Vegetation Mapping in the Kivalliq Using Digital Landsat Tm 5/7 Data
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Taltheilei Houses, Lithics, and Mobility
University of Calgary PRISM: University of Calgary's Digital Repository Graduate Studies The Vault: Electronic Theses and Dissertations 2012-09-06 Taltheilei houses, lithics, and mobility Pickering, Sean Joseph Pickering, S. J. (2012). Taltheilei houses, lithics, and mobility (Unpublished master's thesis). University of Calgary, Calgary, AB. doi:10.11575/PRISM/27975 http://hdl.handle.net/11023/177 master thesis University of Calgary graduate students retain copyright ownership and moral rights for their thesis. You may use this material in any way that is permitted by the Copyright Act or through licensing that has been assigned to the document. For uses that are not allowable under copyright legislation or licensing, you are required to seek permission. Downloaded from PRISM: https://prism.ucalgary.ca UNIVERSITY OF CALGARY Taltheilei Houses, Lithics, and Mobility by Sean J. Pickering A THESIS SUBMITTED TO THE FACULTY OF GRADUATE STUDIES IN PARTIAL FULFILMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF ARTS DEPARTMENT OF ARCHAEOLOGY CALGARY, ALBERTA SEPTEMBER, 2012 © Sean J. Pickering 2012 Abstract The precontact subsistence-settlement strategy of Taltheilei tradition groups has been interpreted by past researchers as representing a high residential mobility forager system characterized by ephemeral warm season use of the Barrenlands environment, while hunting barrenground caribou. However, the excavation of four semi-subterranean house pits at the Ikirahak site (JjKs-7), in the Southern Kivalliq District of Nunavut, has challenged these assumptions. An analysis of the domestic architecture, as well as the morphological and spatial attributes of the excavated lithic artifacts, has shown that some Taltheilei groups inhabited the Barrenlands environment during the cold season for extended periods of time likely subsisting on stored resources. -
Recent Declines in Warming and Vegetation Greening Trends Over Pan-Arctic Tundra
Remote Sens. 2013, 5, 4229-4254; doi:10.3390/rs5094229 OPEN ACCESS Remote Sensing ISSN 2072-4292 www.mdpi.com/journal/remotesensing Article Recent Declines in Warming and Vegetation Greening Trends over Pan-Arctic Tundra Uma S. Bhatt 1,*, Donald A. Walker 2, Martha K. Raynolds 2, Peter A. Bieniek 1,3, Howard E. Epstein 4, Josefino C. Comiso 5, Jorge E. Pinzon 6, Compton J. Tucker 6 and Igor V. Polyakov 3 1 Geophysical Institute, Department of Atmospheric Sciences, College of Natural Science and Mathematics, University of Alaska Fairbanks, 903 Koyukuk Dr., Fairbanks, AK 99775, USA; E-Mail: [email protected] 2 Institute of Arctic Biology, Department of Biology and Wildlife, College of Natural Science and Mathematics, University of Alaska, Fairbanks, P.O. Box 757000, Fairbanks, AK 99775, USA; E-Mails: [email protected] (D.A.W.); [email protected] (M.K.R.) 3 International Arctic Research Center, Department of Atmospheric Sciences, College of Natural Science and Mathematics, 930 Koyukuk Dr., Fairbanks, AK 99775, USA; E-Mail: [email protected] 4 Department of Environmental Sciences, University of Virginia, 291 McCormick Rd., Charlottesville, VA 22904, USA; E-Mail: [email protected] 5 Cryospheric Sciences Branch, NASA Goddard Space Flight Center, Code 614.1, Greenbelt, MD 20771, USA; E-Mail: [email protected] 6 Biospheric Science Branch, NASA Goddard Space Flight Center, Code 614.1, Greenbelt, MD 20771, USA; E-Mails: [email protected] (J.E.P.); [email protected] (C.J.T.) * Author to whom correspondence should be addressed; E-Mail: [email protected]; Tel.: +1-907-474-2662; Fax: +1-907-474-2473. -
Statutory Report on Wildlife to the Nunavut Legislative Assembly Section 176 of the Wildlife Act
Statutory Report on Wildlife to the Nunavut Legislative Assembly Section 176 of the Wildlife Act 1.0 Review of Wildlife and Habitat Management Programs for Terrestrial Species in Nunavut…………………………………………………………….1 1.1 Wildlife Act and Wildlife Regulations………………………………………………..2 1.2 Qikiqtaaluk Region……………………………………………………………………2 1.2.1 Qikiqtaaluk Research Initiatives…………………………………………………….2 a. Peary caribou………………………………………………………………………….2 b. High Arctic muskox…………………………………………………………………...3 c. North Baffin caribou…………………………………………………………………..4 1.2.2 Qikiqtaaluk Management Initiatives………………………………………………...5 a. Peary Caribou Management Plan……………………………………………………...5 b. High Arctic Muskox…………………………………………………………………..5 c. South Baffin Management Plan……………………………………………………….6 1.3 Kitikmeot Region……………………………………………………………………...8 1.3.1 Kitikmeot Research Initiatives………………………………………………………9 a. Wolverine and Grizzly bear Hair Snagging………………………………………….. 9 b. Mainland Caribou Projects……………………………………………………………9 c. Boothia Caribou Project……………………………………………………………...10 d. Dolphin and Union Caribou Project……………………............................................10 e. Mainland and Boothia Peninsula Muskoxen………………………………………...11 f. Harvest and Ecological Research Operational System (HEROS)…………………...12 g. Vegetation Mapping……………………………………………………………….....12 1.3.2 Kitikmeot Management Initiatives…………………………………………………12 a. Grizzly Bear Management…………………………………………………………...12 b. Bluenose East Management Plan…………………………………………………….12 c. DU Caribou Management Plan………………………………………………………13 d. Muskox Status -
Geophysical and Geological Integration and Interpretation of the Northeast Thelon Basin, Nunavut
GEOPHYSICAL INTERPRETATION OF THE NORTHEAST THELON BASIN GEOPHYSICAL AND GEOLOGICAL INTEGRATION AND INTERPRETATION OF THE NORTHEAST THELON BASIN, NUNAVUT By VICTORIA LYNN TSCHIRHART, B.Sc. A Thesis Submitted to the School of Graduate Studies in Partial Fulfillment of the Requirements for the Degree of Doctorate of Philosophy McMaster University © Copyright for Victoria Tschirhart, November 2013 i McMaster University DOCTORATE OF PHILOSPHY (2013) Hamilton, Ontario TITLE: Geophysical and geological integration and interpretation of the northeast Thelon Basin, Nunavut AUTHOR: Victoria Lynn Tschirhart, B.Sc. (McMaster University) SUPERVISOR: Dr. William A. Morris NUMBER OF PAGES: xii, 196 ii Abstract The northeast Thelon Basin, Nunavut, is a rapidly developing albeit poorly studied, frontier exploration domain for unconformity-associated uranium deposits. Critical criteria for unconformity –associated uranium deposit models are knowledge of the basement geology, fault history and depth to unconformity surface. This thesis sets forth to derive working geological and geophysical models for the northeast Thelon Basin through the implementation of integrated geophysical techniques. A physical rock property database is compiled defining average density and susceptibility values for key map units for integration into subsequent modelling iterations. Forward and inverse potential field modelling using these petrophysical with geological controls define the structure and geometry of the Shultz Lake intrusive complex and northeast Amer Belt, both of which are present below the Thelon sedimentary cover. Implementation of a new source edge detection technique estimates fault development and location within the basin. This provides a quantitative analysis of fault timing, identifying potentially reactivated faults which have an increased likelihood to serve as conduits to transport uranium-rich fluids and focus deposition. -
Technical Report on the Gold and Base Metal Potential of the Sy Property, Nunavut, Canada
NTS 65 I/04 to I/06 and J/01 TECHNICAL REPORT ON THE GOLD AND BASE METAL POTENTIAL OF THE SY PROPERTY, NUNAVUT, CANADA Completed By: APEX Geoscience Ltd. Suite 200, 9797-45 Avenue Edmonton, Alberta, Canada T6E 5V8 Completed For: Corsa Capital Ltd. Suite 1440, 625 Howe Street Vancouver, BC V6C 2T6 December 4th, 2007 M.B. Dufresne, M.Sc., P.Geol. TECHNICAL REPORT ON THE GOLD AND BASE METAL POTENTIAL OF THE SY PROPERTY, NUNAVUT, CANADA TABLE OF CONTENTS PAGE SUMMARY...................................................................................................................... 1 INTRODUCTION AND TERMS OF REFERENCE.......................................................... 3 RELIANCE ON OTHER EXPERTS................................................................................. 3 PROPERTY LOCATION AND DESCRIPTION ............................................................... 4 ACCESSIBILITY, CLIMATE, LOCAL RESOURCES, INFRASTRUCTURE AND PHYSIOGRAPHY............................................................................................................ 8 HISTORY ........................................................................................................................ 8 GEOLOGICAL SETTING .............................................................................................. 15 Regional Geology ............................................................................................... 15 Property Geology ............................................................................................... 16 DEPOSIT -
CNGO NU Summary-Of-Activities
SUMMARY OF ACTIVITIES 2015 © 2015 by Canada-Nunavut Geoscience Office. All rights reserved. Electronic edition published 2015. This publication is also available, free of charge, as colour digital files in Adobe Acrobat® PDF format from the Canada- Nunavut Geoscience Office website: www.cngo.ca/ Every reasonable effort is made to ensure the accuracy of the information contained in this report, but Natural Resources Canada does not assume any liability for errors that may occur. Source references are included in the report and users should verify critical information. When using information from this publication in other publications or presentations, due acknowledgment should be given to Canada-Nunavut Geoscience Office. The recommended reference is included on the title page of each paper. The com- plete volume should be referenced as follows: Canada-Nunavut Geoscience Office (2015): Canada-Nunavut Geoscience Office Summary of Activities 2015; Canada- Nunavut Geoscience Office, 208 p. ISSN 2291-1235 Canada-Nunavut Geoscience Office Summary of Activities (Print) ISSN 2291-1243 Canada-Nunavut Geoscience Office Summary of Activities (Online) Front cover photo: Sean Noble overlooking a glacially eroded valley, standing among middle Paleoproterozoic age psam- mitic metasedimentary rocks, nine kilometres west of Chidliak Bay, southern Baffin Island. Photo by Dustin Liikane, Carleton University. Back cover photo: Iqaluit International Airport under rehabilitation and expansion; the Canada-Nunavut Geoscience Of- fice, Geological Survey of Canada (Natural Resources Canada), Centre d’études nordiques (Université Laval) and Trans- port Canada contributed to a better understanding of permafrost conditions to support the planned repairs and adapt the in- frastructure to new climatic conditions. Photo by Tommy Tremblay, Canada-Nunavut Geoscience Office. -
Cold Season Emissions Dominate the Arctic Tundra Methane Budget
Cold season emissions dominate the Arctic tundra methane budget Donatella Zonaa,b,1,2, Beniamino Giolic,2, Róisín Commaned, Jakob Lindaasd, Steven C. Wofsyd, Charles E. Millere, Steven J. Dinardoe, Sigrid Dengelf, Colm Sweeneyg,h, Anna Kariong, Rachel Y.-W. Changd,i, John M. Hendersonj, Patrick C. Murphya, Jordan P. Goodricha, Virginie Moreauxa, Anna Liljedahlk,l, Jennifer D. Wattsm, John S. Kimballm, David A. Lipsona, and Walter C. Oechela,n aDepartment of Biology, San Diego State University, San Diego, CA 92182; bDepartment of Animal and Plant Sciences, University of Sheffield, Sheffield S10 2TN, United Kingdom; cInstitute of Biometeorology, National Research Council, Firenze, 50145, Italy; dSchool of Engineering and Applied Sciences, Harvard University, Cambridge, MA 02138; eJet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109-8099; fDepartment of Physics, University of Helsinki, FI-00014 Helsinki, Finland; gCooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, CO 80304; hEarth System Research Laboratory, National Oceanic and Atmospheric Administration, Boulder, CO 80305; iDepartment of Physics and Atmospheric Science, Dalhousie University, Halifax, Nova Scotia, Canada B3H 4R2; jAtmospheric and Environmental Research, Inc., Lexington, MA 02421; kWater and Environmental Research Center, University of Alaska Fairbanks, Fairbanks, AK 99775-7340; lInternational Arctic Research Center, University of Alaska Fairbanks, Fairbanks, AK 99775-7340; mNumerical Terradynamic Simulation -
AAR Chapter 2
Go back to opening screen 9 Chapter 2 Physical/Geographical Characteristics of the Arctic –––––––––––––––––––––––––––––––––––––––––––––––––––––––––––––––––––––––––––––––––––– Contents 2.2.1. Climate boundaries 2.1. Introduction . 9 On the basis of temperature, the Arctic is defined as the area 2.2. Definitions of the Arctic region . 9 2.2.1. Climate boundaries . 9 north of the 10°C July isotherm, i.e., north of the region 2.2.2. Vegetation boundaries . 9 which has a mean July temperature of 10°C (Figure 2·1) 2.2.3. Marine boundary . 10 (Linell and Tedrow 1981, Stonehouse 1989, Woo and Gre- 2.2.4. Geographical coverage of the AMAP assessment . 10 gor 1992). This isotherm encloses the Arctic Ocean, Green- 2.3. Climate and meteorology . 10 2.3.1. Climate . 10 land, Svalbard, most of Iceland and the northern coasts and 2.3.2. Atmospheric circulation . 11 islands of Russia, Canada and Alaska (Stonehouse 1989, 2.3.3. Meteorological conditions . 11 European Climate Support Network and National Meteoro- 2.3.3.1. Air temperature . 11 2.3.3.2. Ocean temperature . 12 logical Services 1995). In the Atlantic Ocean west of Nor- 2.3.3.3. Precipitation . 12 way, the heat transport of the North Atlantic Current (Gulf 2.3.3.4. Cloud cover . 13 Stream extension) deflects this isotherm northward so that 2.3.3.5. Fog . 13 2.3.3.6. Wind . 13 only the northernmost parts of Scandinavia are included. 2.4. Physical/geographical description of the terrestrial Arctic 13 Cold water and air from the Arctic Ocean Basin in turn 2.4.1. -
Paper 13 (Final).Vp
Overview of the surficial geology map compilation, RapidEye land-cover mapping and permafrost studies for infrastructure in the western Hudson Bay area, Nunavut T. Tremblay1, M.S. Kendall2, A.-M. LeBlanc3, N. Short3, O. Bellehumeur-Génier3, G.A. Oldenborger3, P. Budkewitsch4 and D.J. Mate5 1Canada-Nunavut Geoscience Office, Iqaluit, Nunavut, [email protected] 2Department of Geography, Memorial University of Newfoundland, St. John’s, Newfoundland and Labrador 3Natural Resources Canada, Geological Survey of Canada, Ottawa, Ontario 4Indigenous and Northern Affairs Canada, Iqaluit, Nunavut 5Canadian Northern Economic Development Agency, Iqaluit, Nunavut Tremblay, T., Kendall, M.S., LeBlanc, A.-M., Short, N., Bellehumeur-Génier, O., Oldenborger, G.A., Budkewitsch, P. and Mate, D.J. 2015: Overview of the surficial geology map compilation, RapidEye land-cover mapping and permafrost studies for infrastructure in the western Hudson Bay area, Nunavut; in Summary of Activities 2015, Canada-Nunavut Geoscience Office, p. 145–160. Abstract The Western Hudson Bay project is a Canada-Nunavut Geoscience Office–led geoscience project collecting and compiling geoscience data for infrastructure. Significant new infrastructure is being considered in the Kivalliq region of Nunavut, in- cluding a proposed Manitoba-Nunavut road corridor, in order to support natural resource and community development. Western Hudson Bay lies in the continuous permafrost zone, where 90–100 % of the ground surface is underlain by perma- frost. Alack of compiled regional -
Gjoa Haven © Nunavut Tourism
NUNAVUT COASTAL RESOURCE INVENTORY ᐊᕙᑎᓕᕆᔨᒃᑯᑦ Department of Environment Avatiliqiyikkut Ministère de l’Environnement Gjoa Haven © Nunavut Tourism ᐊᕙᑎᓕᕆᔨᒃᑯᑦ Department of Environment Avatiliqiyikkut NUNAVUT COASTAL RESOURCE INVENTORY • Gjoa Haven INVENTORY RESOURCE COASTAL NUNAVUT Ministère de l’Environnement Nunavut Coastal Resource Inventory – Gjoa Haven 2011 Department of Environment Fisheries and Sealing Division Box 1000 Station 1310 Iqaluit, Nunavut, X0A 0H0 GJOA HAVEN Inventory deliverables include: EXECUTIVE SUMMARY • A final report summarizing all of the activities This report is derived from the Hamlet of Gjoa Haven undertaken as part of this project; and represents one component of the Nunavut Coastal Resource Inventory (NCRI). “Coastal inventory”, as used • Provision of the coastal resource inventory in a GIS here, refers to the collection of information on coastal database; resources and activities gained from community interviews, research, reports, maps, and other resources. This data is • Large-format resource inventory maps for the Hamlet presented in a series of maps. of Gjoa Haven, Nunavut; and Coastal resource inventories have been conducted in • Key recommendations on both the use of this study as many jurisdictions throughout Canada, notably along the well as future initiatives. Atlantic and Pacific coasts. These inventories have been used as a means of gathering reliable information on During the course of this project, Gjoa Haven was visited on coastal resources to facilitate their strategic assessment, two occasions: -
Barren-Ground Caribou Management in the Northwest Territories
Barren-Ground Caribou Management in the Northwest Territories: An Independent Peer Review January 16, 2008 Jason T. Fisher Laurence D. Roy Michelle Hiltz Alberta Research Council Sustainable Ecosystems Unit Ecological Conservation Management Program Vegreville, Alberta, Canada. 1 Table of Contents Table of Contents................................................................................................................ 2 Preface................................................................................................................................. 3 Acknowledgements............................................................................................................. 3 Executive Summary............................................................................................................ 4 Introduction......................................................................................................................... 6 I. Herd-based management ................................................................................................. 7 1. Sample size of collared animals.- ............................................................................. 11 2. Experimental design of collaring surveys.- .............................................................. 14 3. Lack of data on demographic rates for herds.- ......................................................... 16 Conclusions.- ................................................................................................................ 16 II. -
Spatial and Watercourse Influences on Arctic Charr (Salvelinus Alpinus) Migration in Nunavut
Spatial and watercourse influences on Arctic Charr (Salvelinus alpinus) migration in Nunavut Sarah Arnold A thesis submitted to the Faculty of Graduate Studies of The University of Manitoba in partial fulfilment of the requirements of the degree of Master of Science Department of Biological Sciences University of Manitoba Winnipeg, Manitoba Copyright ©2021 by Sarah Arnold ORCID iD: 0000-0002-4653-6981 Abstract Migration is an adaptive mechanism for species to meet life cycle needs in heterogeneous habitats such as the Arctic. The Arctic Charr (Salvelinus alpinus) is a northerly-distributed, partially anadromous fish that is culturally and economically important in Nunavut, Canada. Previous studies have investigated charr migratory choices in specific areas of Nunavut, but our understanding is limited of how these vary across the territory’s freshwater ecosystems. Understanding environmental influences on charr migratory choices can give insight on population reactions to climate change. To assess the drivers behind and differences in Arctic Charr migratory ecotype distribution across Nunavut, I compiled and cleaned three pre-existing sources—the Arctic Fisheries Stock Assessment database (scientific research), the Nunavut Coastal Resource Inventory (mapped Inuit knowledge) and the Nunavut Wildlife Harvest Study (Inuit fishermen harvest records). I used generalized linear mixed models to compare 691 cleaned Inuit knowledge records of anadromous and resident charr populations to river, lake, and geographic variables. I validated these models using 51 independent scientific records and k-fold cross-validation. Inuit knowledge data had more observations across a broader geographic and environmental space. Both models strongly fit the training data, but the resident model was not transferrable to the independent data.