State of the Polar Bear Report 2018
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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. -
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. -
The State of the Polar Bear Report 2020
STATE OF THE POLAR BEAR REPORT 2020 Susan J. Crockford The Global Warming Policy Foundation Report 48 State of the Polar Bear Report 2020 Susan J. Crockford Report 48, The Global Warming Policy Foundation © Copyright 2021, The Global Warming Policy Foundation TheContents Climate Noose: Business, Net Zero and the IPCC's Anticapitalism AboutRupert Darwall the author iv Report 40, The Global Warming Policy Foundation Preface v ISBNExecutive 978-1-9160700-7-3 summary vi 1.© Copyright Introduction 2020, The Global Warming Policy Foundation 1 2. Conservation status 1 3. Population size 2 4. Population trends 10 5. Habitat status 11 6. Prey base 15 7. Health and survival 17 8. Evidence of flexibility 22 9. Human/bear interactions 23 10. Discussion 28 Bibliography 30 About the Global Warming Policy Foundation 58 About the author Dr Susan Crockford is an evolutionary biologist and has been work- ing for more than 40 years in archaeozoology, paleozoology and forensic zoology.1 She is a former adjunct professor at the University of Victoria, British Columbia and works full time for a private con- sulting company she co-owns (Pacific Identifications Inc). She is the author of Rhythms of Life: Thyroid Hormone and the Origin of Species, Eaten: A Novel (a polar bear attack thriller), Polar Bear Facts and Myths (for ages seven and up, also available in French, German, Dutch, and Norwegian), Polar Bears Have Big Feet (for preschoolers), and the fully referenced Polar Bears: Outstanding Survivors of Climate Change and The Polar Bear Catastrophe That Never Happened,2 as well as a scien- tific paper on polar bear conservation status.3 She has authored sev- eral earlier briefing papers, reports, and videos for GWPF on polar bear and walrus ecology and conservation.4 Susan Crockford blogs at www.polarbearscience.com. -
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
Tuktu 399 e Bay Roch 398 elville West M 499 204 el M 12 k lia id 200 3 Ch laq Qi 209 7 6 OVERVIEW 2015 Turqa Aberdeevnik 2, 9 4 NUNAVUT Baker Basin 5 Coats sel and Man Isl y MINERAL EXPLORATION, MINING & GEOSCIENCEand Ba Isl va a ATLAS ga av Un g 13 'Un 120°W 110°W 100°W 90°W 80°W 70°W 60°W 50°W 40°W 30°W ie d A Ba RC TIC O OC CÉ EA AN N 80°W A Y R el C ver T ton Povungnituk IQ B NP U ay aq Bay E irpa ttin QIKIQTANIQu REGION Kiyuk t N 346 DS i 60° a N r A TH t 8 S L E S B s Y I e BA D A r SON H IS a HUD N L ay N A T É dhild B °N L E - Au N 80 B a N N ) E n E SO A s ER UD E K Z N e SM ' H t I I n ELLE AIE D O a R L E S B R a A E o D R u LAN G n n IS ne / u M d ssiz Ka E N A Aga in D N E L ap Bas N t N 80 E ce C li A °N U DE I A l Q la Dobbin L a /D S ninsu Bay N la K E eim Pe E a ÎL 199 Fosh E K R er Princess Marie Bay A uaq P Müll R ikil e an C a Ice Cap G M S E ry AXEL N B C Buch E h anan Bay E 397 U a EIBERG t Q C n H D Inle E n ÎLE ( ig B e her Ha É l ISLAND RE Belc U y ME Q Ba LES ands and 'EL Isl Str d D M n s u ale a o f W s o S ce s n H e Pri ld a e Pri Ellef Ring y efi n n a c c e k I e s S G s Amund e u s o staf Islan u r A d e dol n u f l Ringnes d E Sea S o y u Island a n B d Bay orwegian h N it m Lough S DS eed Cornwall I. -
The Nares 2001 Geoscience Project: an Introduction
Polarforschung 74 (1-3), 1 – 7, 2004 (erschienen 2006) The Nares 2001 Geoscience Project: An Introduction by Ian D. Reid1, H. Ruth Jackson2 and Franz Tessensohn3 Abstract: Nares Strait forms a rather straight set of narrow marine channels Onshore geological evidence, however, implied that no more between Greenland and the Canadian Arctic Islands. Since 1982, the Nares than 25 km of offset had taken place (MAY R & DE VRIES 1982), Strait dilemma forms a classical case of conflict between plate tectonics and regional geology without obvious solution. Plate tectonics postulated a sinis- and this discrepancy has given rise to a long-standing contro- tral continental transform through the strait, whereas regional geological versy. The situation is complicated by the fact that in addition mapping results could not find evidence for the required offsets. Between to the postulated Wegener Fault two more important tectonic 1982 and 2000 new data were gathered in northern Baffin Bay and on either side of the Strait, yet the Strait itself had still not been investigated. We report boundaries are mapped to lie under the waters of the northern on an expedition carried out in 2001 in the previously unexplored water co- part of Nares Strait (Fig. 1). The question: Did Greenland drift vered area. In spite of the difficult ice conditions, we gathered new marine, along Nares Strait? has been argued for more than 90 years, aeromagnetic and geological data relevant to the problem. The results are AWES presented in this volume together with compilations of the related geological and was the subject of a major symposium in 1980 (D & and geophysical data bases. -
Adolphus Washington Greely (1844-1935) Adolphuswashington Greely Became a Worldcelebrity Officer
150 ARCTIC PROFILES Adolphus Washington Greely (1844-1935) AdolphusWashington Greely became a worldcelebrity officer. Here he fell under the spell of Captain Henry W. almost overnight in 1884 when the six survivors of the Lady Howgate, a Signal Service officer who was an enthusiast for Franklin Bay Expedition under his leadership were rescued arctic exploration and who opened his extensivelibrary of arc- from starvation in the Arctic. Yet he was far more than the tic literature to the younger officer. It was through this chain central figure of one tragic expedition. Explorer, soldier, of events that Greely was inspiredto a deep interest in leading scientist, and author, Greely was respected as an international an arctic expedition. He hadseveral motives: to visit a strange authority on polar science from the 1880s until his death 50 and romantic part of the world, to study the physical condi- years later. tions of theFar North, to conduct signaling experiments under Born in Newburyport, Massachusetts, in 1844, Greely vol- severe weather conditions, and also, perhaps, to make a name unteered for Civil War service in the Union Army before he for himself that would help his promotion. was 18. He was grievously wounded at Antietam in 1862, but In October 1879 ai International Polar Conference held in returned to active dutythe following spring as anofficer of the Hamburg agreed ona common program of meteorological and U.S. Colored Infantry, made up of free black soldiers. When otherphysical observations by expeditionssupported by a the war ended he heldthe brevet rank of captainof volunteers dozen countries, all to be placed as far toward the top of the and decided on service in the regular army as his career.