Polar Bear Kills
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Climate in Svalbard 2100
M-1242 | 2018 Climate in Svalbard 2100 – a knowledge base for climate adaptation NCCS report no. 1/2019 Photo: Ketil Isaksen, MET Norway Editors I.Hanssen-Bauer, E.J.Førland, H.Hisdal, S.Mayer, A.B.Sandø, A.Sorteberg CLIMATE IN SVALBARD 2100 CLIMATE IN SVALBARD 2100 Commissioned by Title: Date Climate in Svalbard 2100 January 2019 – a knowledge base for climate adaptation ISSN nr. Rapport nr. 2387-3027 1/2019 Authors Classification Editors: I.Hanssen-Bauer1,12, E.J.Førland1,12, H.Hisdal2,12, Free S.Mayer3,12,13, A.B.Sandø5,13, A.Sorteberg4,13 Clients Authors: M.Adakudlu3,13, J.Andresen2, J.Bakke4,13, S.Beldring2,12, R.Benestad1, W. Bilt4,13, J.Bogen2, C.Borstad6, Norwegian Environment Agency (Miljødirektoratet) K.Breili9, Ø.Breivik1,4, K.Y.Børsheim5,13, H.H.Christiansen6, A.Dobler1, R.Engeset2, R.Frauenfelder7, S.Gerland10, H.M.Gjelten1, J.Gundersen2, K.Isaksen1,12, C.Jaedicke7, H.Kierulf9, J.Kohler10, H.Li2,12, J.Lutz1,12, K.Melvold2,12, Client’s reference 1,12 4,6 2,12 5,8,13 A.Mezghani , F.Nilsen , I.B.Nilsen , J.E.Ø.Nilsen , http://www.miljodirektoratet.no/M1242 O. Pavlova10, O.Ravndal9, B.Risebrobakken3,13, T.Saloranta2, S.Sandven6,8,13, T.V.Schuler6,11, M.J.R.Simpson9, M.Skogen5,13, L.H.Smedsrud4,6,13, M.Sund2, D. Vikhamar-Schuler1,2,12, S.Westermann11, W.K.Wong2,12 Affiliations: See Acknowledgements! Abstract The Norwegian Centre for Climate Services (NCCS) is collaboration between the Norwegian Meteorological In- This report was commissioned by the Norwegian Environment Agency in order to provide basic information for use stitute, the Norwegian Water Resources and Energy Directorate, Norwegian Research Centre and the Bjerknes in climate change adaptation in Svalbard. -
(Late Tertiary) As Seen from Prince Patrick Island, Arctic Canada’ JOHN G
ARCTIC WL. 43, NO. 4 (DECEMBER 1990) P. 393-403 Beaufort Formation (Late Tertiary) as Seen from Prince Patrick Island, Arctic Canada’ JOHN G. FYLES’ (Received 20 March 1990; accepted in revked form 14 June 1990) ABSTRACT. The Beaufort Formation, in its typearea on Prince Patrick Island, is a single lithostratigraphicunit, a few tens of metres thick, consisting of unlithified sandy deposits of braided rivers. Organicbeds in the sand have yielded more than 200 species of plants and insects and probably originated during the Pliocene, when the area supported coniferous forest. ThisBeaufort unit forms the thin eastern edge of a northwest-thickeningwedge of sand and gravel beneath the western part of the island. These largely unexposed beds,up to several hundred metres thick, include the Beaufort unit and perhaps other older or younger deposits.On the islands northeast and southwest of PrincePatrick Island (MeighenIsland to Banks Island),the name BeaufortFormation has been appliedto similar deposits of late Rrtiary age. Most recorded Beaufort beds on these islands are stratigraphically and paleontologically equivalentto the “type” Beaufort, but a few sites that have been called Beaufort (suchas Duck Hawk Bluffsand the lower unit at Ballast Brook,on Banks Island) differ stratigraphicallyand paleontologically from the “type” Beaufort. This paper recommends that these deposits (probably middle Miocene) and others like them be assigned new stratigraphic names and not be included in the Beaufort Formation as now defined. Informal names Mary Sachs gravel (Duck HawkBluffs) and Ballast Brookbeds are proposed as an initial step. Formal use of the name Beaufort Formation shouldrestricted be to the western Arctic Islands. -
Arctic Marine Aviation Transportation
SARA FRENCh, WAlTER AND DuNCAN GORDON FOundation Response CapacityandSustainableDevelopment Arctic Transportation Infrastructure: Transportation Arctic 3-6 December 2012 | Reykjavik, Iceland 3-6 December2012|Reykjavik, Prepared for the Sustainable Development Working Group Prepared fortheSustainableDevelopment Working By InstituteoftheNorth,Anchorage, Alaska,USA PROCEEDINGS: 20 Decem B er 2012 ICElANDIC coast GuARD INSTITuTE OF ThE NORTh INSTITuTE OF ThE NORTh SARA FRENCh, WAlTER AND DuNCAN GORDON FOundation Table of Contents Introduction ................................................................................ 5 Acknowledgments ......................................................................... 6 Abbreviations and Acronyms .......................................................... 7 Executive Summary ....................................................................... 8 Chapters—Workshop Proceedings................................................. 10 1. Current infrastructure and response 2. Current and future activity 3. Infrastructure and investment 4. Infrastructure and sustainable development 5. Conclusions: What’s next? Appendices ................................................................................ 21 A. Arctic vignettes—innovative best practices B. Case studies—showcasing Arctic infrastructure C. Workshop materials 1) Workshop agenda 2) Workshop participants 3) Project-related terminology 4) List of data points and definitions 5) List of Arctic marine and aviation infrastructure AlASkA DepartmENT OF ENvIRONmental -
Long-Distance Migratory Movements and Habitat Selection of Snowy Owls in Nunavut
Long-distance migratory movements and habitat selection of Snowy Owls in Nunavut © Marten Stoffel Jean-François Therrien, Gilles Gauthier Département de biologie & Centre d'études nordiques, Université Laval, Québec Joël Bêty Département de biologie & Centre d’études nordiques, Université du Québec à Rimouski Gary Mouland Parks Canada - Nunavut Field Unit, Iqaluit 29 September 2008 Final report submitted to the Nunavut Wildlife Management Board Project no: # 5-07-01 2 Project no: # 5-07-01 Final report: 30 September 2008 Title Long-distance migratory movements and habitat selection of Snowy Owls in Nunavut. Project Leader Gary Mouland Parks Canada - Nunavut Field Unit, PO Box 278, Iqaluit, NU X0A 0H0 Tel: 867-975-4672; email: [email protected]. Collaborators Jean-François Therrien Department of biology and Centre d’études nordiques, Université Laval, Québec (Québec) G1K 7P4 Tel: 418-656-2131 ext 6327; e-mail: [email protected] Gilles Gauthier Department of biology and Centre d’études nordiques, Université Laval, Québec (Québec) G1K 7P4 Tel: 418-656-5507; e-mail: [email protected] Joël Bêty Department of biology, Université du Québec à Rimouski (UQAR), Rimouski (Québec) G5L 3A1 Tel: 418-656-5507; e-mail: [email protected] Please, do not cite this report without prior consent from the authors Cover picture: This picture of a Snowy Owl marked with a satellite transmitter on Bylot Island in July 2007 was taken in Abernethy, Saskatchewan, on 10 April 2008, 2750 km from the marking site. 3 TABLE OF CONTENT TABLE OF CONTENT .................................................................................................................. 3 LIST OF FIGURES ........................................................................................................................ 5 LIST OF TABLES ......................................................................................................................... -
Spitsbergen-Bear Island
SPITSBERGEN-BEAR ISLAND A voyage to Bear Island and returning to Longyeabyen, in search of seals and bears. The land of the midnight sun, of snow and ice, offers some of the finest scenery and wildlife experiences in the world. Bear Island, or Bjørnøya in Norwegian, is the southernmost island of the Spitsbergen archipelago. ITINERARY Day 1: Departure from Longyearbyen Arrive in Longyearbyen, the administrative capital of the Spitsbergen archipelago of which West Spitsbergen is the largest island. Before embarking there is an opportunity to stroll around this former mining town, whose parish church and Polar Museum are well worth visiting. In the early evening the ship will sail out of Isfjorden. Day 2: Cruising the fjords of Hornshund 01432 507 280 (within UK) [email protected] | small-cruise-ships.com We start the day quietly cruising the side fjords of the amphitheatre of glacier fronts. spectacular Hornsund area of southern Spitsbergen, enjoying the scenery of towering mountain peaks. Hornsundtind rises to Day 7: Stormbukta 1,431m, while Bautaen shows why early Dutch explorers gave If ice conditions allow we will land at Stormbukta with an easily the name ‘Spitsbergen’ - pointed mountains - to the island. accessible Kittiwake colony in a canyon and warm springs, There are also 14 magnificent glaciers in the area and very which do not freeze during winter. Alternatively we land at good chances of encounters with seals and Polar Bear. Palfylodden a Walrus haul out place with the remains of thousands of walruses slaughtered in previous centuries. We Day 3: Hvalrossbukta sail northward along the Spitsbergen banks, looking for Finn At the south side of Bear Island we sail by the largest bird cliffs Whales. -
Update on Polar Bear Research in the Viscount Melville Sound/North Beaufort Polar Bear Subpopulations Spring 2012
Update on Polar Bear research in the Viscount Melville Sound/North Beaufort Polar Bear Subpopulations Spring 2012. This was the first year of a three year mark-recapture program to estimate the current population size of the Viscount Melville Polar Bear Subpopulation. To examine movement patterns and population boundaries, we deployed 14 GPS satellite collars in the Viscount Melville Subpopulation and 15 collars in the North Beaufort Subpopulation; of the latter 15, 5 were deployed north of Norway Island and 10 in the area from Prince of Whales Strait to the mainland. Two field crews were used to conduct research. One field crew worked out of Ulukhaktok. This crew consisted of Andrew Derocher (University of Alberta), Patrick Mislan(University of Alberta), and Kenneth Ehaloak (Ulukhaktok). The second field crew worked from 5 base camps. Three base camps were polar bear cabins located at Wynniatt Bay on Victoria Island, Cape Providence on Melville Island, and near Castel Bay in Aulavik National Park on Banks Island. The two other camps were temporary base camps located at Mould Bay on Prince Patrick Island and Nias Point on Melville Island. The second field crew consisted of a Helicopter pilot (Benedikt Seguro), a helicopter engineer (Scott Hauser) (required due to hrs flown), a research assistant from the community of Ulukhaktok (Peter Ross Klengenberg), Evan Richardson (Environment Canada), and Jodie Pongracz (ENR Inuvik). Research commenced on April 21, 2012 in Wynniatt Bay, Victoria Island and was completed on May 31, 2012 at Polar Bear Cabin on Banks Island. A total of 110 hours were flown in an ASTAR (including ferrying to/from Inuvik). -
Svalbard's Risk of Russian Annexation
The Coldest War: Svalbard's Risk of Russian Annexation The Harvard community has made this article openly available. Please share how this access benefits you. Your story matters Citation Vlasman, Savannah. 2019. The Coldest War: Svalbard's Risk of Russian Annexation. Master's thesis, Harvard Extension School. Citable link http://nrs.harvard.edu/urn-3:HUL.InstRepos:42004069 Terms of Use This article was downloaded from Harvard University’s DASH repository, and is made available under the terms and conditions applicable to Other Posted Material, as set forth at http:// nrs.harvard.edu/urn-3:HUL.InstRepos:dash.current.terms-of- use#LAA The Coldest War: Svalbard’s Risk of Russian Annexation Savannah Vlasman A Thesis In the Field of International Relations for the Degree of Master of Liberal Arts in Extension Studies Harvard University 2018 Savannah Vlasman Copyright 2018 Abstract Svalbard is a remote Norwegian archipelago in the Arctic Ocean, home to the northernmost permanent human settlement. This paper investigates Russia’s imperialistic interest in Svalbard and examines the likelihood of Russia annexing Svalbard in the near future. The examination reveals Svalbard is particularly vulnerable at present due to melting sea ice, rising oil prices, and escalating tension between Russia and the West. Through analyzing the past and present of Svalbard, Russia’s interests in the territory, and the details of the Svalbard Treaty, it became evident that a Russian annexation is plausible if not probable. An assessment of Russia’s actions in annexing Crimea, as well as their legal justifications, reveals that these same arguments could be used in annexing Svalbard. -
2019 Wild Norway & Svalbard Field Report
Wild Norway & Svalbard May 17 - June 2, 2019 SVALBARD ARCHIPELAGO Smeerenburg Magdalenefjorden SPITSBERGEN Longyearbyen Poolepynten Van Mijenfjorden Storfjorden Hornsund Bear Island ARCTIC OCEAN Skarsvaag/ North Cape LOFOTEN ISLANDS Trollfjord Stamsund Tromsø Kjerringøy Reine CLE Røst ARCTIC CIR Husey/Sanna Runde Geirangerfjord Bergen NORWAY Sunday, May 19, 2019 Bergen, Norway / Embark Ocean Adventurer Unusual for Bergen, it was a dry, warm, and sunny weekend when we arrived here to begin our travels in Wild Norway and Svalbard. Bergen experiences only five rain-free days a year, and this exceptional weather was being fully enjoyed by the locals, especially as this was also the Norwegian National Day holiday weekend. We set out on foot early this morning, for a tour of the old wharf-side district of Bryggen with its picturesque and higgledy-piggledy medieval wooden houses, their colorful gables lit up by today’s bright sunshine. Next, we boarded coaches which took us to Troldhaugen, the home of Norwegian composer Edvard Grieg for over 20 years. The hut where he did much of his work still stands on the lakeside at the foot of the garden. We were treated to an excellent piano recital of some of Grieg’s music before we went to lunch. All too soon, it was time to return to Bergen where our home for the next two weeks, the Ocean Adventurer, awaited us. Once settled in our cabins, our Expedition Leader, John Yersin, introduced us to his team of Zodiac drivers and lecturers who would be accompanying us on our journey over the next two weeks. -
Searching for the Effects of Climate Change on Northern Vegetation
Searching for the effects of climate change on northern vegetation Hrafnaþing Náttúrufræðistofnun Íslands Icelandic Institute of Natural History Martha Raynolds 6 April 2011 Photo – M. K. Raynolds Climate Carbon sequestration Vegetation Humans use of Wildlife ecosystems As snow and ice melt, Why Does the Arctic Warm Faster than Lower Latitudes? darker land and ocean More of the extra trapped surfaces absorb more energy goes directly into solar energy. warming rather than into evaporation, because the water is cool. The atmospheric layer that has to warm in order to warm the surface is shallower in the Arctic. As sea ice retreats, solar heat absorbed by the oceans is more easily transferred to the atmosphere. Alterations in atmospheric and oceanic circulation can increase warming. (Arctic Climate Impact Assessment, 2004) Decreasing Arctic sea ice NASA National Snow and Ice Data Center Seasonal trends in surface temperature 1981-2003 Comiso 2003 J. of Climate Projected Change in Growing Season Length by 2070-2090 (minimum temperature greater than OoC Alaska Russia Canada Russia Greenland Scandinavia (Arctic Climate Impact Assessment, 2004) Androsace chamaejasme Rock jasmine a – mosses, liverworts and lichens, b – forbs, c – prostrate dwarf- shrubs, d – non-tussock graminoids, e -hemiprostrate dwarf shrubs, f – erect dwarf shrubs, g – low shrubs, h – tussock graminoids Raynolds et al. 2006 Remote Sensing of Environment Plant physiognomy occurring in different Tundra Bioclimate Subzones • A – mosses, liverworts and lichens with some grasses -
The Rough-Legged Hawk in the American Arctic
THEROUGH-LEGGED HAWK IN THE AMERICANARCTIC GeorgeMiksch Sutton* andDavid F. Parmelee? HE rough-legged hawk (Buteo Zagopus) has often been referred to as a “subarctic” or “HudsonianZone” bird. Peters (193 1) did not mention anyT of the arctic islands in his statement concerning the breeding range of the New World race, B. 1. sanctijohmnis. Taverner (1935) stated that the northern limit of its range seemed “to just touch the southernedge of the arctic islands”. Soper (1928;1946) and Wynne-Edwards (1952) have giveninformation concerning its breeding in southern BaffinIsland. Sutton (1932) reported its breeding on Southampton Island, Porsild (1951) on Victoria and Banks islands, MacDonald (1954) on Prince Patrick Island. Apparentlyit does not range as far north in the eastern American Arctic as in the western. The map in Cade (1955) gives a good idea of its breeding distribution inthe Canadian Arctic Archipelago. Oddly enough, it has neverbeen found in Greenland (Salomonsen, 1950-1). In southern Baffin Island Buteo Z@gopusis widely distributed today. The MacMillan expedition to the southwestern part of the island collected “one specimen and eggs” (Soper, 1928). Soper (Zoc. cit.) collected it at Cape Dorset andsaw it at Amadjuak Bay. Hisrecent comments (Soper, 1946) on the species are: “Breeds sparingly along the south coast from at least Lake Harbour to Foxe Channel. At present it is not known to occur elsewhere on the island.” The northernmost record for Baffin Island is apparently that of Manning (in Bray, 1913), who saw one at Taverner Bay, along the west coast just north of the Arctic Circle, on June 8, 1940. -
Business Opportunities in Greenland Project Overview 2018 2 Business Opportunities in Greenland – Project Overview 2018
BUSINESS OPPORTUNITIES IN GREENLAND PROJECT OVERVIEW 2018 2 BUSINESS OPPORTUNITIES IN GREENLAND – PROJECT OVERVIEW 2018 BUSINESS OPPORTUNITIES IN GREENLAND PROJECT OVERVIEW 2018 Published by the Arctic Cluster of Raw Materials (ACRM) in collaboration with the Confederation of Danish Industry (DI), February 2018 di.dk/english acrm.dk Prepared by Up Front Communication ApS, Managing director Hans Bak UP Front COMMUNICATION APS Up-North ApS, Managing director Martin Schjøtz-Christensen The publication was made possible through the financial support of The Bank of Greenland Edited by Mads Qvist Frederiksen, Head of Secretariat, ACRM Photos: Hans Bak/UP Front Communication ApS: Page 14 and 57. Kalaallit Airports: Page 60. Ivars Silis: Page 56. Kommuneqarfik Sermersooq: Page 45. Mads Pihl/Visit Greenland: Page 4, 6, 41 (bottom) and 42 (bottom). Petter Cohen, Xtravel/Visit Greenland: Page 42 (top). Rebecca Gustafsson/Visit Greenland: Page 41 (top). Print: Kailow Graphic A/S ISBN 978-87-7144-135-2 (print) 250.02.2018 BUSINESS OPPORTUNITIES IN GREENLAND – PROJECT OVERVIEW 2018 3 ARCTIC CLUSTER OF RAW MATERIALS The Arctic Cluster of Raw Materials (ACRM) is established by Greenland Business Asso- ciation (GE), The Confederation of Danish Industry (DI) and the Technical University of Denmark (DTU). The cluster was originally funded by the Danish Industry Foundation (IF). Purpose ACRM is a platform for companies with interests, experience and competences within the extractive industries. ACRM’s main purpose is to strengthen the competitiveness in Greenland and Denmark in the industry and contribute to sustainable growth and employment in both countries. To obtain this goal, ACRM will build up and support busi- ness cooperation, industry consortia and business concepts. -
The Norwegian Fjords, Bear Island & Svalbard
SVALBARDTHE NORWEGIAN FJORDS, BEAR ISLAND & SVALBARD - SPRINGTIME IN SVALBARD - SVALBARD 2 ADVENTURE021 - EXPEDITION SVALBARD POLAR ADVENTURES SINCE 1999 For more than 20 years, we have taken adventurous travellers to the Arctic archipelago of Svalbard. From May to September, our three small expedition ships explore this magnificent wilderness that are home to animals such as the charming walrus, the cute Arctic fox, the endemic Svalbard reindeer and last, but certainly not least, the king of the Arctic – the polar bear. Every expedition with us is unique and our aim is that each passenger will have the trip of a lifetime. When you call our office you will speak to members of staff, whom all have been to Svalbard themselves and can answer all your questions about the big adventure. Sustainability is at the heart of PolarQuest and all trips are climate compensated. Welcome on board! SMALL EXPEDITION SHIPS – GREAT MOMENTS Our expedition ships are comfortable, carry only 12 or 53 passengers and when you travel through Svalbard’s untamed wilderness as the exact route offer a completely different experience compared to a larger ship. We can depends on weather, ice conditions and wildlife encounters. Sometimes you reach some of the most inaccessible areas, all passengers can go ashore might be woken up in the middle of the bright night if a polar bear has been at the same time and we can maximise the time to ensure that you get the spotted on the ice or a whale in front of the ship. Below, please find our most out of your trip.