The Northwest Passage Opens for Bowhead Whales
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Highs and Lows: Height Changes in the Ice Sheets Mapped EGU Press Release on Research Published in the Cryosphere
15 Highs and lows: height changes in the ice sheets mapped EGU press release on research published in The Cryosphere Researchers from the Alfred Wegener Institute in Germany have used satellite data to map elevation and elevation changes in both Greenland and Antarctica. The new maps are the most complete published to date, from a single satellite mission. They also show the ice sheets are losing volume at an unprecedented rate of about 500 cubic kilometres per year. The results are now published in The Cryosphere, an open access journal of the European Geosciences Union (EGU). “The new elevation maps are snapshots of the current state of the ice sheets,” says lead-author Veit Helm of the Alfred Wegener Insti- tute, Helmholtz Centre for Polar and Marine Research (AWI), in Bremerhaven, Germany. The snapshots are very accurate, to just a few metres in height, and cover close to 16 million km2 of the area of the ice sheets. “This is 500,000 square kilometres more than any previous elevation model from altimetry – about the size of Spain.” Satellite altimetry missions measure height by bouncing radar New elevation model of Greenland derived from CryoSat-2. More elevation and elevation change maps are available online. (Credit: Helm et al., The Cryo- or laser pulses off the surface of the ice sheets and surrounding sphere, 2014) water. The team derived the maps, which show how height differs across each of the ice sheets, using just over a year’s worth of data collected in 2012 by the altimeter on board the European Space authors. -
Northwest Passage Trail
Nunavut Parks & Special Places – Editorial Series January, 2008 NorThwesT Passage Trail The small Nunavut community of Gjoa Haven Back in the late eighteenth and nineteenth is located on King William Island, right on the centuries, a huge effort was put forth by historic Northwest Passage and home to the Europeans to locate a passage across northern Northwest Passage Trail which meanders within North America to connect the European nations the community, all within easy walking distance with the riches of the Orient. From the east, many from the hotel. A series of signs, a printed guide, ships entered Hudson Bay and Lancaster Sound, and a display of artifacts in the hamlet office mapping the routes and seeking a way through interpret the local Inuit culture, exploration of the ice-choked waters and narrow channels to the the Northwest Passage, and the story of the Gjoa Pacific Ocean and straight sailing to the oriental and Roald Amundsen. It is quite an experience lands and profitable trading. The only other to walk the shores of history here, learning of routes were perilous – rounding Cape Horn at the exploration of the North, and the lives of the the southern tip of South America or the Cape of people who helped the explorers. Good Hope at the southern end of Africa. As a result, many expeditions were launched to seek a passage through the arctic archipelago. Aussi disponible en français xgw8Ns7uJ5 wk5tg5 Pilaaktut Inuinaqtut ᑲᔾᔮᓇᖅᑐᖅ k a t j a q n a a q listen to the land aliannaktuk en osmose avec la terre Through the efforts of the Royal Navy, and WANDER THROUGH HISTORY Lady Jane Franklin, John Franklin’s wife, At the Northwest Passage Trail in the at least 29 expeditions were launched to community of Gjoa Haven, visitors can, seek Franklin and his men, or evidence of through illustrations and text on interpretive their fate. -
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. -
Transits of the Northwest Passage to End of the 2020 Navigation Season Atlantic Ocean ↔ Arctic Ocean ↔ Pacific Ocean
TRANSITS OF THE NORTHWEST PASSAGE TO END OF THE 2020 NAVIGATION SEASON ATLANTIC OCEAN ↔ ARCTIC OCEAN ↔ PACIFIC OCEAN R. K. Headland and colleagues 7 April 2021 Scott Polar Research Institute, University of Cambridge, Lensfield Road, Cambridge, United Kingdom, CB2 1ER. <[email protected]> The earliest traverse of the Northwest Passage was completed in 1853 starting in the Pacific Ocean to reach the Atlantic Oceam, but used sledges over the sea ice of the central part of Parry Channel. Subsequently the following 319 complete maritime transits of the Northwest Passage have been made to the end of the 2020 navigation season, before winter began and the passage froze. These transits proceed to or from the Atlantic Ocean (Labrador Sea) in or out of the eastern approaches to the Canadian Arctic archipelago (Lancaster Sound or Foxe Basin) then the western approaches (McClure Strait or Amundsen Gulf), across the Beaufort Sea and Chukchi Sea of the Arctic Ocean, through the Bering Strait, from or to the Bering Sea of the Pacific Ocean. The Arctic Circle is crossed near the beginning and the end of all transits except those to or from the central or northern coast of west Greenland. The routes and directions are indicated. Details of submarine transits are not included because only two have been reported (1960 USS Sea Dragon, Capt. George Peabody Steele, westbound on route 1 and 1962 USS Skate, Capt. Joseph Lawrence Skoog, eastbound on route 1). Seven routes have been used for transits of the Northwest Passage with some minor variations (for example through Pond Inlet and Navy Board Inlet) and two composite courses in summers when ice was minimal (marked ‘cp’). -
Erik the Red's Land
In May this year, a Briton named Alex Hartley gamely claimed as his personal territory a tiny island in Sval- bard that had been revealed by retreating ice. Sval bard’s islands have a long history of claims and counter-claims by adventurers of diverse nations: the question of who owns the Arctic is an old one. In this next article in our unreviewed biographical/historical series, Frode Skarstein describes Norway’s bid to wrest a corner of Greenland from the Danish crown 75 years ago. Erik the Red’s Land: the land that never was Frode Skarstein Norwegian Polar Institute, Polar Environmental Centre, NO-9296 Tromsø, Norway, [email protected]. “Saturday, 27th of June, 1931. Eventful day. A long coded telegram late last night that I deciphered during the night. At fi ve pm we hoisted the fl ag and occupied the land from Calsbergfjord to Besselsfjord. It will be exciting to see how it develops.” (Devold 1931: author’s translation.) Although not as pithy as the Unity’s log entry from 1616—“Cape Hoorn in 57° 48' S. Rounded 8 p.m.”—when the southern tip of the Americas was fi rst rounded (Hough 1971), the above diary entry by Hallvard Devold is still a salient understatement given the context in which it was made. The next day Devold sent the following telegram to a select few Norwegian newspapers: “In the presence of Eiliv Herdal, Tor Halle, Ingvald Strøm and Søren Rich- ter, the Norwegian fl ag has been hoisted today in Myggbukta. And the land between Carls berg fjord to the south and Bessel fjord to the north occupied in His Pawns in their game: Devold (left) and fellow expe di tion mem bers during the Majesty King Haakon’s name. -
Thermodynamic and Dynamic Ice Thickness Contributions in the Canadian Arctic Archipelago in NEMO-LIM2 Numerical Simulations
The Cryosphere, 12, 1233–1247, 2018 https://doi.org/10.5194/tc-12-1233-2018 © Author(s) 2018. This work is distributed under the Creative Commons Attribution 4.0 License. Thermodynamic and dynamic ice thickness contributions in the Canadian Arctic Archipelago in NEMO-LIM2 numerical simulations Xianmin Hu1,a, Jingfan Sun1,b, Ting On Chan1,c, and Paul G. Myers1 1Department of Earth and Atmospheric Sciences, University of Alberta, Edmonton, T6G 2E3, Canada anow at: Bedford Institute of Oceanography, Fisheries and Oceans Canada, Dartmouth, Nova Scotia, Canada bnow at: School of Electrical and Computer Engineering, Georgia Institute of Technology, Atlanta, GA, USA cnow at: Skytech Solutions Ltd., Canada Correspondence: Xianmin Hu ([email protected]) Received: 6 September 2017 – Discussion started: 10 October 2017 Revised: 16 March 2018 – Accepted: 19 March 2018 – Published: 10 April 2018 Abstract. Sea ice thickness evolution within the Canadian is found in the northern CAA and Baffin Bay while a de- Arctic Archipelago (CAA) is of great interest to science, as cline (r2 ≈ 0:6, p < 0:01) is simulated in Parry Channel re- well as local communities and their economy. In this study, gion. The two main contributors (thermodynamic growth and based on the NEMO numerical framework including the lateral transport) have high interannual variabilities which LIM2 sea ice module, simulations at both 1=4 and 1=12◦ hor- largely balance each other, so that maximum ice volume can izontal resolution were conducted from 2002 to 2016. The vary interannually by ±12 % in the northern CAA, ±15 % in model captures well the general spatial distribution of ice Parry Channel, and ±9 % in Baffin Bay. -
Canada's Sovereignty Over the Northwest Passage
Michigan Journal of International Law Volume 10 Issue 2 1989 Canada's Sovereignty Over the Northwest Passage Donat Pharand University of Ottawa Follow this and additional works at: https://repository.law.umich.edu/mjil Part of the International Law Commons, and the Law of the Sea Commons Recommended Citation Donat Pharand, Canada's Sovereignty Over the Northwest Passage, 10 MICH. J. INT'L L. 653 (1989). Available at: https://repository.law.umich.edu/mjil/vol10/iss2/10 This Article is brought to you for free and open access by the Michigan Journal of International Law at University of Michigan Law School Scholarship Repository. It has been accepted for inclusion in Michigan Journal of International Law by an authorized editor of University of Michigan Law School Scholarship Repository. For more information, please contact [email protected]. CANADA'S SOVEREIGNTY OVER THE NORTHWEST PASSAGE Donat Pharand* In 1968, when this writer published "Innocent Passage in the Arc- tic,"' Canada had yet to assert its sovereignty over the Northwest Pas- sage. It has since done so by establishing, in 1985, straight baselines around the whole of its Arctic Archipelago. In August of that year, the U. S. Coast Guard vessel PolarSea made a transit of the North- west Passage on its voyage from Thule, Greenland, to the Chukchi Sea (see Route 1 on Figure 1). Having been notified of the impending transit, Canada informed the United States that it considered all the waters of the Canadian Arctic Archipelago as historic internal waters and that a request for authorization to transit the Northwest Passage would be necessary. -
Arctic Passage 1 the Northwest Passage Is the Sea Route Linking the Atlantic and Pacific Oceans
Original broadcast: February 28, 2006 BEFORE WATCHING Arctic Passage 1 The Northwest Passage is the sea route linking the Atlantic and Pacific Oceans. The Franklin Expedition traveled from England PROGRAM OVERVIEW to western Greenland through what NOVA recreates the expeditions of Sir is now Baffin Bay, then on to Resolute Island. Some believe the John Franklin and Roald Amundsen, crew made it as far as King William two Arctic explorers who set out to Island. Have students plot the fi nd the legendary Arctic sea route Northwest Passage on a map known as the Northwest Passage. and estimate its distance. 2 Organize the class into five teams. Hour one of the program: As they watch the program, have • tells how Sir John Franklin and his British Admiralty crew of 128 men four of the teams track one of the set out in May of 1845 with two ships to fi nd the mythical route following types of evidence related to why the expedition failed: connecting the Atlantic and Pacifi c Oceans. diseases, health issues and physical • notes the food and other provisions brought on the journey. remains; ship-related artifacts; Inuit • presents the types of evidence that historians relied on to determine testimony; and written notes and what happened to the expedition—artifacts that included a written journals. Have a fifth group keep track of when events occurred. note, ice core data, interviews with Inuit, and forensic analysis of body remains. • pieces together an account of where expedition members traveled and how they may have died. AFTER WATCHING • explains how Franklin and 20 percent of his crew died two years into 1 Have students refer to their notes the expedition; the fi nal four crew members died after six years on the ice. -
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. -
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. -
Information on Tax Identification Numbers Section I – TIN
Information on Tax Identification Numbers Section I – TIN Description In Greenland the TIN equals the CPR number for all natural persons and equals the GER number for all non-natural persons/companies etc. The CPR number is a Danish system and is issued after the rules in the Civil Registration System Act by the Central Registration Office. All residents in Greenland or Denmark gets a CPR number that is used for almost all communication with public authorities and therefore also in tax matters. The CPR number is also issued for all non-residents in Greenland but where the Greenlandic Tax Administration finds the person is taxable to Greenland. The CPR number is a unique number for one person and is not renewed. The GER number for non-natural persons and legal entities is issued according to different tax- and excise laws. The GER number is administrated by Skattestyrelsen (The Greenlandic Customs and Tax Administration) placed under the Greenlandic Ministry of Finance. Additional information on the mandatory issuance of Tax Identification Numbers (TINs) Question 1 – Does your jurisdiction automatically issue TINs to all residents for tax purposes? Individuals Yes Entities Yes S ection II – TIN Structure For natural persons the format of the TIN is a 10 digits structure. From the left it is constructed in the following way: the digits in the positions 1-2 indicate the day of birth of the person; the digits in the positions 3-4 indicate the months of birth of the person; the digits in the positions 5-6 indicate the year of the birth of the person, without indicating the century; the digits in the positions 7-10 form a serial number. -
GBO Site List.Xlsx
EPO Year University of Alberta (CARISMA) Year Greenland Year Russia (AARI) Year BMLS – Bay Mills 2005-07, 10-Current FSIM: Fort Simpson 2006-Current DTU sites: AMD: Amderma, Russia 2011-Current CCNV – Carson City 2004-Current FSMI: Fort Smith 2006-Current AMK: Tassiilaq, Greenland 2007-Current DIK: Dikson, Russia 2011-Current DRBY – Derby 2005-Current GILL: Gillam 2006-Current ATU: Attu, Greenland 2007-09, Current TIK: Tiksi, Russia 2011-Current FYTS – Fort Yates (not in operation) 2005-10 PINA: Pinawa 2006-Current BFE: Brorfelde, Denmark, 2008-Current PBK: Pevek, Russia 2011-Current HOTS – Hot Springs 2004-10 RANK: Rankin Inlet 2006-Current DMH: Danmarkshavn, Greenland 2007-09, Current LOYS – Loysburg 2005-11 SNKQ: Sanikiluaq 2007-Current DNB: Daneborg, Greenland (not in operation) 2007 SGU Year PGEO – Prince Georgeg( (formerly y GBO site) ) 2005-Current ATHA: Athabasca (g(origin NRCan) ) 2008-Current FHB: Paamuit ((Frederikshåp), p), Greenland 2009-Current ABK: Abisko,, Sweden 2007-Current PINE – Pine Ridge 2004-Current GDH: Qeqertarsuaq (Godhavn), Greenland 2007-Current PTRS – Petersburg 2004-Current MACCS (/THEMIS code) Year GHB: Nuuk (Godthåp), Greenland 2009-Current Leirvogur Year RMUS – Remus 2005-Current CDR/CDRT: Cape Dorset 2007-Current KUV: Kullorsuaq, Greenland 2007, 09-Current LRV: Leirvogur, Iceland 2007-Current SWNO – Shawano 2005-Current CRV/CRVR: Clyde River 2008-Current NAQ: Narsarsuaq, Greenland (aka NRSQ) 2007-Current UKIA – Ukiah 2004-Current GJO/GJOA: Gjoa 2008-Current NRD: Nord, Greenland (Data only to 2009) 2007-09