Canada's Remote Arctic
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Department of Environment– Wildlife Division
Department of Environment– Wildlife Division Wildlife Research Section Department of Environment Box 209 Igloolik, NU X0A 0L0 Tel: (867) 934-2179 Fax: (867) 934-2190 Email: [email protected] Frequently Asked Questions Government of Nunavut 1. What is the role of the GN in issuing wildlife research permits? On June 1, 1999, Nunavut became Canada’s newest territory. Since its creation, interest in studying its natural resources has steadily risen. Human demands on animals and plants can leave them vulnerable, and wildlife research permits allow the Department to keep records of what, and how much research is going on in Nunavut, and to use this as a tool to assist in the conservation of its resources. The four primary purposes of research in Nunavut are: a. To help ensure that communities are informed of scientific research in and around their communities; b. To maintain a centralized knowledgebase of research activities in Nunavut; c. To ensure that there are no conflicting or competing research activities in Nunavut; and d. To ensure that wildlife research activities abide by various laws and regulations governing the treatment and management of wildlife and wildlife habitat in Nunavut. 2. How is this process supported by the Nunavut Land Claims Agreement? Conservation: Article 5.1.5 The principles of conservation are: a. the maintenance of the natural balance of ecological systems within the Nunavut Settlement Area; b. the protection of wildlife habitat; c. the maintenance of vital, healthy, wildlife populations capable of sustaining harvesting needs as defined in this article; and d. the restoration and revitalization of depleted populations of wildlife and wildlife habitat. -
15 Canadian High Arctic-North Greenland
15/18: LME FACTSHEET SERIES CANADIAN HIGH ARCTIC-NORTH GREENLAND LME tic LMEs Arc CANADIAN HIGH ARCTIC-NORTH GREENLAND LME MAP 18 of Central Map Arctic Ocean LME North Pole Ellesmere Island Iceland Greenland 15 "1 ARCTIC LMEs Large ! Marine Ecosystems (LMEs) are defined as regions of work of the ArcNc Council in developing and promoNng the ocean space of 200,000 km² or greater, that encompass Ecosystem Approach to management of the ArcNc marine coastal areas from river basins and estuaries to the outer environment. margins of a conNnental shelf or the seaward extent of a predominant coastal current. LMEs are defined by ecological Joint EA Expert group criteria, including bathymetry, hydrography, producNvity, and PAME established an Ecosystem Approach to Management tropically linked populaNons. PAME developed a map expert group in 2011 with the parNcipaNon of other ArcNc delineaNng 17 ArcNc Large Marine Ecosystems (ArcNc LME's) Council working groups (AMAP, CAFF and SDWG). This joint in the marine waters of the ArcNc and adjacent seas in 2006. Ecosystem Approach Expert Group (EA-EG) has developed a In a consultaNve process including agencies of ArcNc Council framework for EA implementaNon where the first step is member states and other ArcNc Council working groups, the idenNficaNon of the ecosystem to be managed. IdenNfying ArcNc LME map was revised in 2012 to include 18 ArcNc the ArcNc LMEs represents this first step. LMEs. This is the current map of ArcNc LMEs used in the This factsheet is one of 18 in a series of the ArcCc LMEs. OVERVIEW: CANADIAN HIGH ARCTIC-NORTH GREENLAND LME The Canadian High Arcc-North Greenland LME (CAA) consists of the northernmost and high arcc part of Canada along with the adjacent part of North Greenland. -
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. -
Wolf-Sightings on the Canadian Arctic Islands FRANK L
ARCTIC VOL. 48, NO.4 (DECEMBER 1995) P. 313–323 Wolf-Sightings on the Canadian Arctic Islands FRANK L. MILLER1 and FRANCES D. REINTJES1 (Received 6 April 1994; accepted in revised form 13 March 1995) ABSTRACT. A wolf-sighting questionnaire was sent to 201 arctic field researchers from many disciplines to solicit information on observations of wolves (Canis lupus spp.) made by field parties on Canadian Arctic Islands. Useable responses were obtained for 24 of the 25 years between 1967 and 1991. Respondents reported 373 observations, involving 1203 wolf-sightings. Of these, 688 wolves in 234 observations were judged to be different individuals; the remaining 515 wolf-sightings in 139 observations were believed to be repeated observations of 167 of those 688 wolves. The reported wolf-sightings were obtained from 1953 field-weeks spent on 18 of 36 Arctic Islands reported on: no wolves were seen on the other 18 islands during an additional 186 field-weeks. Airborne observers made 24% of all wolf-sightings, 266 wolves in 48 packs and 28 single wolves. Respondents reported seeing 572 different wolves in 118 separate packs and 116 single wolves. Pack sizes averaged 4.8 ± 0.28 SE and ranged from 2 to 15 wolves. Sixty-three wolf pups were seen in 16 packs, with a mean of 3.9 ± 2.24 SD and a range of 1–10 pups per pack. Most (81%) of the different wolves were seen on the Queen Elizabeth Islands. Respondents annually averaged 10.9 observations of wolves ·100 field-weeks-1 and saw on average 32.2 wolves·100 field-weeks-1· yr -1 between 1967 and 1991. -
ESTIMATING PEARY CARIBOU (Rangifer Tarandus Pearyi) and MUSKOX (Ovibos Moschatus) NUMBERS, COMPOSITION and DISTRIBUTIONS on the HIGH ARCTIC ISLANDS of NUNAVUT
ESTIMATING PEARY CARIBOU (Rangifer tarandus pearyi) AND MUSKOX (Ovibos moschatus) NUMBERS, COMPOSITION AND DISTRIBUTIONS ON THE HIGH ARCTIC ISLANDS OF NUNAVUT Mitch Campbell1 1Regional Wildlife Biologist, Department of Environment, Government of Nunavut, P.O. Box 120, Arviat, NU X0C 0E0 2006 Status Report, No. 19 Campbell, M. 2006. Estimating Peary caribou (Rangifer tarandus pearyi) and muskox (Ovibos moschatus) numbers, composition and distributions on Ellesmere Island, Nunavut. Government of Nunavut, Department of Environment, Status report: 19, Iqaluit, 12 pp. SUMMARY REPORT TO NUNAVUT CO-MANAGERS Prepared By: Mitch W. Campbell Regional Biologist Department of Environment Wildlife Research Division P.O. 120 Arviat, Nu X0C 0E0 Ph: (867)857-2828 Fax: (867)857-2986 E-mail: [email protected] June 15th, 2006 Title: Estimating Peary Caribou (Rangifer tarandus pearyi) and Muskox (Ovibos moschatus) Numbers, Composition and Distributions on Ellesmere Island, Nunavut. Summary: The scientific study of Peary caribou and Muskox on Nunavut’s high arctic islands has been ongoing since May 2000. The data collected thus far on West Devon Island, Bathurst Island and Ellesmere Island are being analyzed and archived. The resulting file report will include a history of scientific study of Peary Caribou, the methods used during these studies, the population estimates of all surveys up to and including the 2006 Ellesmere survey, an analysis of satellite collar movement data, a resource selection analysis examining Peary caribou habitat, a summary of IQ collected by GN Biologists and a in-depth section pulling all aspects of the report into comprehensive management recommendations for the future study and continued co-management of Peary Caribou in Nunavut. -
POLYNYAS in the CANADIAN ARCTIC Analysis of MODIS Sea Ice Temperature Data Between June 2002 and July 2013
Canatec Associates International Ltd. POLYNYAS IN THE CANADIAN ARCTIC Analysis of MODIS Sea Ice Temperature Data Between June 2002 and July 2013 David Currie 7/16/2014 Using daily sea ice temperature grids produced from MODIS optical satellite imagery, polynya occurrences in the Canadian Arctic and Northwest Greenland were mapped with a spatial resolution of one square kilometer and a temporal resolution of one week. The eleven year dataset was used to identify and measure locations with a high probability of open water occurrence. This approach appears to be most suitable for the spring months, when polynyas and shore leads represent the only open water in the region. An analysis of the results at several geographic scales reveals considerable yearly variation in polynya extents, although the relatively short period studied makes identifying trends rather difficult. Contents Introduction ................................................................................................................................................................ 3 Goals ............................................................................................................................................................................... 5 Source Data ................................................................................................................................................................. 6 MODIS Sea Ice Temperature Product MOD29/MYD29 ....................................................................... 6 Landsat Quicklook -
Uria Lomvia) and Black-Legged Kittiwakes (Rissa Tridactyla
A First Count of Thick-billed Murres ( Uria lomvia ) and Black-legged Kittiwakes ( Rissa tridactyla ) Breeding on Bylot Island ANTHONY J. G ASTON 1, 4 , MARC -A NDRÉ CYR 2, and KIERAN O’D ONOVAN 3 1Science and Technology Branch, Environment and Climate Change Canada, Carleton University, Ottawa, Ontario K1A 0H3 Canada 2Canadian Wildlife Service, Environment and Climate Change Canada, Place Vincent Massey, 351 St. Joseph Boulevard, Gatineau, Quebec K1A 0H3 Canada 3308a Klukshu Avenue, Whitehorse, Yukon Y1A 3Y1 Canada 4Corresponding author: [email protected] Gaston, Anthony J., Marc-André Cyr, and Kieran O’Donovan. 2017. A first count of Thick-billed Murres ( Uria lomvia ) and Black-legged Kittiwakes ( Rissa tridactyla ) breeding on Bylot Island. Canadian Field-Naturalist 131(1): 69 –74. https:// doi.org/10.22621/cfn.v 131i 1.1953 Bylot Island, part of Sirmilik National Park, supports two major breeding colonies of intermingled Thick-billed Murres ( Uria lomvia ) and Black-legged Kittiwakes ( Rissa tridactyla ): at Cape Hay near the northwest tip and at Cape Graham Moore at the opposite end of the island. Although the size of these colonies has been estimated previously, there is no information on how the estimates were made, except for Thick-billed Murres at Cape Hay in 1977, when the numbers were based on sampling only about 30% of the colony. In 2013, high-resolution digital photographs of the whole area of both colonies were taken in July, when most birds were probably incubating eggs. Individual birds were counted on the photographs, and the numbers were corrected for image quality and converted to numbers of breeding pairs based on correction factors from another High Arctic colony. -
Polar Continental Shelf Program Science Report 2019: Logistical Support for Leading-Edge Scientific Research in Canada and Its Arctic
Polar Continental Shelf Program SCIENCE REPORT 2019 LOGISTICAL SUPPORT FOR LEADING-EDGE SCIENTIFIC RESEARCH IN CANADA AND ITS ARCTIC Polar Continental Shelf Program SCIENCE REPORT 2019 Logistical support for leading-edge scientific research in Canada and its Arctic Polar Continental Shelf Program Science Report 2019: Logistical support for leading-edge scientific research in Canada and its Arctic Contact information Polar Continental Shelf Program Natural Resources Canada 2464 Sheffield Road Ottawa ON K1B 4E5 Canada Tel.: 613-998-8145 Email: [email protected] Website: pcsp.nrcan.gc.ca Cover photographs: (Top) Ready to start fieldwork on Ward Hunt Island in Quttinirpaaq National Park, Nunavut (Bottom) Heading back to camp after a day of sampling in the Qarlikturvik Valley on Bylot Island, Nunavut Photograph contributors (alphabetically) Dan Anthon, Royal Roads University: page 8 (bottom) Lisa Hodgetts, University of Western Ontario: pages 34 (bottom) and 62 Justine E. Benjamin: pages 28 and 29 Scott Lamoureux, Queen’s University: page 17 Joël Bêty, Université du Québec à Rimouski: page 18 (top and bottom) Janice Lang, DRDC/DND: pages 40 and 41 (top and bottom) Maya Bhatia, University of Alberta: pages 14, 49 and 60 Jason Lau, University of Western Ontario: page 34 (top) Canadian Forces Combat Camera, Department of National Defence: page 13 Cyrielle Laurent, Yukon Research Centre: page 48 Hsin Cynthia Chiang, McGill University: pages 2, 8 (background), 9 (top Tanya Lemieux, Natural Resources Canada: page 9 (bottom -
The Breeding Distribution and Current Population Status of the Ivory Gull in Canada V.G
ARCTIC VOL 40, NO. 3 (SEPTEMBER 1987) P. 21 1-218 The Breeding Distribution and Current Population Status of the Ivory Gull in Canada V.G. THOMAS’ and S.D. MACDONALD’ (Received 9 December 1985; accepted in revised form 17 June 1987) ABSTRACT. Aerialsweys were conductedin the eastern CanadianHigh Arctic from 1982 to 1985 to determine the distributionsize and of breeding populations of the ivorygull (Pugophila eburneu).The known Canadian population is confined to Ellesmere,Devon, Seymour, Baffii and Perleyislands. Two major concentrationsof ivory gull coloniesexist, one among the granitic nunataksof southeastern Ellesmere Island andother the on the sedimentary plateaus of the Brodeur Peninsula of Baffii Island. The size of breeding groups varies greatly from4 to over 300 adult gulls. Breeding colonies are typified by their inland, remote and desolate locations and virtual absenceof other animal species. We suggest that is there a single Canadian population of ivory gulls whose adult cohort contains over 2400birds. The small number of leg band recoveries and retrapping of banded birds indicates that individuals can live at least 15 years. One-year-old ivory gulls were notseen at the coloniesor on adjacent waters, andtheir location during summer remains unknown. Key words: ivory gull, Pugophilu eburneu, arctic breeding populations, nunataks, polynyas RÉSUMÉ. On a effectué des relevCs akriens dans la partie est de l’Extrême-Arctique canadien deil 1985 1982 pour établi la distribution et la taille des populations de mouettes blanches (Pugophila eburneu) qui se reproduisent. La population canadienne que l’on connaît habite seulement les îles Ellesmere, Devon, Seymour, Baffin et Perley. I1 y a deux endroits importantsoil se concentrent les coloniesde mouettes blanches, l’une parmi les nunataks granitiquesdu sud-est de l’île Ellesmere,et l’autre sur les plateauxs6dhentaires de la presqu’lleBrodeur dans l’île Baffin. -
Canada's Arctic Marine Atlas
Lincoln Sea Hall Basin MARINE ATLAS ARCTIC CANADA’S GREENLAND Ellesmere Island Kane Basin Nares Strait N nd ansen Sou s d Axel n Sve Heiberg rdr a up Island l Ch ann North CANADA’S s el I Pea Water ry Ch a h nnel Massey t Sou Baffin e Amund nd ISR Boundary b Ringnes Bay Ellef Norwegian Coburg Island Grise Fiord a Ringnes Bay Island ARCTIC MARINE z Island EEZ Boundary Prince i Borden ARCTIC l Island Gustaf E Adolf Sea Maclea Jones n Str OCEAN n ait Sound ATLANTIC e Mackenzie Pe Ball nn antyn King Island y S e trait e S u trait it Devon Wel ATLAS Stra OCEAN Q Prince l Island Clyde River Queens in Bylot Patrick Hazen Byam gt Channel o Island Martin n Island Ch tr. Channel an Pond Inlet S Bathurst nel Qikiqtarjuaq liam A Island Eclipse ust Lancaster Sound in Cornwallis Sound Hecla Ch Fitzwil Island and an Griper nel ait Bay r Resolute t Melville Barrow Strait Arctic Bay S et P l Island r i Kel l n e c n e n Somerset Pangnirtung EEZ Boundary a R M'Clure Strait h Island e C g Baffin Island Brodeur y e r r n Peninsula t a P I Cumberland n Peel Sound l e Sound Viscount Stefansson t Melville Island Sound Prince Labrador of Wales Igloolik Prince Sea it Island Charles ra Hadley Bay Banks St s Island le a Island W Hall Beach f Beaufort o M'Clintock Gulf of Iqaluit e c n Frobisher Bay i Channel Resolution r Boothia Boothia Sea P Island Sachs Franklin Peninsula Committee Foxe Harbour Strait Bay Melville Peninsula Basin Kimmirut Taloyoak N UNAT Minto Inlet Victoria SIA VUT Makkovik Ulukhaktok Kugaaruk Foxe Island Hopedale Liverpool Amundsen Victoria King -
Baffin Fan and Its Inverted Rift System of Arctic Eastern Canada; Is This Another Beaufort-Mackenzie Basin?
Baffin Fan and its inverted rift system of Arctic eastern Canada; is this another Beaufort-Mackenzie Basin? Christopher Harrison* Geological Survey of Canada, 615 Booth St., Ottawa, ON, K1A 0E9, Canada e-mail: [email protected] Thomas A. Brent Geological Survey of Canada, 3303-33rd St. NW, Calgary, AB, T2L 2A7, Canada and Gordon N. Oakey Geological Survey of Canada, 1 Challenger Dr., Dartmouth, NS, B2Y 4A2, Canada. Summary Baffin Fan is a twelve km thick sedimentary wedge of Eocene to Pleistocene age in northwestern Baffin Bay; size and resource potential comparable to Beaufort-Mackenzie Basin (Figure 1). Notable is syntectonic sedimentation with possible volcanism and rifting in the Cretaceous-Danian. Sequences associated with inversion in the later Paleocene and Eocene display out-of-graben thrust anticlines formed over horst blocks in Lady Ann and Lancaster Sound basins. The Oligocene to mid-Miocene is associated with fluvial-deltaic systems; replaced since then by glacial-interglacial sequences including submarine canyons and deep-water fans. Exploration targets are located in Lancaster Sound, and a Baffin Bay fairway that runs 220 km northwestward to east of Coburg Island. Sixty-five percent of prospects are located under Neogene cover. Fourteen are each greater than 70 km2, and five are between 334 and 592 km2. Based on drilling success rates elsewhere and the existence of a petroleum system, 12 of the 40 mapped structures may contain hydrocarbons in significant quantity. Introduction Emerging areas for offshore exploration in Arctic eastern Canada are located on the continental margins of Labrador Sea and Baffin Bay, and in the fault-controlled grabens that underlie some of the larger bays and the entrances to several major inter-island channels. -
NIRB Uuktuutinga Ihivriuqhikhamut #125443 Prince Leopold Island Migratory Bird Sactuary Permit & Nirjutiqarvik NWA Wildlife Viewing Permit
NIRB Uuktuutinga Ihivriuqhikhamut #125443 Prince Leopold Island Migratory Bird Sactuary Permit & Nirjutiqarvik NWA wildlife viewing permit Uuktuutinga Qanurittuq: Amendment Havaap Qanurittunia: Puulaktunik Takuyaktuiyunik Akuiyunik Aihinit Uuktuutinga Ublua: 1/29/2019 5:24:34 PM Period of operation: from 0001-01-01 to 0001-01-01 Piumayaat Angirutinga: from 0001-01-01 to 0001-01-01 Havauhikhaq Ikayuqtinga: Nansen Weber Canadian Arctic Holidays Ltd. PO 1252 STN MAIN Yellowknife NWT X1A 2n9 Canada Hivayautit Nampanga:: 2503084656, Kayumiktukkut Nampanga:: QANURITTUT Tukihiannaqtunik havaariyauyumayumik uqauhiuyun Qablunaatitut: Number of personnel covered under permit: Maximum 10Project objectives: View the arctic flora and fauna on Prince Leopold Island and Coburg Island with guests from Arctic Watch Wilderness Lodge. Project location: Prince Leopold Island MBS and Nirjutiqarvik NWAPrince Leopold Island MBS (74°N 090°W)Nirjutiqarvik NWA (75°57′N 79°18′W)Please keep in mind that I do not have exact location of the airstrips for both Prince Leopold Island or Coburg Island since I have not visited either. They both have twin-otter landing strips walking distance from the viewpoints we wish to visit. Proposed dates and Duration of Visit:We would like to fly and land a Summit Air Twin-Otter too both Prince Leopold Island and Coburg Island. We will be using the airstrips that are already designated on the islands and then walk to the cliffs and waters edge. No vessel, all-terrain vechiles or helicopters will be used in either location. Proposed dates for visiting both locations are August 2-4, 2019 weather permitting. This is a one-day visit, with an approximate 3-4 hour viewing at each location.