristics, and their ecological patterns and processes. -
MANITOBA HYDRO-ELECTRIC BOARD, (Hereinafter Called “Hydro”)
AGREEMENT IN PRINCIPLE BETWEEN: NISICHAWAYASIHK CREE NATION, (hereinafter called “NCN”) OF THE FIRST PART, - and - THE MANITOBA HYDRO-ELECTRIC BOARD, (hereinafter called “Hydro”) OF THE SECOND PART. WHEREAS: 1. NCN is a Cree Nation which carried on, and continues to carry on, activities within its traditional and Treaty 5 areas. NCN’s vision statement is: “To exercise sovereignty that sustains a prosperous socio-economic future for the Nisichawayasihk Cree Nation”. 2. There are about 4,500 Members, approximately 2,300 of whom live on Reserve Lands located at Nelson House, upstream of Taskinigup Falls and Wuskwatim Lake and downstream of the Notigi Control Structure. 3. Neither the AIP nor any other arrangements entered into between the Parties will alter or amend treaty or aboriginal rights recognized and affirmed by s. 35 of the Constitution Act, 1982, including any inherent rights of self government of NCN and its Members. 4. Hydro is a Crown Corporation that was established in 1949, and which is continued by The Manitoba Hydro Act, RSM 1987, c. H190, as amended from time to time, for the purposes of providing a continuing supply of power adequate for the needs of the Province of Manitoba; providing and marketing products, services and expertise related to the development, generation, transmission, distribution, supply and end-use of power within and outside of the Province; and marketing and supplying power to persons and other entities outside the Province. -5- 5. In the late 1960's Manitoba and Canada determined that it would be in the Provincial and National interest to expand the planning and development of hydro-electric generating facilities in northern Manitoba. -
Manitoba's Last ·Great River By
-- t . FEDERAL 'ENERGY REGULATORY COMMISSION WASHINGTON, D.C. 20416 ·' ,' OGC Project No. 7114 Alaska Power Authority Jane Drennan, Esquire Pillsbury, Madison & Sutro Suite 900 1050 Seventeenth Street, N.Wv Wash1nQton, D.C. 20036 Dear Ms. Drennanz Please provide Staff with the following information by D~cember 5, 1983: 1) Raw data (disch~rge vs. percent exceedance Yalues) used to plot the flow duration curves in Exhibit E. These curves, for the Cantwell, Gold Creek, Sunshine, an~ Susitna Station gaQing stations, were found in • Chapter 2, Exhibit E~ 2) Sediment transport and bedload data collected by the USGS in CY 1982. , 3) A complete copy of the December 1981 R&M report entitled "Hydrology, Lower Susitna StudiesM. 4) Copies of the reports ~ntitled, •Alaska Department of Fish and Game Sueitna Hydro studies Final Data Report~ and Synopsisa. These reports include 1982 and 1983 5tudies. 5) A copy of the Braalay Lake Instream Flu~ Assessment being prepared by Jean Baldrige for Woodward-Clyde and th~ APA. 6) Preliminary result~ of the habitat preference criteria etudy now in progress. 7) Results of any new HEC-2 calibration studies, and the data input, to upgrade water aurf&ee elevation predictions in the main channel, including new channel cross sections, and water •urface elevations. ~ •..' ' Documentation for the SNTEMP lftodel that haa been ". proposed by AEIDC t.o simula.te downstream vater t•mper&ture regimes. r 'i '· ' . ' ------- .•·" -2- 9) A complete copy of Table 6.10 from Volume 2 of the Chakachamna Hydroelectric Project Inte~im Feasibility Assessment Report, March 1983. 10) A report on nitrocen supersaturation due to temperature differences at the Cultus Lake facility in British Columbia.