The State of the Polar Bear Report 2020
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Management Consultations for the Western Hudson Bay (Wh) Polar Bear Population (01-02 December 2005)
MANAGEMENT CONSULTATIONS FOR THE WESTERN HUDSON BAY (WH) POLAR BEAR POPULATION (01-02 DECEMBER 2005) Martha Dowsley1 Mitch Taylor2 1Department of Geography, 705 Burnside Hall, McGill University, 805 Sherbrooke St. West, Montreal, QC H3A 2K6 2Wildlife Research Section, Department of Environment, Government of Nunavut, P.O. Box 209, Igloolik, NU X0A 0L0 2006 Final Wildlife Report, No. 3 Dowsley, M. and M. K. Taylor. 2006. Management consultations for the Western Hudson Bay (WH) polar bear population (01-02 December 2005). Government of Nunavut, Department of Environment, Final Wildlife Report: 3, Iqaluit, 55 pp. Management Consultations for the Western Hudson Bay (WH) Polar Bear Population (01-02 December 2005) Participants included: Arviat, Whale Cove, Rankin Inlet, Chesterfield Inlet, and Baker Lake HTOs Kivalliq Wildlife Board Nunavut Tungavik Incorporated Department of Environment, Government of Nunavut Martha Dowsley, McGill University and Mitchell Taylor, Department of Environment, GN 4 May 2007 Background: A recent population analysis by the Canadian Wildlife Service (CWS) for the WH population has demonstrated that the population has declined from about 1100 in 1994 to about 950 in 2004. This decline occurred at removal rates that had previously allowed the population to increase. The scientific data are entirely consistent with the hypothesis that survival and birth rates have been reduced by climate change, which caused the historical removal rates to cause decline in numbers. However, in December 2004 Nunavut increased the TA for WH polar bears by 9/year (from 47 to 56) based on Inuit perceptions that the population had increased. The final Canadian Wildlife Service Analysis indicates that population numbers and productivity have declined to so that a maximum of 24 bears per year can be taken from the population at 2 males per female without exceeding risk management guidelines (i.e., less than a 10% chance of an unacceptable decline). -
The Second Norwegian Polar Expedition in the “Fram,” 1898–1902
Scottish Geographical Magazine ISSN: 0036-9225 (Print) (Online) Journal homepage: http://www.tandfonline.com/loi/rsgj19 The second Norwegian Polar expedition in the “Fram,” 1898–1902 Captain Otto Sverdrup To cite this article: Captain Otto Sverdrup (1903) The second Norwegian Polar expedition in the “Fram,” 1898–1902, Scottish Geographical Magazine, 19:7, 337-353, DOI: 10.1080/14702540308554276 To link to this article: http://dx.doi.org/10.1080/14702540308554276 Published online: 30 Jan 2008. Submit your article to this journal Article views: 6 View related articles Full Terms & Conditions of access and use can be found at http://www.tandfonline.com/action/journalInformation?journalCode=rsgj19 Download by: [University of Sydney Library] Date: 07 June 2016, At: 04:10 THE SCOTTISH GEOGRAPHICAL MAGAZINE. THE SECOND NORWEGIAN POLAR EXPEDITION IN THE "FRAM," 1898-19022 By Captain OTTO SVERDRUP. UPON learning that Messrs. Axel Heiberg and Ringnes Brothers were willing to defray the costs of a Polar expedition under my guidance and direction, I petitioned the Norwegian Government to lend me the Arctic vessel Fram. The Government at once placed her at my service, while the Storthing generously granted 26,000 kroner (2 £1445)for the renovation of the ship and the construction of a new saloon forward, two working-cabins, and six berths for the officers and scientific staff. The Fram was a first-rate boat before these alterations were made. Prof. Nansen had asked Mr. Collin Archer to make her strong, and strong she unquestionably was. But now she was better than ever; and though she was not so severely tried on the second occasion as she was on the first, still she did not escape without two or three pretty severe tussles. -
Seismic Reflection Profiles from Kane to Hall Basin, Nares Strait: Evidence for Faulting
Polarforschung 74 (1-3), 21 – 39, 2004 (erschienen 2006) Seismic Reflection Profiles from Kane to Hall Basin, Nares Strait: Evidence for Faulting by H. Ruth Jackson1, Tim Hannon1, Sönke Neben2, Karsten Piepjohn2 and Tom Brent3 Abstract: Three major tectonic boundaries are predicted to be present beneath durch eine folgende kompressive Phase reaktiviert wurde. Als Arbeitshypo- the waters of this segment of Nares Strait: (1) the orogenic front of the Paleo- these fassen wir die oberflächennahen Teile dieses Systems als Stirn der Plat- zoic Ellesmerian Foldbelt between thrust sheets on Ellesmere Island and flat- tengrenze zwischen Nordamerika und Grönland auf. lying foreland rocks on Greenland, (2) the supposed sinistral strike-slip plate boundary of Paleocene age between the Ellemere Island section of the North America plate and the Greenland plate, and (3) the orogenic front of the Eocene to Oligocene Eurekan Foldbelt that must lie between thrust tectonics INTRODUCTION on Ellesmere Island and undeformed rocks of Greenland. To understand this complicated situation and to look for direct evidence of the plate boundary, The Late Cretaceous and Tertiary deformation on Ellesmere new seismic reflection profiles were collected and, together with industry data in the south, interpreted. The profiles are clustered in three areas controlled by Island (Fig. 1) called the Eurekan Orogeny has been attributed the distribution of the sea ice. Bathymetry is used to extrapolate seismic to the counter clockwise rotation of Greenland (e.g., OKULITCH features with a topographic expression between the regions. Based on high- & TRETTIN 1991). However reconciling the geology on oppo- resolution boomer and deeper penetration airgun profiles five seismic units are mapped. -
Chapter 8 Polar Bear Harvesting in Baffin Bay and Kane Basin: a Summary of Historical Harvest and Harvest Reporting, 1993 to 2014
Chapter 8 SWG Final Report CHAPTER 8 POLAR BEAR HARVESTING IN BAFFIN BAY AND KANE BASIN: A SUMMARY OF HISTORICAL HARVEST AND HARVEST REPORTING, 1993 TO 2014 KEY FINDINGS Both Canada (Nunavut) and Greenland harvest from the shared subpopulations of polar • bears in Baffin Bay and Kane Basin. During 1993-2005 (i.e., before quotas were introduced in Greenland) the combined • annual harvest averaged 165 polar bears (range: 120-268) from the Baffin Bay subpopulation and 12 polar bears (range: 6-26) from Kane Basin (for several of the years, harvest reported from Kane Basin was based on an estimate). During 2006-2014 the combined annual harvest averaged 161 (range: 138-176) from • Baffin Bay and 6 (range: 3-9) polar bears from Kane Basin. Total harvest peaked between 2002 and 2005 coinciding with several events in harvest • reporting and harvest management in both Canada and Greenland. In Baffin Bay the sex ratio of the combined harvest has remained around 2:1 (male: • females) with an annual mean of 35% females amongst independent bears. In Kane Basin the sex composition of the combined harvest was 33% females overall for • the period 1993-2014. The estimated composition of the harvest since the introduction of a quota in Greenland is 44% female but the factual basis for estimation of the sex ratio in the harvest is weak. In Greenland the vast majority of bears are harvested between January and June in Baffin • Bay and Kane Basin whereas in Nunavut ca. 40% of the harvest in Baffin Bay is in the summer to fall (August – November) while bears are on or near shore. -
Re-Evaluation of Strike-Slip Displacements Along and Bordering Nares Strait
Polarforschung 74 (1-3), 129 – 160, 2004 (erschienen 2006) In Search of the Wegener Fault: Re-Evaluation of Strike-Slip Displacements Along and Bordering Nares Strait by J. Christopher Harrison1 Abstract: A total of 28 geological-geophysical markers are identified that lich der Bache Peninsula und Linksseitenverschiebungen am Judge-Daly- relate to the question of strike slip motions along and bordering Nares Strait. Störungssystem (70 km) und schließlich die S-, später SW-gerichtete Eight of the twelve markers, located within the Phanerozoic orogen of Kompression des Sverdrup-Beckens (100 + 35 km). Die spätere Deformation Kennedy Channel – Robeson Channel region, permit between 65 and 75 km wird auf die Rotation (entgegen dem Uhrzeigersinn) und ausweichende West- of sinistral offset on the Judge Daly Fault System (JDFS). In contrast, eight of drift eines semi-rigiden nördlichen Ellesmere-Blocks während der Kollision nine markers located in Kane Basin, Smith Sound and northern Baffin Bay mit der Grönlandplatte zurückgeführt. indicate no lateral displacement at all. Especially convincing is evidence, presented by DAMASKE & OAKEY (2006), that at least one basic dyke of Neoproterozoic age extends across Smith Sound from Inglefield Land to inshore eastern Ellesmere Island without any recognizable strike slip offset. INTRODUCTION These results confirm that no major sinistral fault exists in southern Nares Strait. It is apparent to both earth scientists and the general public To account for the absence of a Wegener Fault in most parts of Nares Strait, that the shape of both coastlines and continental margins of the present paper would locate the late Paleocene-Eocene Greenland plate boundary on an interconnected system of faults that are 1) traced through western Greenland and eastern Arctic Canada provide for a Jones Sound in the south, 2) lie between the Eurekan Orogen and the Precam- satisfactory restoration of the opposing lands. -
Development of a Pan‐Arctic Monitoring Plan for Polar Bears Background Paper
CAFF Monitoring Series Report No. 1 January 2011 DEVELOPMENT OF A PAN‐ARCTIC MONITORING PLAN FOR POLAR BEARS BACKGROUND PAPER Dag Vongraven and Elizabeth Peacock ARCTIC COUNCIL DEVELOPMENT OF A PAN‐ARCTIC MONITORING PLAN FOR POLAR BEARS Acknowledgements BACKGROUND PAPER The Conservation of Arctic Flora and Fauna (CAFF) is a Working Group of the Arctic Council. Author Dag Vongraven Table of Contents CAFF Designated Agencies: Norwegian Polar Institute Foreword • Directorate for Nature Management, Trondheim, Norway Elizabeth Peacock • Environment Canada, Ottawa, Canada US Geological Survey, 1. Introduction Alaska Science Center • Faroese Museum of Natural History, Tórshavn, Faroe Islands (Kingdom of Denmark) 1 1.1 Project objectives 2 • Finnish Ministry of the Environment, Helsinki, Finland Editing and layout 1.2 Definition of monitoring 2 • Icelandic Institute of Natural History, Reykjavik, Iceland Tom Barry 1.3 Adaptive management/implementation 2 • The Ministry of Domestic Affairs, Nature and Environment, Greenland 2. Review of biology and natural history • Russian Federation Ministry of Natural Resources, Moscow, Russia 2.1 Reproductive and vital rates 3 2.2 Movement/migrations 4 • Swedish Environmental Protection Agency, Stockholm, Sweden 2.3 Diet 4 • United States Department of the Interior, Fish and Wildlife Service, Anchorage, Alaska 2.4 Diseases, parasites and pathogens 4 CAFF Permanent Participant Organizations: 3. Polar bear subpopulations • Aleut International Association (AIA) 3.1 Distribution 5 • Arctic Athabaskan Council (AAC) 3.2 Subpopulations/management units 5 • Gwich’in Council International (GCI) 3.3 Presently delineated populations 5 3.3.1 Arctic Basin (AB) 5 • Inuit Circumpolar Conference (ICC) – Greenland, Alaska and Canada 3.3.2 Baffin Bay (BB) 6 • Russian Indigenous Peoples of the North (RAIPON) 3.3.3 Barents Sea (BS) 7 3.3.4 Chukchi Sea (CS) 7 • Saami Council 3.3.5 Davis Strait (DS) 8 This publication should be cited as: 3.3.6 East Greenland (EG) 8 Vongraven, D and Peacock, E. -
Polar Bears Have Not Been Harmed by Sea Ice Declines in Summer – the Evidence August 18, 2013 Dr
Polar bears have not been harmed by sea ice declines in summer – the evidence August 18, 2013 Dr. S. J. Crockford Http://www.polarbearscience.com Polar bears have not been harmed by sea ice declines in summer – the evidence The polar bear biologists and professional activists of the IUCN Polar Bear Specialist Group (PBSG) continue to insist that since 1979 increasingly smaller amounts of Arctic sea ice left at the end of summer (the the September ice minimum) have already caused harm to polar bears. They contend that global warming due to CO2 from fossil fuels (“climate warming” in their lexicon) is the cause of this decline in summer ice. In a recent (2012) paper published in the journal Global Change Biology (“Effects of climate warming on polar bears: a review of the evidence”), long-time Canadian PBSG members Ian Stirling and Andrew Derocher (both of University of Alberta) summarized their position this way: “Climate warming is causing unidirectional changes to annual patterns of sea ice distribution, structure, and freeze-up. We summarize evidence that documents how loss of sea ice, the primary habitat of polar bears (Ursus maritimus), negatively affects their long-term survival” I’ve spent the last year examining their evidence of on-going harm, but in addition, I’ve looked at the evidence (much of it not mentioned in the Stirling and Derocher paper1) that polar bears have either not been harmed by less sea ice in summer or have thrived in spite of it. This is a summary of my findings. I have provided links to my original essays on individual topics, (available online at www.polarbearscience.com), which are fully referenced and illustrated. -
Wendy Calvert and Ian Stirling Source: Bears: Their Biology and Management, Vol
Interactions between Polar Bears and Overwintering Walruses in the Central Canadian High Arctic Author(s): Wendy Calvert and Ian Stirling Source: Bears: Their Biology and Management, Vol. 8, A Selection of Papers from the Eighth International Conference on Bear Research and Management, Victoria, British Columbia, Canada, February 1989 (1990), pp. 351-356 Published by: International Association of Bear Research and Management Stable URL: http://www.jstor.org/stable/3872939 Accessed: 03/01/2009 20:40 Your use of the JSTOR archive indicates your acceptance of JSTOR's Terms and Conditions of Use, available at http://www.jstor.org/page/info/about/policies/terms.jsp. JSTOR's Terms and Conditions of Use provides, in part, that unless you have obtained prior permission, you may not download an entire issue of a journal or multiple copies of articles, and you may use content in the JSTOR archive only for your personal, non-commercial use. Please contact the publisher regarding any further use of this work. Publisher contact information may be obtained at http://www.jstor.org/action/showPublisher?publisherCode=iba. Each copy of any part of a JSTOR transmission must contain the same copyright notice that appears on the screen or printed page of such transmission. JSTOR is a not-for-profit organization founded in 1995 to build trusted digital archives for scholarship. We work with the scholarly community to preserve their work and the materials they rely upon, and to build a common research platform that promotes the discovery and use of these resources. For more information about JSTOR, please contact [email protected]. -
Atlantic Walrus Odobenus Rosmarus Rosmarus
COSEWIC Assessment and Update Status Report on the Atlantic Walrus Odobenus rosmarus rosmarus in Canada SPECIAL CONCERN 2006 COSEWIC COSEPAC COMMITTEE ON THE STATUS OF COMITÉ SUR LA SITUATION ENDANGERED WILDLIFE DES ESPÈCES EN PÉRIL IN CANADA AU CANADA COSEWIC status reports are working documents used in assigning the status of wildlife species suspected of being at risk. This report may be cited as follows: COSEWIC 2006. COSEWIC assessment and update status report on the Atlantic walrus Odobenus rosmarus rosmarus in Canada. Committee on the Status of Endangered Wildlife in Canada. Ottawa. ix + 65 pp. (www.sararegistry.gc.ca/status/status_e.cfm). Previous reports: COSEWIC 2000. COSEWIC assessment and status report on the Atlantic walrus Odobenus rosmarus rosmarus (Northwest Atlantic Population and Eastern Arctic Population) in Canada. Committee on the Status of Endangered Wildlife in Canada. Ottawa. vi + 23 pp. (www.sararegistry.gc.ca/status/status_e.cfm). Richard, P. 1987. COSEWIC status report on the Atlantic walrus Odobenus rosmarus rosmarus (Northwest Atlantic Population and Eastern Arctic Population) in Canada. Committee on the Status of Endangered Wildlife in Canada. Ottawa. 1-23 pp. Production note: COSEWIC would like to acknowledge D.B. Stewart for writing the status report on the Atlantic Walrus Odobenus rosmarus rosmarus in Canada, prepared under contract with Environment Canada, overseen and edited by Andrew Trites, Co-chair, COSEWIC Marine Mammals Species Specialist Subcommittee. For additional copies contact: COSEWIC Secretariat c/o Canadian Wildlife Service Environment Canada Ottawa, ON K1A 0H3 Tel.: (819) 997-4991 / (819) 953-3215 Fax: (819) 994-3684 E-mail: COSEWIC/[email protected] http://www.cosewic.gc.ca Également disponible en français sous le titre Évaluation et Rapport de situation du COSEPAC sur la situation du morse de l'Atlantique (Odobenus rosmarus rosmarus) au Canada – Mise à jour. -
Canadian Arctic Tide Measurement Techniques and Results
International Hydrographie Review, Monaco, LXIII (2), July 1986 CANADIAN ARCTIC TIDE MEASUREMENT TECHNIQUES AND RESULTS by B.J. TAIT, S.T. GRANT, D. St.-JACQUES and F. STEPHENSON (*) ABSTRACT About 10 years ago the Canadian Hydrographic Service recognized the need for a planned approach to completing tide and current surveys of the Canadian Arctic Archipelago in order to meet the requirements of marine shipping and construction industries as well as the needs of environmental studies related to resource development. Therefore, a program of tidal surveys was begun which has resulted in a data base of tidal records covering most of the Archipelago. In this paper the problems faced by tidal surveyors and others working in the harsh Arctic environment are described and the variety of equipment and techniques developed for short, medium and long-term deployments are reported. The tidal characteris tics throughout the Archipelago, determined primarily from these surveys, are briefly summarized. It was also recognized that there would be a need for real time tidal data by engineers, surveyors and mariners. Since the existing permanent tide gauges in the Arctic do not have this capability, a project was started in the early 1980’s to develop and construct a new permanent gauging system. The first of these gauges was constructed during the summer of 1985 and is described. INTRODUCTION The Canadian Arctic Archipelago shown in Figure 1 is a large group of islands north of the mainland of Canada bounded on the west by the Beaufort Sea, on the north by the Arctic Ocean and on the east by Davis Strait, Baffin Bay and Greenland and split through the middle by Parry Channel which constitutes most of the famous North West Passage. -
STEPPING BACK from the DANGER ZONE Conlt4h~-J ------SPRING 2009 No
Spring 2009 No. 62 $5US $6CAN A HARSH NE~ REALITY TRANSFORMS THE ARCTIC REINVENTING WHAT IT MEANS TO BE INUIT S SSED OUT WILDLIFE FACE MASSIVE OIL DEVELO - STEPPING BACK FROM THE DANGER ZONE Conlt4H~-j --------------- SPRING 2009 No. 62 Dear Reader ARCTIC he facts aboutthe recent warming A HARSH NEW REALITY TRANSFORMS THE ARCTIC 3 "DRILL, BABY, DRILL: STRESSED OUT ARCTIC WILDLIFE FACE MAS- of Earth's north pole, as described SIVE NEW OIL DEVELOPMENT .•••••....•.••......••..•. 14 Tin chis issue of Cascadia Times, are ,_THE ARCT1C0S DISAPPEARING SEA ICE 3 truly frightening. Journalists who report • THE WALRUS' FATAL REACTION TO GLOBAL WARMING •........ 16 the facts about global warming arc often ARCTIC WARMING "DRAMATIC" AND "WIDESPREAD" 4 accused of fear-mongering, as if reporciing INCREASED INTEREST IN ARCTIC SHIPPING ROUTES POSES NEW the facts about climate change is some• how a crime. It would be a crime not to ARCTIC TEMPERATURES RISING TWICE THE RATE AS THE ENTIRE RISKS TO FRAGILE ECOSYSTEMS ....••••....•....••..... 19 do so. PLANET ..••.•............•......•................ 5 We also believe chat it is much worse SOLUTIONS: STEPPING BACK FROM THE DANGER ZONE •...... 20 to deny· the truth about these facts. REINVENTING WHAT IT MEANS TO BE·INUIT: INDIGENOUS PEOPLES Global warming is not just a theory. It is ADAPT TO CLIMATE CHANGE . • . • . 10 UNPRECEDENTED COMMERCIAL FISHING BAN SEEN AS BIG STEP already happening. TOWARD CONSERVATION OF THE ARCTIC ..•••..•.......... 22 What frightens us most is that global POSIER THE ARCTIC~W HERE POLAR BEARS. OILDRILLERS MEET .• 11 warming is arriving with unexpected REFERENCES .................••.•.••.•.....•..... 23 speed and ferocity. The United Nations RUSSIAN OIL FIELDS COLLIDE WITH REINDEER HERDING TRADnlONS .12 lncernacional Panel on Climate Change, has underestimated global warming. -
Qikiqtani Region
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