Peary Caribou Management Plan Was Submitted to the NWMB for Decision in 2014 but the Process Was Delayed Until the September, 2017 Regular Board Meeting
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Modelling the Transfer of Supraglacial Meltwater to the Bed of Leverett Glacier, Southwest Greenland
The Cryosphere, 9, 123–138, 2015 www.the-cryosphere.net/9/123/2015/ doi:10.5194/tc-9-123-2015 © Author(s) 2015. CC Attribution 3.0 License. Modelling the transfer of supraglacial meltwater to the bed of Leverett Glacier, Southwest Greenland C. C. Clason1, D. W. F. Mair2, P. W. Nienow3, I. D. Bartholomew3, A. Sole4, S. Palmer5, and W. Schwanghart6 1Department of Physical Geography and Quaternary Geology, Stockholm University, 106 91 Stockholm, Sweden 2Geography and Environment, University of Aberdeen, Aberdeen, AB24 3UF, UK 3School of Geosciences, University of Edinburgh, Edinburgh, EH8 9XP, UK 4Department of Geography, University of Sheffield, Sheffield, S10 2TN, UK 5Geography, College of Life and Environmental Sciences, University of Exeter, Exeter, EX4 4RJ, UK 6Institute of Earth and Environmental Science, University of Potsdam, 14476 Potsdam-Golm, Germany Correspondence to: C. C. Clason ([email protected]) Received: 23 June 2014 – Published in The Cryosphere Discuss.: 29 July 2014 Revised: 12 December 2014 – Accepted: 24 December 2014 – Published: 22 January 2015 Abstract. Meltwater delivered to the bed of the Greenland melt to the bed matches the observed delay between the peak Ice Sheet is a driver of variable ice-motion through changes air temperatures and subsequent velocity speed-ups, while in effective pressure and enhanced basal lubrication. Ice sur- the instantaneous transfer of melt to the bed in a control sim- face velocities have been shown to respond rapidly both ulation does not. Although both moulins and lake drainages to meltwater production at the surface and to drainage of are predicted to increase in number for future warmer climate supraglacial lakes, suggesting efficient transfer of meltwa- scenarios, the lake drainages play an increasingly important ter from the supraglacial to subglacial hydrological systems. -
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 -
A Hans Krüger Arctic Expedition Cache on Axel Heiberg Island, Nunavut ROBERT W
ARCTIC VOL. 60, NO. 1 (MARCH 2007) P. 1–6 A Hans Krüger Arctic Expedition Cache on Axel Heiberg Island, Nunavut ROBERT W. PARK1 and DOUGLAS R. STENTON2 (Received 13 June 2006; accepted in revised form 31 July 2006) ABSTRACT. In 1999 a team of geologists discovered an archaeological site near Cape Southwest, Axel Heiberg Island. On the basis of its location and the analysis of two artifacts removed from the site, the discoverers concluded that it was a hastily abandoned campsite created by Hans Krüger’s German Arctic Expedition, which was believed to have disappeared between Meighen and Amund Ringnes islands in 1930. If the attribution to Krüger were correct, the existence of this site would demonstrate that the expedition got farther on its return journey to Bache Peninsula than previously believed. An archaeological investigation of the site by the Government of Nunavut in 2004 confirmed its tentative attribution to the German Arctic Expedition but suggested that it is not a campsite, but the remains of a deliberately and carefully constructed cache. The finds suggest that one of the three members of the expedition may have perished before reaching Axel Heiberg Island, and that the survivors, in order to lighten their sledge, transported valued but heavy items (including Krüger’s geological specimens) to this prominent and well-known location to cache them, intending to return and recover them at some later date. Key words: German Arctic Expedition, Hans Krüger, archaeology, geology, Axel Heiberg Island, Nunavut RÉSUMÉ. En 1999, une équipe de géologues a découvert un lieu d’importance archéologique près du cap Southwest, sur l’île Axel Heiberg. -
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. -
Volume 12, 1959
THE ARCT IC CIRCLE THE COMMITTEE 1959 Officers President: Dr. D.C. Rose Vice -Presidents Mr. L.A.C.O. Hunt Secretary: Mr. D. Snowden Treasurer: Mr. J .E. Cleland Publications Secretary: Miss Mary Murphy Editor: Mrs .G.W. Rowley Members Mr. Harvey Blandford Mr. Welland Phipps Mr. J. Cantley Mr. A. Stevenson Mr. F..A. Cate Mr. Fraser Symington L/Cdr. J.P. Croal, R.C.N. Mr. J .5. Tener Miss Moira Dunbar Dr. R. Thorsteinsson W IC K. R. Greenaway, R.C.A.F. Dr. J.S. Willis Mr. T .H. Manning Mr. J. Wyatt Mr. Elijah Menarik CONTENTS VOLUME XlI, 1959 NO.1 Meetings of the Arctic Circle 1 Officers and Committee Members for 1959 Z Research in the Lake Hazen region of northern Ellesmere Island in the International Geophysical Year Z Anthropological work in the Eastern Arctic, 1958 13 Geomorphological studies on Southampton Island, 1958 15 Bird Sanctuaries in Southampton Island 17 Subscriptions for 1959 18 Change of Address 18 Editorial Note 18 NO. Z U.S. Navy airship flight to Ice Island T3 19 Firth River archaeological activities. 1956 and 1958 Z6 A light floatplane operation in the far northern islands, 1958 Z9 Change of Address 31 Editorial Note 31 NO.3 Meetings of the Arctic Circle 3Z The Polar Continental Shelf Project, 1959 3Z Jacobsen-McGill Arctic Research Expedition to Axel Heiberg Island 38 Biological work on Prince of Wales Island in the summer of 1958 40 Geographical Branch Survey in southern Melville Peninsula, 1959 43 Pilot of Arctic Canada 48 Subsc riptions for 1960 50 Change of Address 51 • Editorial Note 51 I NO.4 Meetings of the Arctic Circle 52 Officers and Committee Members for 1960 52 Some factors regarding northern oil and gas 53 Nauyopee. -
Origin, Burial and Preservation of Late Pleistocene-Age Glacier Ice in Arctic
Origin, burial and preservation of late Pleistocene-age glacier ice in Arctic permafrost (Bylot Island, NU, Canada) Stephanie Coulombe1 2 3, Daniel Fortier 2 3 5, Denis Lacelle4, Mikhail Kanevskiy5, Yuri Shur5 6 1Polar Knowledge Canada, Cambridge Bay, X0B 0C0, Canada 5 2Department of Geography, Université de Montréal, Montréal, H2V 2B8, Canada 3Centre for Northern Studies, Université Laval, Quebec City, G1V 0A6, Canada 4Department of Geography, Environment and Geomatics, University of Ottawa, Ottawa, K1N 6N5, Canada 5Institute of Northern Engineering, University of Alaska Fairbanks, Fairbanks, 99775-5910, USA 6Department of Civil and Environmental Engineering, University of Alaska Fairbanks, Fairbanks, 99775-5960, USA 10 Correspondence to: Stephanie Coulombe ([email protected]) Over the past decades, observations of buried glacier ice exposed in coastal bluffs and headwalls of retrogressive thaw slumps of the Arctic indicate that considerable amounts of late Pleistocene glacier ice survived the deglaciation and are still preserved in permafrost. In exposures, relict glacier ice and intrasedimental ice often coexist and look alike but their genesis is strikingly different. This paper aims to present a detailed description and infer the origin of a massive ice body preserved in the permafrost 15 of Bylot Island (Nunavut). The massive ice exposure and core samples were described according to the cryostratigraphic approach, combining the analysis of permafrost cryofacies and cryostructures, ice crystallography, stable O-H isotopes and cation contents. The ice was clear to whitish in appearance with large crystals (cm) and small gas inclusions (mm) at crystal intersections, similar to observations of englacial ice facies commonly found on contemporary glaciers and ice sheets. -
Appendix A. Survival Strategies of the Ecotonal Species
Appendix A. Survival Strategies of the Ecotonal Species With greater numbers of species found in relatively high abundance in communities of both the boreal zone and the arctic regions, with fewer in the forest-tundra ecotonal communities, the question arises as to the strategies involved that permit adaptations to disparate environments yet prohibit all but a few from surviving in the ecotone, at least in numbers sufficient so they are recorded in quadrats of the size employed in transects of this study. There is a depauperate zone in the forest-tundra ecotone marked by a paucity of species, a zone in which only a relatively few wide-ranging species are persistently dominant (see Tables 5.1-5.9). Plant communities in both the forests to the south and the tundra to the north possess more species of sufficient abundance to show up in the transects. In the depauperate zone, there is no lack of vegetational cover over the landscape, but fewer species in total dominate the communities. There are fewer species demonstrating intermediate abundance, fewer rare species. The obvious question is, "Why should this be so?" As yet, there is perhaps no fully satisfactory answer, but there have been studies that at least seem to point the way for an approach to the question. Studies of the survival and reproductive strategies oftundra plants, arctic and alpine, have a long history, and these are thoroughly discussed in classic papers and reviews by Britton (1957), Jeffree (1960), Warren Wilson (1957a,b, 1966a,b, 1967), Johnson et al. (1966), Johnson and Packer (1967), Billings and Mooney (1968), Bliss (1956, 1958, 1962, 1971), Billings (1974), and Wiclgolaski et al. -
Across Borders, for the Future: Torngat Mountains Caribou Herd Inuit
ACROSS BORDERS, FOR THE FUTURE: Torngat Mountains Caribou Herd Inuit Knowledge, Culture, and Values Study Prepared for the Nunatsiavut Government and Makivik Corporation, Parks Canada, and the Torngat Wildlife and Plants Co-Management Board - June 2014 This report may be cited as: Wilson KS, MW Basterfeld, C Furgal, T Sheldon, E Allen, the Communities of Nain and Kangiqsualujjuaq, and the Co-operative Management Board for the Torngat Mountains National Park. (2014). Torngat Mountains Caribou Herd Inuit Knowledge, Culture, and Values Study. Final Report to the Nunatsiavut Government, Makivik Corporation, Parks Canada, and the Torngat Wildlife and Plants Co-Management Board. Nain, NL. All rights reserved. No part of this publication may be reproduced, stored in a retrieval system, or transmitted in any form or by any means, electronic, mechanical, photocopying, recording, or otherwise (except brief passages for purposes of review) without the prior permission of the authors. Inuit Knowledge is intellectual property. All Inuit Knowledge is protected by international intellectual property rights of Indigenous peoples. As such, participants of the Torngat Mountains Caribou Herd Inuit Knowledge, Culture, and Values Study reserve the right to use and make public parts of their Inuit Knowledge as they deem appropriate. Use of Inuit Knowledge by any party other than hunters and Elders of Nunavik and Nunatsiavut does not infer comprehensive understanding of the knowledge, nor does it infer implicit support for activities or projects in which this knowledge is used in print, visual, electronic, or other media. Cover photo provided by and used with permission from Rodd Laing. All other photos provided by the lead author. -
Who Discovered the Northwest Passage? Janice Cavell1
ARCTIC VOL. 71, NO.3 (SEPTEMBER 2018) P.292 – 308 https://doi.org/10.14430/arctic4733 Who Discovered the Northwest Passage? Janice Cavell1 (Received 31 January 2018; accepted in revised form 1 May 2018) ABSTRACT. In 1855 a parliamentary committee concluded that Robert McClure deserved to be rewarded as the discoverer of a Northwest Passage. Since then, various writers have put forward rival claims on behalf of Sir John Franklin, John Rae, and Roald Amundsen. This article examines the process of 19th-century European exploration in the Arctic Archipelago, the definition of discovering a passage that prevailed at the time, and the arguments for and against the various contenders. It concludes that while no one explorer was “the” discoverer, McClure’s achievement deserves reconsideration. Key words: Northwest Passage; John Franklin; Robert McClure; John Rae; Roald Amundsen RÉSUMÉ. En 1855, un comité parlementaire a conclu que Robert McClure méritait de recevoir le titre de découvreur d’un passage du Nord-Ouest. Depuis lors, diverses personnes ont avancé des prétentions rivales à l’endroit de Sir John Franklin, de John Rae et de Roald Amundsen. Cet article se penche sur l’exploration européenne de l’archipel Arctique au XIXe siècle, sur la définition de la découverte d’un passage en vigueur à l’époque, de même que sur les arguments pour et contre les divers prétendants au titre. Nous concluons en affirmant que même si aucun des explorateurs n’a été « le » découvreur, les réalisations de Robert McClure méritent d’être considérées de nouveau. Mots clés : passage du Nord-Ouest; John Franklin; Robert McClure; John Rae; Roald Amundsen Traduit pour la revue Arctic par Nicole Giguère. -
ARCTIC Exploration the SEARCH for FRANKLIN
CATALOGUE THREE HUNDRED TWENTY-EIGHT ARCTIC EXPLORATION & THE SeaRCH FOR FRANKLIN WILLIAM REESE COMPANY 409 Temple Street New Haven, CT 06511 (203) 789-8081 A Note This catalogue is devoted to Arctic exploration, the search for the Northwest Passage, and the later search for Sir John Franklin. It features many volumes from a distinguished private collection recently purchased by us, and only a few of the items here have appeared in previous catalogues. Notable works are the famous Drage account of 1749, many of the works of naturalist/explorer Sir John Richardson, many of the accounts of Franklin search expeditions from the 1850s, a lovely set of Parry’s voyages, a large number of the Admiralty “Blue Books” related to the search for Franklin, and many other classic narratives. This is one of 75 copies of this catalogue specially printed in color. Available on request or via our website are our recent catalogues: 320 Manuscripts & Archives, 322 Forty Years a Bookseller, 323 For Readers of All Ages: Recent Acquisitions in Americana, 324 American Military History, 326 Travellers & the American Scene, and 327 World Travel & Voyages; Bulletins 36 American Views & Cartography, 37 Flat: Single Sig- nificant Sheets, 38 Images of the American West, and 39 Manuscripts; e-lists (only available on our website) The Annex Flat Files: An Illustrated Americana Miscellany, Here a Map, There a Map, Everywhere a Map..., and Original Works of Art, and many more topical lists. Some of our catalogues, as well as some recent topical lists, are now posted on the internet at www.reeseco.com. -
Supraglacial Rivers on the Northwest Greenland Ice Sheet, Devon Ice Cap, and Barnes Ice Cap Mapped Using Sentinel-2 Imagery
This is a repository copy of Supraglacial rivers on the northwest Greenland Ice Sheet, Devon Ice Cap, and Barnes Ice Cap mapped using Sentinel-2 imagery. White Rose Research Online URL for this paper: http://eprints.whiterose.ac.uk/141238/ Version: Accepted Version Article: Yang, K., Smith, L., Sole, A. et al. (4 more authors) (2019) Supraglacial rivers on the northwest Greenland Ice Sheet, Devon Ice Cap, and Barnes Ice Cap mapped using Sentinel-2 imagery. International Journal of Applied Earth Observation and Geoinformation, 78. pp. 1-13. ISSN 0303-2434 https://doi.org/10.1016/j.jag.2019.01.008 Article available under the terms of the CC-BY-NC-ND licence (https://creativecommons.org/licenses/by-nc-nd/4.0/). Reuse This article is distributed under the terms of the Creative Commons Attribution-NonCommercial-NoDerivs (CC BY-NC-ND) licence. This licence only allows you to download this work and share it with others as long as you credit the authors, but you can’t change the article in any way or use it commercially. More information and the full terms of the licence here: https://creativecommons.org/licenses/ Takedown If you consider content in White Rose Research Online to be in breach of UK law, please notify us by emailing [email protected] including the URL of the record and the reason for the withdrawal request. [email protected] https://eprints.whiterose.ac.uk/ 1 Supraglacial rivers on the northwest Greenland Ice Sheet, Devon Ice Cap, and 2 Barnes Ice Cap mapped using Sentinel-2 imagery 3 Kang Yang1,2,3, Laurence C. -
Submission to The
SUBMISSION TO THE NUNAVUT WILDLIFE MANAGEMENT BOARD FOR Information: Decision: X Issue: Southampton Island (SHI) Caribou Management Background: • The Southampton Island caribou herd was in decline beginning in June 2003, and by June 2011 had declined to levels unable to sustain the estimated subsistence harvest. • The main cause of the decline was a reproductive disease termed Brucellosis. This disease causes severe reproductive declines within caribou populations, negatively impacting birth rates in females and sperm production in reproductive males through testicular tissue damage. • Though the disease is thought to have caused the decline, intra-territorial sales of caribou meat from SHI to primarily Baffin Communities dramatically accelerated the decline in 2010 and 2011. • The establishment of a TAH helped control this intra-territorial sale, helping to stabilize the population. • Management actions have proven effective thus far but all parties are very concerned about finding a way to control the intra-territorial sale of caribou meat if we are to secure the herds future. Current Status • The SHI caribou population has increased from an estimated 7,287 caribou in May 2013 to 12,297 caribou in May 2015. • Both the Department of Environment (DOE) and the Coral Harbour Hunters and Trappers Organization (HTO) believe this increase is at least in part related to an emigration event detected by Coral Harbour hunters in the winter of 2013/2014 from mainland Nunavut. • DOE is currently comparing genetic profiles of recent caribou samples with pre- immigration samples in an attempt to confirm this immigration event. • Additionally both Coral Harbour harvesters and DOE survey crews have detected an increase in calf observations between the 2012/13 harvesting season and the present suggesting an increase in productivity over the same period.