Community Areas of Interest – Multiple Values
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Green Paper the Lancaster Sound Region
Green Paper The Lancaster Sound Region: 1980-2000 Issues and Options on the Use and Management of the Region Lancaster Sound Regional Study H.J. Dirschl Project Manager January 1982 =Published under the authority of the Hon. John C. Munro, P.C., M.P., Minister of Indian Affairs and Northern Development, Ottawa, 1981. 05-8297-020-EE-A1 Catalogue No. R72-164/ 1982E ISBN 0-662-11869 Cette publication peut aussi etre obtenue en francais. Preface In the quest for a "best plan" for Lancaster Sound criticisms. This feedback is discussed in detail in a and its abundant resources, this public discussion recently puolished report by the workshop chairman. paper seeks to stimulate a continued. wide-ranging, Professor Peter Jacobs, entitled People. Resources examination of the issues involved in the future use and the Environment: Perspectives on the Use and and management of this unique area of the Canadian Management of the Lancaster Sound Region. All the Arctic. input received during the public review phase has been taken into consideration in the preparation of the The green paper is the result of more than two years final green paper. of work by the Northern Affairs Program of the Department of Indian Affairs and Northern From the beginning of the study, it was expected that Development, in co-operation with the government of to arrive at an overall consensus of the optimum fu the Northwest Territories and the federal departments ture use and management of the Lancaster Sound of Energy, Mines and Resources, Environment. region would require intensive public discussion fol Fisheries and Oceans. -
198 13. Repulse Bay. This Is an Important Summer Area for Seals
198 13. Repulse Bay. This is an important summer area for seals (Canadian Wildlife Service 1972) and a primary seal-hunting area for Repulse Bay. 14. Roes Welcome Sound. This is an important concentration area for ringed seals and an important hunting area for Repulse Bay. Marine traffic, materials staging, and construction of the crossing could displace seals or degrade their habitat. 15. Southampton-Coats Island. The southern coastal area of Southampton Island is an important concentration area for ringed seals and is the primary ringed and bearded seal hunting area for the Coral Harbour Inuit. Fisher and Evans Straits and all coasts of Coats Island are important seal-hunting areas in late summer and early fall. Marine traffic, materials staging, and construction of the crossing could displace seals or degrade their habitat. 16.7.2 Communities Affected Communities that could be affected by impacts on seal populations are Resolute and, to a lesser degree, Spence Bay, Chesterfield Inlet, and Gjoa Haven. Effects on Arctic Bay would be minor. Coral Harbour and Repulse Bay could be affected if the Quebec route were chosen. Seal meat makes up the most important part of the diet in Resolute, Spence Bay, Coral Harbour, Repulse Bay, and Arctic Bay. It is a secondary, but still important food in Chesterfield Inlet and Gjoa Haven. Seal skins are an important source of income for Spence Bay, Resolute, Coral Harbour, Repulse Bay, and Arctic Bay and a less important income source for Chesterfield Inlet and Gjoa Haven. 16.7.3 Data Gaps Major data gaps concerning impacts on seal populations are: 1. -
Final Complete Dissertation Kua 1
Trends and Ontology of Artistic Practices of the Dorset Culture 800 BC - 1300 AD Hardenberg, Mari Publication date: 2013 Document version Early version, also known as pre-print Citation for published version (APA): Hardenberg, M. (2013). Trends and Ontology of Artistic Practices of the Dorset Culture 800 BC - 1300 AD. København: Det Humanistiske Fakultet, Københavns Universitet. Download date: 08. Apr. 2020 Trends and Ontology of Artistic Practices of the Dorset Culture 800 BC – 1300 AD Volume 1 By © Mari Hardenberg A Dissertation Submitted to the Ph.d.- School In Partial fulfillment of the Requirements for the Degree of Doctor of Philosophy SAXO-Institute, Department of Prehistoric Archaeology, Faculty of Humanities University of Copenhagen August 2013 Copenhagen Denmark ABSTRACT This dissertation examines the various artistic carvings produced by the hunter-gatherer Dorset people who occupied the eastern Arctic and temperate regions of Canada and Greenland between circa BC 800 – AD 1300. It includes considerations on how the carved objects affected and played a role in Dorset social life. To consider the role of people, things and other beings that may be said to play as actors in interdependent entanglements of actions, the agency/actor- network theory is employed. From this theoretical review an interpretation of social life as created by the ways people interact with the material world is presented. This framework is employed as a lens into the social role and meaning the carvings played in the Dorset society. The examined assemblages were recovered from a series of Dorset settlement sites, mainly in house, midden, and burial contexts, providing a substantive case study through which variations and themes of carvings are studied. -
Seasonal Summary
Canadian Ice Service Seasonal Summary for the Canadian Arctic Summer 2009 Produced by the Canadian Ice Service November 06th, 2009 Seasonal Summary - Canadian Arctic Waters - Summer 2009 -1- Canadian Ice Service Table of Contents Hudson and Foxe .......................................................................................................... 4 June 2009.................................................................................................................... 4 July 2009 ..................................................................................................................... 5 August 2009 ................................................................................................................ 5 September 2009 .......................................................................................................... 6 Eastern and High Arctic.............................................................................................. 12 June 2009.................................................................................................................. 12 July 2009 ................................................................................................................... 13 August 2009 .............................................................................................................. 13 September 2009 ........................................................................................................ 14 Western and Central Arctic ....................................................................................... -
Seasonal Outlook for North American Arctic Waters Issued by the North American Ice Service on 2 June 2015
Seasonal Outlook North American Arctic Waters Summer 2015 By the North American Ice Service Seasonal outlook for North American Arctic Waters issued by the North American Ice Service on 2 June 2015. Hudson Bay, Davis Strait and Labrador Coast Summer temperature and ice outlook. Average air temperatures will be near normal over most locations from June to August except for slightly above normal over western Hudson Bay and southern Labrador Coast. However temperatures will be slightly below normal over eastern Hudson Bay and in Davis Strait. In general, forecast ice events are expected to be near normal for most locations this summer except earlier than normal for Hudson Strait, Ungava Bay and southwestern Hudson Bay. Southern Labrador Coast. Over the southern section bergy water. Over the northern section open drift first-year ice with a trace of old ice within 120 miles of the coast. Outlook for June…Open drift ice becoming very open drift ice during the second week. Ice melting completely during the third week. Outlook for July…Bergy water. Northern Labrador Coast. Close to very close pack first-year ice with a trace of old ice within 120 miles of the coast. A narrow zone of very open drift first-year ice along the coast. Outlook for June…Close to very close pack ice becoming open drift ice during the fourth week of June. Outlook for July…Open drift ice melting completely during the second week of July then bergy water. Outlook for August…Bergy water. Lake Melville. Close pack first-year ice except open water along the northern shore. -
Resolute Bay
Qikiqtani Truth Commission Community Histories 1950–1975 Resolute Bay Qikiqtani Inuit Association Published by Inhabit Media Inc. www.inhabitmedia.com Inhabit Media Inc. (Iqaluit), P.O. Box 11125, Iqaluit, Nunavut, X0A 1H0 (Toronto), 146A Orchard View Blvd., Toronto, Ontario, M4R 1C3 Design and layout copyright © 2013 Inhabit Media Inc. Text copyright © 2013 Qikiqtani Inuit Association Photography copyright © 2013 Library and Archives Canada, Northwest Territories Archives, and Tim Kalusha Originally published in Qikiqtani Truth Commission: Community Histories 1950–1975 by Qikiqtani Inuit Association, April 2014. ISBN 978-1-927095-62-1 All rights reserved. The use of any part of this publication reproduced, transmitted in any form or by any means, electronic, mechanical, photocopying, recording, or otherwise, or stored in a retrievable system, without written consent of the publisher, is an infringement of copyright law. We acknowledge the support of the Government of Canada through the Department of Canadian Heritage Canada Book Fund program. We acknowledge the support of the Canada Council for the Arts for our publishing program. Please contact QIA for more information: Qikiqtani Inuit Association PO Box 1340, Iqaluit, Nunavut, X0A 0H0 Telephone: (867) 975-8400 Toll-free: 1-800-667-2742 Fax: (867) 979-3238 Email: [email protected] Errata Despite best efforts on the part of the author, mistakes happen. The following corrections should be noted when using this report: Administration in Qikiqtaaluk was the responsibility of one or more federal departments prior to 1967 when the Government of the Northwest Territories was became responsible for the provision of almost all direct services. The term “the government” should replace all references to NANR, AANDC, GNWT, DIAND. -
The Late Wisconsinan and Holocene Record of Walrus (Odobenus Rosmarus) from North America: a Review with New Data from Arctic and Atlantic Canada ARTHUR S
ARCTIC VOL. 52, NO. 2 (JUNE 1999) P. 160–181 The Late Wisconsinan and Holocene Record of Walrus (Odobenus rosmarus) from North America: A Review with New Data from Arctic and Atlantic Canada ARTHUR S. DYKE,1 JAMES HOOPER,2 C. RICHARD HARINGTON3 and JAMES M. SAVELLE4 (Received 30 March 1998; accepted in revised form 20 October 1998) ABSTRACT. The Late Wisconsinan and Holocene record of the Atlantic walrus is known from numerous collections of bones and tusks from Arctic Canada and south to North Carolina, as well as from many archaeological sites in the Arctic and Subarctic. In contrast, the Pacific walrus has no dated Late Wisconsinan or early Holocene record in North America, and it may have been displaced into the northwest Pacific at Last Glacial Maximum (LGM). The Atlantic walrus rapidly exploited newly deglaciated territory, moving northward from its LGM refugium and reaching the Bay of Fundy by 12800 B.P., the Grand Banks by 12500 B.P., southern Labrador by 11 500 B.P., and the central Canadian Arctic Archipelago (CAA) by 9700 B.P. Its southern range limit may have retracted to the Bay of Fundy by ca. 7500 B.P. Within the CAA, walrus remains cluster in two main age groups: 9700 to 8500 B.P. and 5000 to 4/3000 B.P. This pattern strongly resembles the distribution of bowhead whale radiocarbon ages from the same area, which suggests a common control by sea-ice conditions. Walrus remains occur in Indian culture archaeological sites as old as 7500 B.P. and, in some cases (Namu, British Columbia, and Mackinac Island, Michigan), they evidently represent long-distance human transport. -
LNG Transport in Parry Channel: Possible Environmental Hazards Brian D
LNG Transport in Parry Channel: Possible environmental hazards Brian D. Smiley and Allen R. Milne Institute of Ocean Sciences, Patricia Bay Sidney, B.C. ": t 005562 LNG TRANSPORT IN PARRY CHANNEL: POSSIBLE ENVIRONMENTAL HAZARDS By ". .' Brian D. Smiley and Allen R. Milne Institute of Ocean Sciences, Patricia Bay Sidney, B.C. 1979 This is a manuscript which ha~ received only limited circulation. On citing this report in a 1;:libliography, tl;1e title should be followed 1;:ly the words "UNPUELISHED MANUSCRIPT" which is in accordance with accepted bib liographic custom. (i) TABLE OF CONTENTS Page Table of Contents (i) Li s t of Fi gures (i i) List of Tables (i i i) Map of Parry Channel (i v) Acknowl edgments ( i v) l. SUMMARY 2. I NTRODUCTI ON 3 3. ARCTIC PILOT PROJECT 7 3.1 Components 7 3.2 Gas Delivery Rate 7 3.3 Energy Efficiency 7 3.4 Properties of LNG 8 3.5 Carrier Characteristics 8 3.6 Carrier Operation 8 3.7: The Future 9 4. ACCIDENTS . 10 5. ICE AND LNG ICEBREAKERS IN PARRY CHANNEL 12 5.1 Ice Drift and Surface Circulation 12 5.2 Wi nter Ice Cover 13 5.3 The Icebreaker's Wake in Ice 15 5.4 Routing through Ice 18 6. CLIMATE AND LNG ICEBREAKERS IN PARRY CHANNEL 20 6.1 Long-term Climate Trends 21 7. ECOLOGICAL SIGNIFICANCE OF PARRY CHANNEL 22 8. WILDLIFE AND LNG ICEBREAKERS IN PARRY CHANNEL 26 8.1 Seabirds 26 8.2 Ringed Seals 29 8.3 Bearded Seals 33 8.4 Polar Bears 33 8.5 Whales 36 8.6 Harp Seals 37 8.7 Wal ruses 38 8.8 Caribou 38 9. -
The Use of Dog Sledges During the British Search for the Missing Franklin Expedition in the North American Arctic Islands, 1848–59 WILLIAM BARR1
ARCTIC VOL. 62, NO. 3 (SEPTEMBER 2009) P. 257–272 The Use of Dog Sledges during the British Search for the Missing Franklin Expedition in the North American Arctic Islands, 1848–59 WILLIAM BARR1 (Received 4 September 2008; accepted in revised form 17 October 2008) ABSTRACT. While the bulk of the searching parties sent out from the British ships deployed on the search for the missing Franklin expedition in the North American Arctic Islands over the period 1848–59 employed man-hauled sledges, dog sledges were also used quite extensively. The dog sledges were especially (but not exclusively) used as “couriers,” that is, for communi- cation between the various wintering ships, where speed was the primary requirement. The total distance covered by dog sledges (excluding short hauls in the vicinity of the wintering ships) was, at a minimum, 11 576 km; this distance compares with the minimum 41 555 km covered by man-hauled sledges. Key words: dog sledges, Franklin search expeditions, North American Arctic Islands RÉSUMÉ. Bien que la plupart des équipes de recherche déployées par les navires britanniques à la recherche de l’expédition de Franklin disparue dans l’archipel Arctique nord-américain pendant la période de 1848–1859 se soient servi de traîneaux tirés par des humains, elles ont également employé des traîneaux à chiens à maintes reprises. Les traîneaux à chiens servaient plus particulièrement (mais non pas exclusivement) de « messagers » en ce sens qu’ils établissaient les liens de communication entre les divers navires en hivernage, la rapidité de transmission étant essentielle. La distance totale à avoir été parcourue par les traîneaux à chiens (ce qui ne comprend pas les courtes distances dans la région des navires en hivernage) s’est chiffrée, au minimum, à 11 576 kilomètres, comparativement à la distance minimale de 41 555 kilomètres parcourue par les traîneaux tirés par des humains. -
November 29, 1995
FECN16 CWIS 011800 THIRTY DAY ICE OUTLOOK FOR THE EASTERN AND NORTHERN ARCTIC FOR JULY ISSUED BY ENVIRONMENT CANADA ON 01 JULY 2021. THE NEXT 30 DAY OUTLOOK WILL BE ISSUED ON 15 JULY 2021. Summary for June 15 to 28. Average air temperatures were above normal over Baffin Bay and into the northern Queen Elizabeth Islands. Elsewhere, average air temperatures were near normal. Ice melt was 1 to 2 weeks earlier than normal. Weather forecast for July 1 to 31. Air temperatures are forecast to be near to below normal for the entire area. Northern Baffin Bay. July 1-7 - Bergy water with isolated patches of 4-6 tenths first-year including up to 2 tenths old ice drifting from Kane Basin into the northwestern section. - Bergy water with areas of 4-6 tenths first-year ice including a trace of old ice in the western section. - Elsewhere, 7-8 tenths first-year ice including a trace of old ice with areas of 9-9+ tenths first-year ice including a trace of old ice. July 8-15 - Bergy water with isolated patches of 4-6 tenths ice drifting in from Kane Basin and from eastern Jones Sound. - Bergy water with areas of 1-3 tenths ice in the western section. - Elsewhere, 4-6 tenths ice with areas of 7-8 tenths ice. July 16-21 - Bergy water with isolated patches of 1-3 tenths ice drifting in from Kane Basin and eastern Jones Sound. - 1-3 tenths ice with areas of 4-6 tenths ice in the southern section. -
The Increase in the Length of the Ice-Free Season in the Arctic
Cold Regions Science and Technology 59 (2009) 78–101 Contents lists available at ScienceDirect Cold Regions Science and Technology journal homepage: www.elsevier.com/locate/coldregions The increase in the length of the ice-free season in the Arctic J. Rodrigues Department of Applied Mathematics and Theoretical Physics, University of Cambridge, Cambridge, CB3 0WA, UK article info abstract Article history: The length of the ice-free season and a variable designated by inverse sea ice index are used to quantify the rapid Received 24 February 2009 decline of the Arctic sea ice of the last decades. It is argued that for this purpose they are at least as suitable as the Accepted 10 May 2009 other variables more often found in the literature, namely the sea ice area and extent at the times of annual minimum. Daily sea ice concentrations obtained from satellite passive microwave imagery are used to calculate Keywords: the length of the ice-free season and the inverse sea ice index in each point of the Arctic for each year between Sea ice 1979 and 2008. Time-series for these two quantities are constructed and analysed to investigate how they have Ice-free season Sea ice index been varying in the last 30 years in 85 disjoint regions of the northern hemisphere. It is shown that between 1979 Arctic Ocean and 2006 the spatially averaged ice-free season in the Arctic increased at a steady rate of 1.1 days/year and that the Climate change growth was considerably faster (5.5 days/year), and monotonic, in the 2001–2007 period. -
From Wherever the Fast Ice Edge Is Located in Lancaster Sound Or Barrow Strait, and in an Easterly Direction from M'clure Strait and Amundsen Gulf
from wherever the fast ice edge is located in Lancaster Sound or Barrow Strait, and in an easterly direction from M'Clure Strait and Amundsen Gulf. Figure 7.3.1.8 presents the average date of occurrence for each event as well as the range of dates recorded over 13 years (Gorman 1988). Break-up of the ice cover between each of the geographic locations occurs very rapidly; in the order of days (Dickins 1983; Gorman 1986). In most years, the ice sheet becomes extensively fractured and then breaks into large floes in the order of tens of kilometres (Maxwell 1980). b) Prince of Wales Strait Prince of Wales Strait is one of two channels to be used by the Polar 8 to access the Beaufort Sea from Parry Channel. It is a narrow channel, and concerns were raised during the Beaufort EIS over the effect of icebreaking ships on the ice regime of such channels. The ice regime of Prince of Wales Strait and possible effects of ship traffic were the subject of a discussion paper written by Dickens (1983) on behalf of the proponents of the Beaufort Sea development. The Strait is typically covered by stable landfast ice from late October until mid to late Julf(Dickins 1983; Gorman 1988). Gorman (1988) reported the average date of fracture was July 15 with a range from July 5 to 28 based on 13 years of data. Dickins (1983) divided the ice regime into north and south sections of the channel, separated by the Princess Royal Islands. Break-up begins in the south section and is extremely variable with up to three weeks between first fracturing and major ice movement (Dickins 1983).