Summary of the Hudson Bay Marine Ecosystem Overview

Total Page:16

File Type:pdf, Size:1020Kb

Summary of the Hudson Bay Marine Ecosystem Overview i SUMMARY OF THE HUDSON BAY MARINE ECOSYSTEM OVERVIEW by D.B. STEWART and W.L. LOCKHART Arctic Biological Consultants Box 68, St. Norbert P.O. Winnipeg, Manitoba CANADA R3V 1L5 for Canada Department of Fisheries and Oceans Central and Arctic Region, Winnipeg, Manitoba R3T 2N6 Draft March 2004 ii Preface: This report was prepared for Canada Department of Fisheries and Oceans, Central And Arctic Region, Winnipeg. MB. Don Cobb and Steve Newton were the Scientific Authorities. Correct citation: Stewart, D.B., and W.L. Lockhart. 2004. Summary of the Hudson Bay Marine Ecosystem Overview. Prepared by Arctic Biological Consultants, Winnipeg, for Canada Department of Fisheries and Oceans, Winnipeg, MB. Draft vi + 66 p. iii TABLE OF CONTENTS 1.0 INTRODUCTION.........................................................................................................................1 2.0 ECOLOGICAL OVERVIEW.........................................................................................................3 2.1 GEOLOGY .....................................................................................................................4 2.2 CLIMATE........................................................................................................................6 2.3 OCEANOGRAPHY .........................................................................................................8 2.4 PLANTS .......................................................................................................................13 2.5 INVERTEBRATES AND UROCHORDATES.................................................................14 2.6 FISH .............................................................................................................................16 2.7 MAMMALS ...................................................................................................................17 2.8 BIRDS ..........................................................................................................................22 2.9 HUMAN OCCUPATION................................................................................................26 3.0 ECOSYSTEM STRESSORS.....................................................................................................28 3.1 HARVESTING ..............................................................................................................28 3.1.1 Plants and Invertebrates...................................................................................30 3.1.2 Fish..................................................................................................................31 3.1.3 Marine mammals..............................................................................................32 3.2 DEVELOPMENT...........................................................................................................34 3.3 CONTAMINANTS .........................................................................................................37 3.3.1 Synthetic ..........................................................................................................38 3.3.2 Naturally occurring ...........................................................................................40 3.4 CLIMATE CHANGE......................................................................................................43 4.0 CONCLUDING REMARKS........................................................................................................47 5.0 ACKNOWLEDGMENTS............................................................................................................48 6.0 SELECTED REFERENCES ......................................................................................................48 iv LIST OF FIGURES Figure 1. Marine ecoregions in Arctic Canada identified and under discussion by the Department of Fisheries and Oceans from an arctic science planning workshop in 2000........................... 1 Figure 2. Map of Hudson Bay and James Bay......................................................................................... 2 Figure 3. Hudson Bay watershed ............................................................................................................ 3 Figure 4. Geological Provinces and lithology .......................................................................................... 4 Figure 5. Permafrost .............................................................................................................................. 5 Figure 6. Coastal types bordering Hudson Bay and James Bay .............................................................. 5 Figure 7. Relief . ..................................................................................................................................... 6 Figure 8. Bathymetry of Hudson Bay ...................................................................................................... 6 Figure 9. Mean daily air temperature (ºC) . ............................................................................................. 7 Figure 10. Freshwater addtion by ice cover, runoff (A), precipitation (P), and evaporation (E) for Hudson Bay, using a 1.6 m maximum ice-cover thickness..................................................... 7 Figure 11. Terrestrial ecozones and ecoregions bordering Hudson Bay and James Bay.......................... 8 Figure 12. General surface circulation pattern for the summer condition of Hudson Bay and James Bay (Left) (from Prinsenberg 1986a; numbers are observed velocity values in cm •s-1) compared with surface circulation determined from model results (Right) ................. 9 Figure 13. Patterns of sea ice freeze-up (top left) and breakup (bottom left) and frequency and type of late winter (top right) and late summer (bottom right) sea ice, based on 30 years of data.........................................................................................................................10 Figure 14. Representative vertical profiles of temperature and salinity in southeastern Hudson Bay at various times of the year (different years); April 15, 1982 (dashed line), May 16, 1982 (dashed-dotted line), August 15, 1976 (solid line) ..................................................11 Figure 15. Sea ice concentration in the Hudson Bay marine ecosystem during the week of 28 April –2 May 2003.................................................................................................................11 Figure 16. Surface salinity and temperature distribution of Hudson Bay in August-September 1975 .....................................................................................................................................12 Figure 17. Surface salinities in summer (A) and winter (B) in James Bay ...............................................12 Figure 18. Surface chlorophyll a (mg•m-3) distribution in Hudosn Bay, August-September 1975. Station location is base of bar...............................................................................................13 Figure 19. Seasonal variations of diatom counts, primary productivity rates, and ciliate counts at selected depths near the Belcher Islands. .............................................................................13 Figure 21. Distribution or marsh and coast types (A) and fall concentrations of shorebirds and waterfowl (B) on the west coast of James Bay. .....................................................................14 Figure 20. Distribution of eelgrass beds in the James Bay marine region ...............................................14 Figure 22. The life cycles of anadromous: A) lake cisco (Coregonus artedi), and B) lake whitefish (C. clupeaformis) in coastal James Bay..................................................................16 Figure 23. Proportion of fish prey types delivered to thick-billed murre chicks in 1984-87 and 1999-2002 (benthic = sculpins and zoarcids).........................................................................17 Figure 24. Spread of rainbow smelt in the Hudson Bay drainage............................................................17 Figure 25. Information on the spring and fall movements of belugas and areas where they are first seen in the spring, concentrate in summer, and spend the winter compiled from traditional and scientific sources ...........................................................................................18 Figure 26. Map showing the seasonal movements of 5 belugas that were radio-tagged at the Nelson Estuary between 30 July and 5 August 2003 and followed until 27 November 2003 .....................................................................................................................................19 Figure 27. Movements of 41 adult female polar bears through a total of 46 bear years, between 1991 and 1998......................................................................................................................19 Figure 28. Denning habitats, summer retreats, and winter concentration areas of polar bears in the Hudson Bay and James Bay areas..................................................................................20 Figure 29. Use of habitats of the northeast coast of James Bay by ducks...............................................23 Figure 30. Map of Hudson Bay and James Bay showing locations of protected areas. The Cape v Churchill and Cape Tatnam Wildife Management areas in Manitoba are not shown..............25 Figure 31. Sites occupied
Recommended publications
  • An Overview of the Hudson Bay Marine Ecosystem
    5–1 5.0 OCEANOGRAPHY Chapter Contents 5.1 CIRCULATION........................................................................................................................................................5–5 5.2 TIDES......................................................................................................................................................................5–7 5.3 WAVE CLIMATE AND STORM SURGES............................................................................................................5–10 5.4 SEA ICE ................................................................................................................................................................5–10 5.4.1 Terminology.......................................................................................................................................................5–11 5.4.2 Seasonal Changes............................................................................................................................................5–12 5.5 SALINITY, TEMPERATURE, AND MIXING .........................................................................................................5–18 5.5.1 Surface Distributions .........................................................................................................................................5–20 5.5.2 Vertical Profiles .................................................................................................................................................5–22 5.6 WATER CLARITY
    [Show full text]
  • Ramsar Sites in Order of Addition to the Ramsar List of Wetlands of International Importance
    Ramsar sites in order of addition to the Ramsar List of Wetlands of International Importance RS# Country Site Name Desig’n Date 1 Australia Cobourg Peninsula 8-May-74 2 Finland Aspskär 28-May-74 3 Finland Söderskär and Långören 28-May-74 4 Finland Björkör and Lågskär 28-May-74 5 Finland Signilskär 28-May-74 6 Finland Valassaaret and Björkögrunden 28-May-74 7 Finland Krunnit 28-May-74 8 Finland Ruskis 28-May-74 9 Finland Viikki 28-May-74 10 Finland Suomujärvi - Patvinsuo 28-May-74 11 Finland Martimoaapa - Lumiaapa 28-May-74 12 Finland Koitilaiskaira 28-May-74 13 Norway Åkersvika 9-Jul-74 14 Sweden Falsterbo - Foteviken 5-Dec-74 15 Sweden Klingavälsån - Krankesjön 5-Dec-74 16 Sweden Helgeån 5-Dec-74 17 Sweden Ottenby 5-Dec-74 18 Sweden Öland, eastern coastal areas 5-Dec-74 19 Sweden Getterön 5-Dec-74 20 Sweden Store Mosse and Kävsjön 5-Dec-74 21 Sweden Gotland, east coast 5-Dec-74 22 Sweden Hornborgasjön 5-Dec-74 23 Sweden Tåkern 5-Dec-74 24 Sweden Kvismaren 5-Dec-74 25 Sweden Hjälstaviken 5-Dec-74 26 Sweden Ånnsjön 5-Dec-74 27 Sweden Gammelstadsviken 5-Dec-74 28 Sweden Persöfjärden 5-Dec-74 29 Sweden Tärnasjön 5-Dec-74 30 Sweden Tjålmejaure - Laisdalen 5-Dec-74 31 Sweden Laidaure 5-Dec-74 32 Sweden Sjaunja 5-Dec-74 33 Sweden Tavvavuoma 5-Dec-74 34 South Africa De Hoop Vlei 12-Mar-75 35 South Africa Barberspan 12-Mar-75 36 Iran, I. R.
    [Show full text]
  • Evaluation of Special Management Measures for Midcontinent Lesser Snow Geese and Ross’S Geese Report of the Arctic Goose Habitat Working Group
    Evaluation of special management measures for midcontinent lesser snow geese and ross’s geese Report of the Arctic Goose Habitat Working Group A Special Publication of the Arctic Goose Joint Venture of the North American Waterfowl Management Plan Evaluation of special management measures for midcontinent lesser snow geese and ross’s geese Report of the Arctic Goose Habitat Working Group A Special Publication of the Arctic Goose Joint Venture of the North American Waterfowl Management Plan Edited by: James O. Leafloor, Timothy J. Moser, and Bruce D.J. Batt Working Group Members James O. Leafloor Co-Chair Canadian Wildlife Service Timothy J. Moser Co-Chair U.S. Fish and Wildlife Service Bruce D. J. Batt Past Chair Ducks Unlimited, Inc. Kenneth F. Abraham Ontario Ministry of Natural Resources Ray T. Alisauskas Wildlife Research Division, Environment Canada F. Dale Caswell Canadian Wildlife Service Kevin W. Dufour Canadian Wildlife Service Michel H. Gendron Canadian Wildlife Service David A. Graber Missouri Department of Conservation Robert L. Jefferies University of Toronto Michael A. Johnson North Dakota Game and Fish Department Dana K. Kellett Wildlife Research Division, Environment Canada David N. Koons Utah State University Paul I. Padding U.S. Fish and Wildlife Service Eric T. Reed Canadian Wildlife Service Robert F. Rockwell American Museum of Natural History Evaluation of Special Management Measures for Midcontinent Snow Geese and Ross's Geese: Report of the Arctic Goose Habitat Working Group SUGGESTED citations: Abraham, K. F., R. L. Jefferies, R. T. Alisauskas, and R. F. Rockwell. 2012. Northern wetland ecosystems and their response to high densities of lesser snow geese and Ross’s geese.
    [Show full text]
  • Imaging Laurentide Ice Sheet Drainage Into the Deep Sea: Impact on Sediments and Bottom Water
    Imaging Laurentide Ice Sheet Drainage into the Deep Sea: Impact on Sediments and Bottom Water Reinhard Hesse*, Ingo Klaucke, Department of Earth and Planetary Sciences, McGill University, Montreal, Quebec H3A 2A7, Canada William B. F. Ryan, Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY 10964-8000 Margo B. Edwards, Hawaii Institute of Geophysics and Planetology, University of Hawaii, Honolulu, HI 96822 David J. W. Piper, Geological Survey of Canada—Atlantic, Bedford Institute of Oceanography, Dartmouth, Nova Scotia B2Y 4A2, Canada NAMOC Study Group† ABSTRACT the western Atlantic, some 5000 to 6000 State-of-the-art sidescan-sonar imagery provides a bird’s-eye view of the giant km from their source. submarine drainage system of the Northwest Atlantic Mid-Ocean Channel Drainage of the ice sheet involved (NAMOC) in the Labrador Sea and reveals the far-reaching effects of drainage of the repeated collapse of the ice dome over Pleistocene Laurentide Ice Sheet into the deep sea. Two large-scale depositional Hudson Bay, releasing vast numbers of ice- systems resulting from this drainage, one mud dominated and the other sand bergs from the Hudson Strait ice stream in dominated, are juxtaposed. The mud-dominated system is associated with the short time spans. The repeat interval was meandering NAMOC, whereas the sand-dominated one forms a giant submarine on the order of 104 yr. These dramatic ice- braid plain, which onlaps the eastern NAMOC levee. This dichotomy is the result of rafting events, named Heinrich events grain-size separation on an enormous scale, induced by ice-margin sifting off the (Broecker et al., 1992), occurred through- Hudson Strait outlet.
    [Show full text]
  • Established/Outsider Relations in Hérouxville
    Space without scales: established/outsider relations in Hérouxville Tim Nieguth Aurélie Lacassagne Laurentian University Abstract: In 1965, Norbert Elias and John Scotson published a seminal study on the dynamics of established/outsider relations. Their analysis has been criticized on several grounds, including its relative inattention to space. A number of recent studies have sought to build on Elias and Scotson's model by putting greater emphasis on space. These studies represent important interventions in the development of a relational approach to local established/outsider relations. Nonetheless, such an approach would benefit from further refinement. In particular, an Eliasian approach can be especially valuable to the study of local power relations and identity constructions if it takes into account the overlapping nature of configurations, emphasizes that individuals are simultaneously embedded in a large number of configurations, recognizes that different spatial contexts are not merely external resources to be manipulated by (local) actors, and refuses to treat conflicts that happen to play out in local contexts as purely local phenomena. Keywords: Established/outsiders, scale, immigration, national identity, settler societies, urban/rural divide Résumé: En 1965, Norbert Elias et John Scotson ont publié un ouvrage dressant les bases des études sur les logiques d’exclusion. Leur analyse a fait l’objet de plusieurs critiques dont le peu d’attention accordée à la question de l’espace. En s’inspirant des travaux de Norbert Elias et de John Scotson, de nouvelles recherches ont tenté de remédier à la situation en accordant plus d’attention aux enjeux d’espace. Du coup, ces études ont grandement contribué au développement d’une sociologie relationnelle.
    [Show full text]
  • A Historical and Legal Study of Sovereignty in the Canadian North : Terrestrial Sovereignty, 1870–1939
    University of Calgary PRISM: University of Calgary's Digital Repository University of Calgary Press University of Calgary Press Open Access Books 2014 A historical and legal study of sovereignty in the Canadian north : terrestrial sovereignty, 1870–1939 Smith, Gordon W. University of Calgary Press "A historical and legal study of sovereignty in the Canadian north : terrestrial sovereignty, 1870–1939", Gordon W. Smith; edited by P. Whitney Lackenbauer. University of Calgary Press, Calgary, Alberta, 2014 http://hdl.handle.net/1880/50251 book http://creativecommons.org/licenses/by-nc-nd/4.0/ Attribution Non-Commercial No Derivatives 4.0 International Downloaded from PRISM: https://prism.ucalgary.ca A HISTORICAL AND LEGAL STUDY OF SOVEREIGNTY IN THE CANADIAN NORTH: TERRESTRIAL SOVEREIGNTY, 1870–1939 By Gordon W. Smith, Edited by P. Whitney Lackenbauer ISBN 978-1-55238-774-0 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 ucpress@ ucalgary.ca 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 specificwork without breaching the artist’s copyright.
    [Show full text]
  • Assessment of the Vulnerability of Peatland Carbon in the Albany Ecodistrict of the Hudson Bay Lowlands, Ontario, Canada to Climate Change
    Ministry of Natural Resources and Forestry Assessment of the vulnerability Science and Research of peatland carbon in the Albany Ecodistrict of the 46 Hudson Bay Lowlands, Ontario, CLIMATE CHANGE Canada to climate change RESEARCH REPORT CCRR-46 Responding to Climate Change Through Partnership Assessment of the vulnerability of peatland carbon in the Albany Ecodistrict of the Hudson Bay Lowlands, Ontario, Canada to climate change Jim McLaughlin, Maara Packalen, and Bharat Shrestha Forest Research and Monitoring Section Ontario Ministry of Natural Resources and Forestry 2018 Science and Research Branch • Ministry of Natural Resources and Forestry © 2018, Queen’s Printer for Ontario Printed in Ontario, Canada Single copies of this publication are available from [email protected]. Cette publication hautement spécialisée Assessment of the Vulnerability of Peatland Carbon in the Albany Ecodistrict of the Hudson Bay Lowlands, Ontario, Canada to Climate Change n’est disponible qu’en anglais conformément au Règlement 671/92, selon lequel il n’est pas obligatoire de la traduire en vertu de la Loi sur les services en français. Pour obtenir des renseignements en français, veuillez communiquer avec le ministère des Richesses naturelles et des Forêts au [email protected]. Some of the information in this document may not be compatible with assistive technologies. If you need any of the information in an alternate format, please contact [email protected]. Cite this report as: McLaughlin, J., M. Packalen and B. Shrestha. 2018. Assessment of the vulnerability of peatland carbon in the Albany Ecodistrict of the Hudson Bay Lowlands, Ontario, Canada to climate change. Ontario Ministry of Natural Resources and Forestry, Science and Research Branch, Peterborough, ON.
    [Show full text]
  • Carbon Storage and Potential Methane Production in the Hudson Bay Lowlands Since Mid-Holocene Peat Initiation
    ARTICLE Received 28 Aug 2013 | Accepted 9 May 2014 | Published 11 Jun 2014 DOI: 10.1038/ncomms5078 Carbon storage and potential methane production in the Hudson Bay Lowlands since mid-Holocene peat initiation Maara S. Packalen1, Sarah A. Finkelstein2 & James W. McLaughlin3 Peatlands have influenced Holocene carbon (C) cycling by storing atmospheric C and releasing methane (CH4). Yet, our understanding of contributions from the world’s second largest peatland, the Hudson Bay Lowlands (HBL), Canada, to peat-climate-C-dynamics is constrained by the paucity of dated peat records and regional C-data. Here we examine HBL peatland development in relation to Holocene C-dynamics. We show that peat initiation in the HBL is tightly coupled with glacial isostatic adjustment (GIA) through most of the record, and occurred within suitable climatic conditions for peatland development. HBL peatlands initiated most intensively in the mid-Holocene, when GIA was most rapid and climate was cooler and drier. As the peat mass developed, we estimate that the HBL potentially released 1–7 Tg CH4 per year during the late Holocene. Our results indicate that the HBL currently stores a C-pool of B30 Pg C and provide support for a peatland-derived CH4 contribution to the late Holocene atmosphere. 1 Department of Geography, University of Toronto, Toronto, Ontario, Canada M5S 3G3. 2 Department of Earth Sciences, University of Toronto, Toronto, Ontario, Canada M5S 3B1. 3 Ontario Forest Research Institute, Ontario Ministry of Natural Resources, Sault Ste. Marie, Ontario, Canada P6A 2E5. Correspondence and requests for materials should be addressed to M.S.P.
    [Show full text]
  • Arctic Goose Joint Venture STRATEGIC PLAN 2008 – 2012
    Arctic Goose Joint Venture STRATEGIC PLAN 2008 – 2012 Arctic Goose Joint Venture STRATEGIC PLAN 2008 – 2012 Cover Photos (clockwise from top left): Doug Steinke, Doug Steinke, John Conkin, Jeff Coats, Tim Moser, Tim Moser, Doug Steinke Arctic Goose Joint Venture Technical Committee. 2008. Arctic Goose Joint Venture Strategic Plan: 2008 - 2012. Unpubl. Rept. [c/o AGJV Coordination Office, CWS, Edmonton, Alberta]. 112pp. Strategic Plan 2008 – 2012 Table of Contents INtroductioN ................................................................................................................ 7 ACCOMPLISHMENts AND FUTURE CHALLENGES .................................................... 9 Past Accomplishments ....................................................................................................... 9 Banding ...................................................................................................................... 9 Surveys ..................................................................................................................... 10 Research ................................................................................................................... 10 Future Challenges ........................................................................................................... 11 INformatioN NEEDS AND Strategies to ADDRESS THEM ............................ 12 Definitions of Information Needs.................................................................................... 12 Strategies for Meeting the Information
    [Show full text]
  • Hudson Bay Ice Conditions
    Hudson Bay Ice Conditions ERIC W. DANIELSON, JR.l ABSTRACT.Monthly mean ice cover distributions for Hudson Bay have been derived, based upon an analysis of nine years of aerial reconnaissance and other data. Information is presented in map form, along with diseussian Of significant features. Ice break-up is seen to work southward from the western, northern, and eastern edges of the Bay; the pattern seems to be a result of local topography, cur- rents, and persistent winds. Final melting occurs in August. Freeze-up commences in October, along the northwestern shore, and proceeds southeastward. The entire Bay is ice-covered by early January,except for persistent shore leads. RÉSUMÉ. Conditions de la glace dans la mer d’Hudson. A partir de l’analyse de neuf années de reconnaissances aériennes et d’autres données, on a pu déduire des moyennes mensuelles de distribution de la glace pour la mer d’Hudson. L‘informa- tion est présentte sous formes de cartes et de discussion des Cléments significatifs. On y voit que la débâcle progresse vers le sud à partir des marges ouest, nord et est dela mer; cette séquence sembleêtre le résultat de la topographielocale, des courants et .des vents dominants. La fonte se termine en aofit. L’enge€wommence en octobre le long de la rive nord-ouest et progresse vers le sud-est. Sauf pow les chenaux côtiers persistants, la mer est entihrement gelée au début de janvier. INTRODUCTION In many respects, ice cover is a basic hydrometeorological variable. In Hudson Bay (Fig. 1) it might be considered the most basic of all, as it influences all other conditions so decisively.
    [Show full text]
  • “How Frigid Zones Reward the Advent‟Rers Toils”: Natural History Writing and the British Imagination in the Making of Hudson Bay, 1741-1752
    “How frigid Zones reward the Advent‟rers Toils”: Natural History Writing and the British Imagination in the Making of Hudson Bay, 1741-1752 by Nicholas Melchin B.A., Ottawa University, 2005 A Thesis Submitted in Partial Fulfillment of the Requirements for the Degree of MASTER OF ARTS in the Department of History Nicholas Melchin, 2009 University of Victoria All rights reserved. This thesis may not be reproduced in whole or in part, by photocopy or other means, without the permission of the author. Library and Archives Bibliothèque et Canada Archives Canada Published Heritage Direction du Branch Patrimoine de l’édition 395 Wellington Street 395, rue Wellington Ottawa ON K1A 0N4 Ottawa ON K1A 0N4 Canada Canada Your file Votre référence ISBN: 978-0-494-66809-2 Our file Notre référence ISBN: 978-0-494-66809-2 NOTICE: AVIS: The author has granted a non- L’auteur a accordé une licence non exclusive exclusive license allowing Library and permettant à la Bibliothèque et Archives Archives Canada to reproduce, Canada de reproduire, publier, archiver, publish, archive, preserve, conserve, sauvegarder, conserver, transmettre au public communicate to the public by par télécommunication ou par l’Internet, prêter, telecommunication or on the Internet, distribuer et vendre des thèses partout dans le loan, distribute and sell theses monde, à des fins commerciales ou autres, sur worldwide, for commercial or non- support microforme, papier, électronique et/ou commercial purposes, in microform, autres formats. paper, electronic and/or any other formats. The author retains copyright L’auteur conserve la propriété du droit d’auteur ownership and moral rights in this et des droits moraux qui protège cette thèse.
    [Show full text]
  • Massive Water Diversion Schemes in North America: a Solution to Water Scarcity?
    Water Resources Management III 385 Massive water diversion schemes in North America: a solution to water scarcity? F. Lasserre Department of Geography, Laval University, Canada Abstract Massive water diversion projects have been proposed by engineers or public officials in the United States since 1951, but so far, only regional water transfers have been built, often at great cost and questionable economic benefit. Public opinions and governments are still worried in Canada and in the Great Lakes area that these projects could somehow be carried on. However, these massive undertakings prove to be poorly profitable compared to other means of water management, and are not necessary since water withdrawals are stabilizing in the United States, and other demand management techniques are emerging. Keywords: water supply, water diversion, aqueduct, water transfer, irrigation, water conflict, Canada, United States. 1 Massive water transfer projects were once considered Large-scale diversions of Great Lakes and Canada's waters have been discussed for several decades. Various proposals for transferring Canadian or Great Lakes water have emerged since the 1950s, beginning with the United Western Investigation in 1951, an extensive study conducted by the Bureau of Reclamation. The proposals have often been made by engineering corporations because of the obvious possibility to profit from large construction projects. Proposals to import water were also meant to satisfy rapidly growing urban areas like Phoenix and Las Vegas. According to the U.S. Census Bureau, the top five fastest-growing cities in the U.S. from 2000 to 2002 were all in Arizona and Nevada. With this great influx of people to an area with no substantial supply of freshwater, the temptation to look at the large water reserves in northern United States and in Canada was strong.
    [Show full text]