Shipping in the Northwest Passage: Comparing 2013 with 2019
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Transits of the Northwest Passage to End of the 2019 Navigation Season Atlantic Ocean ↔ Arctic Ocean ↔ Pacific Ocean
TRANSITS OF THE NORTHWEST PASSAGE TO END OF THE 2019 NAVIGATION SEASON ATLANTIC OCEAN ↔ ARCTIC OCEAN ↔ PACIFIC OCEAN R. K. Headland and colleagues 12 December 2019 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 but used sledges over the sea ice of the central part of Parry Channel. Subsequently the following 314 complete maritime transits of the Northwest Passage have been made to the end of the 2019 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 (transits 149 and 167). -
Statement by Denmark on Behalf of Finland, Iceland, Norway, Sweden and Denmark
Statement by Denmark on behalf of Finland, Iceland, Norway, Sweden and Denmark 75th Session of the General Assembly of the United Nations Debate in the General Assembly Agenda item 74: Report of the International Court of Justice Delivered by: Counsellor Rasmus Jensen, Denmark New York 2 November 2020 Check against delivery E-mail: [email protected] http://fnnewyork.um.dk 1 M(r/s) Chair, I have the honour to speak on behalf of Finland, , Iceland, Norway, Sweden - and my own country - Denmark. The Nordic countries would like to thank the President of the International Court of Justice for his report on the Court’s work over the past year (A/75/4) and for his presentation today. The big amount of cases indicate the trust and confidence States place in the Court by referring disputes to it for resolution. The Nordic countries would in particular like to note the case filed by The Gambia against Myanmar regarding application of the Convention on the Prevention and Punishment of the Crime of Genocide, where the Court indicated provisional measures on January 23rd. In addition to being important for the gravity of the issues The Gambia’s application seeks to address, the case is also an opportunity for the Court to develop its jurisprudence regarding obligations erga omnes and erga omnes partes. All States parties share an interest in compliance with the obligations under the Genocide Convention by all States parties. We applaud the Court and its personnel for continuing to discharge its judicial functions as described by the President in his report, despite the difficult circumstances following the outbreak of the COVID-19 pandemic. -
Ice Shelf Advance and Retreat Rates Along the Coast of Queen Maud Land, Antarctica K
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 106, NO. C4, PAGES 7097–7106, APRIL 15, 2001 Ice shelf advance and retreat rates along the coast of Queen Maud Land, Antarctica K. T. Kim,1 K. C. Jezek,2 and H. G. Sohn3 Byrd Polar Research Center, The Ohio State University, Columbus, Ohio Abstract. We mapped ice shelf margins along the Queen Maud Land coast, Antarctica, in a study of ice shelf margin variability over time. Our objective was to determine the behavior of ice shelves at similar latitudes but different longitudes relative to ice shelves that are dramatically retreating along the Antarctic Peninsula, possibly in response to changing global climate. We measured coastline positions from 1963 satellite reconnaissance photography and 1997 RADARSAT synthetic aperture radar image data for comparison with coastlines inferred by other researchers who used Landsat data from the mid-1970s. We show that these ice shelves lost ϳ6.8% of their total area between 1963 and 1997. Most of the areal reduction occurred between 1963 and the mid-1970s. Since then, ice margin positions have stabilized or even readvanced. We conclude that these ice shelves are in a near-equilibrium state with the coastal environment. 1. Introduction summer 0Њ isotherm [Tolstikov, 1966, p. 76; King and Turner, 1997, p. 141]. Following Mercer’s hypothesis, we might expect Ice shelves are vast slabs of glacier ice floating on the coastal these ice shelves to be relatively stable at the present time. ocean surrounding Antarctica. They are a continuation of the Following the approach of other investigators [Rott et al., ice sheet and form, in part, as glacier ice flowing from the 1996; Ferrigno et al., 1998; Skvarca et al., 1999], we compare the interior ice sheet spreads across the ocean surface and away position of ice shelf margins and grounding lines derived from from the coast. -
Arctic Seabirds and Shrinking Sea Ice: Egg Analyses Reveal the Importance
www.nature.com/scientificreports OPEN Arctic seabirds and shrinking sea ice: egg analyses reveal the importance of ice-derived resources Fanny Cusset1*, Jérôme Fort2, Mark Mallory3, Birgit Braune4, Philippe Massicotte1 & Guillaume Massé1,5 In the Arctic, sea-ice plays a central role in the functioning of marine food webs and its rapid shrinking has large efects on the biota. It is thus crucial to assess the importance of sea-ice and ice-derived resources to Arctic marine species. Here, we used a multi-biomarker approach combining Highly Branched Isoprenoids (HBIs) with δ13C and δ15N to evaluate how much Arctic seabirds rely on sea-ice derived resources during the pre-laying period, and if changes in sea-ice extent and duration afect their investment in reproduction. Eggs of thick-billed murres (Uria lomvia) and northern fulmars (Fulmarus glacialis) were collected in the Canadian Arctic during four years of highly contrasting ice conditions, and analysed for HBIs, isotopic (carbon and nitrogen) and energetic composition. Murres heavily relied on ice-associated prey, and sea-ice was benefcial for this species which produced larger and more energy-dense eggs during icier years. In contrast, fulmars did not exhibit any clear association with sympagic communities and were not impacted by changes in sea ice. Murres, like other species more constrained in their response to sea-ice variations, therefore appear more sensitive to changes and may become the losers of future climate shifts in the Arctic, unlike more resilient species such as fulmars. Sea ice plays a central role in polar marine ecosystems; it drives the phenology of primary producers that con- stitute the base of marine food webs. -
February 17, 2016
The Arctic in 2045: A Long Term Vision Okalik Eegeesiak | Wilton Park, London, UK| February 17, 2016 An Inuit Vision of the Arctic in 2045 (check against delivery) Ullukkut, Good afternoon. My name is Okalik Eegeesiak. First, thank you to the organizers for the invitation to speak at this conference at such a beautiful and inspiring venue and to the participants who share the value of the Arctic and its peoples. A thirty year vision for the Arctic is important. Inuit believe in a vision for the Arctic – our vision looks back and forward – guided by our past to inform our future. I hope my thoughts will add to the discussion. I will share with you about what Inuit are doing to secure our vision and how we can work together for our shared vision of the Arctic. Inuit have occupied the circumpolar Arctic for millennia – carving a resilient and pragmatic culture from the land and sea – we have lived through famines, the little ice age, Vikings, whalers, missionaries, residential schools, successive governments and we intend to thrive with climate change. A documentary was recently released in Canada that told of the accounts of two Inuit families and an single man from Labrador, Canada now called Nunatsiavut – these Inuit were brought to Europe in the 1880’s and displayed in “zoo’s”. Their remains are still in storage in museums in France and Germany and their predecessors are now working to repatriate them. I share these struggles and trauma to illustrate that we have come a long way… and I am with a solid foundation of our history. -
Imaging Laurentide Ice Sheet Drainage Into the Deep Sea: Impact on Sediments and Bottom Water
Imaging Laurentide Ice Sheet Drainage into the Deep Sea: Impact on Sediments and Bottom Water Reinhard Hesse*, Ingo Klaucke, Department of Earth and Planetary Sciences, McGill University, Montreal, Quebec H3A 2A7, Canada William B. F. Ryan, Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY 10964-8000 Margo B. Edwards, Hawaii Institute of Geophysics and Planetology, University of Hawaii, Honolulu, HI 96822 David J. W. Piper, Geological Survey of Canada—Atlantic, Bedford Institute of Oceanography, Dartmouth, Nova Scotia B2Y 4A2, Canada NAMOC Study Group† ABSTRACT the western Atlantic, some 5000 to 6000 State-of-the-art sidescan-sonar imagery provides a bird’s-eye view of the giant km from their source. submarine drainage system of the Northwest Atlantic Mid-Ocean Channel Drainage of the ice sheet involved (NAMOC) in the Labrador Sea and reveals the far-reaching effects of drainage of the repeated collapse of the ice dome over Pleistocene Laurentide Ice Sheet into the deep sea. Two large-scale depositional Hudson Bay, releasing vast numbers of ice- systems resulting from this drainage, one mud dominated and the other sand bergs from the Hudson Strait ice stream in dominated, are juxtaposed. The mud-dominated system is associated with the short time spans. The repeat interval was meandering NAMOC, whereas the sand-dominated one forms a giant submarine on the order of 104 yr. These dramatic ice- braid plain, which onlaps the eastern NAMOC levee. This dichotomy is the result of rafting events, named Heinrich events grain-size separation on an enormous scale, induced by ice-margin sifting off the (Broecker et al., 1992), occurred through- Hudson Strait outlet. -
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. -
Northwest Passage: Fury & Hecla
NORTHWEST PASSAGE: FURY & HECLA On this active expedition, well visit some of the main highlights of the fabled Northwest Passage, a sea route long-known to sailors around the world for its formidable channels. Traversing this passage was considered the greatest geographical quest for the last three centuries, tempting renowned explorers such as Roald Amundsen and Sir John Franklin. From landscapes to icescapes to seascapes, well explore some of the regions most interesting and stunning landmarks. MANDATORY TRANSFER PACKAGE INCLUDES: One night airport hotel accommodation in Edmonton with breakfast Flight from Edmonton to Kugluktuk Transfers to and from ship to hotel Flight from Kangerlussuaq to Ottawa One night hotel accommodation in Ottawa with breakfast Group transfer Ottawa airport ITINERARY Day 1 Edmonton, Alberta, Canada Enjoy an included night in Edmonton, Alberta and meet your fellow travelers. Day 2 Kugluktuk, Nunavut Kugluktuk meaning place of moving water is aptly named, as the beautiful Kugluk cascade can be found here. In the summertime, so can wildflowers, berry plants and green grasses. We will arrive by way of our group charter flight and then transfer to our small expedition ship. Enjoy your first night on board as you meet your expedition team, the captain and his 01432 507 280 (within UK) [email protected] | small-cruise-ships.com officers, and take part in introductory briefings. We sail eastward through Bellot Strait, a narrow channel separating mainland North America from Somerset Island. Day 3 Port Epworth About mid-point through the channel is the northernmost area Your first views will be that of the expansive landscapes of Port of the continental land mass, Zenith Point. -
Arctic Species Trend Index 2010
Arctic Species Trend Index 2010Tracking Trends in Arctic Wildlife CAFF CBMP Report No. 20 discover the arctic species trend index: www.asti.is ARCTIC COUNCIL Acknowledgements CAFF Designated Agencies: • Directorate for Nature Management, Trondheim, Norway • Environment Canada, Ottawa, Canada • Faroese Museum of Natural History, Tórshavn, Faroe Islands (Kingdom of Denmark) • Finnish Ministry of the Environment, Helsinki, Finland • Icelandic Institute of Natural History, Reykjavik, Iceland • The Ministry of Infrastructure and Environment, the Environmental Agency, the Government of Greenland • Russian Federation Ministry of Natural Resources, Moscow, Russia • Swedish Environmental Protection Agency, Stockholm, Sweden • United States Department of the Interior, Fish and Wildlife Service, Anchorage, Alaska CAFF Permanent Participant Organisations: • Aleut International Association (AIA) • Arctic Athabaskan Council (AAC) • Gwich’in Council International (GCI) • Inuit Circumpolar Conference (ICC) Greenland, Alaska and Canada • Russian Indigenous Peoples of the North (RAIPON) • The Saami Council This publication should be cited as: Louise McRae, Christoph Zöckler, Michael Gill, Jonathan Loh, Julia Latham, Nicola Harrison, Jenny Martin and Ben Collen. 2010. Arctic Species Trend Index 2010: Tracking Trends in Arctic Wildlife. CAFF CBMP Report No. 20, CAFF International Secretariat, Akureyri, Iceland. For more information please contact: CAFF International Secretariat Borgir, Nordurslod 600 Akureyri, Iceland Phone: +354 462-3350 Fax: +354 462-3390 Email: [email protected] Website: www.caff.is Design & Layout: Lily Gontard Cover photo courtesy of Joelle Taillon. March 2010 ___ CAFF Designated Area Report Authors: Louise McRae, Christoph Zöckler, Michael Gill, Jonathan Loh, Julia Latham, Nicola Harrison, Jenny Martin and Ben Collen This report was commissioned by the Circumpolar Biodiversity Monitoring Program (CBMP) with funding provided by the Government of Canada. -
Arctic Marine Transport Workshop 28-30 September 2004
Arctic Marine Transport Workshop 28-30 September 2004 Institute of the North • U.S. Arctic Research Commission • International Arctic Science Committee Arctic Ocean Marine Routes This map is a general portrayal of the major Arctic marine routes shown from the perspective of Bering Strait looking northward. The official Northern Sea Route encompasses all routes across the Russian Arctic coastal seas from Kara Gate (at the southern tip of Novaya Zemlya) to Bering Strait. The Northwest Passage is the name given to the marine routes between the Atlantic and Pacific oceans along the northern coast of North America that span the straits and sounds of the Canadian Arctic Archipelago. Three historic polar voyages in the Central Arctic Ocean are indicated: the first surface shop voyage to the North Pole by the Soviet nuclear icebreaker Arktika in August 1977; the tourist voyage of the Soviet nuclear icebreaker Sovetsky Soyuz across the Arctic Ocean in August 1991; and, the historic scientific (Arctic) transect by the polar icebreakers Polar Sea (U.S.) and Louis S. St-Laurent (Canada) during July and August 1994. Shown is the ice edge for 16 September 2004 (near the minimum extent of Arctic sea ice for 2004) as determined by satellite passive microwave sensors. Noted are ice-free coastal seas along the entire Russian Arctic and a large, ice-free area that extends 300 nautical miles north of the Alaskan coast. The ice edge is also shown to have retreated to a position north of Svalbard. The front cover shows the summer minimum extent of Arctic sea ice on 16 September 2002. -
A Historical and Legal Study of Sovereignty in the Canadian North : Terrestrial Sovereignty, 1870–1939
University of Calgary PRISM: University of Calgary's Digital Repository University of Calgary Press University of Calgary Press Open Access Books 2014 A historical and legal study of sovereignty in the Canadian north : terrestrial sovereignty, 1870–1939 Smith, Gordon W. University of Calgary Press "A historical and legal study of sovereignty in the Canadian north : terrestrial sovereignty, 1870–1939", Gordon W. Smith; edited by P. Whitney Lackenbauer. University of Calgary Press, Calgary, Alberta, 2014 http://hdl.handle.net/1880/50251 book http://creativecommons.org/licenses/by-nc-nd/4.0/ Attribution Non-Commercial No Derivatives 4.0 International Downloaded from PRISM: https://prism.ucalgary.ca A HISTORICAL AND LEGAL STUDY OF SOVEREIGNTY IN THE CANADIAN NORTH: TERRESTRIAL SOVEREIGNTY, 1870–1939 By Gordon W. Smith, Edited by P. Whitney Lackenbauer ISBN 978-1-55238-774-0 THIS BOOK IS AN OPEN ACCESS E-BOOK. It is an electronic version of a book that can be purchased in physical form through any bookseller or on-line retailer, or from our distributors. Please support this open access publication by requesting that your university purchase a print copy of this book, or by purchasing a copy yourself. If you have any questions, please contact us at ucpress@ ucalgary.ca Cover Art: The artwork on the cover of this book is not open access and falls under traditional copyright provisions; it cannot be reproduced in any way without written permission of the artists and their agents. The cover can be displayed as a complete cover image for the purposes of publicizing this work, but the artwork cannot be extracted from the context of the cover of this specificwork without breaching the artist’s copyright. -
Supplementary File For: Blix A.S. 2016. on Roald Amundsen's Scientific Achievements. Polar Research 35. Correspondence: AAB Bu
Supplementary file for: Blix A.S. 2016. On Roald Amundsen’s scientific achievements. Polar Research 35. Correspondence: AAB Building, Institute of Arctic and Marine Biology, University of Tromsø, NO-9037 Tromsø, Norway. E-mail: [email protected] Selected publications from the Gjøa expedition not cited in the text Geelmuyden H. 1932. Astronomy. The scientific results of the Norwegian Arctic expedition in the Gjøa 1903-1906. Geofysiske Publikasjoner 6(2), 23-27. Graarud A. 1932. Meteorology. The scientific results of the Norwegian Arctic expedition in the Gjøa 1903-1906. Geofysiske Publikasjoner 6(3), 31-131. Graarud A. & Russeltvedt N. 1926. Die Erdmagnetischen Beobachtungen der Gjöa-Expedition 1903- 1906. (Geomagnetic observations of the Gjøa expedition, 1903-06.) The scientific results of the Norwegian Arctic expedition in the Gjøa 1903-1906. Geofysiske Publikasjoner 3(8), 3-14. Holtedahl O. 1912. On some Ordovician fossils from Boothia Felix and King William Land, collected during the Norwegian expedition of the Gjøa, Captain Amundsen, through the North- west Passage. Videnskapsselskapets Skrifter 1, Matematisk–Naturvidenskabelig Klasse 9. Kristiania (Oslo): Jacob Dybwad. Lind J. 1910. Fungi (Micromycetes) collected in Arctic North America (King William Land, King Point and Herschell Isl.) by the Gjöa expedition under Captain Roald Amundsen 1904-1906. Videnskabs-Selskabets Skrifter 1. Mathematisk–Naturvidenskabelig Klasse 9. Christiania (Oslo): Jacob Dybwad. Lynge B. 1921. Lichens from the Gjøa expedition. Videnskabs-Selskabets Skrifter 1. Mathematisk– Naturvidenskabelig Klasse 15. Christiania (Oslo): Jacob Dybwad. Ostenfeld C.H. 1910. Vascular plants collected in Arctic North America (King William Land, King Point and Herschell Isl.) by the Gjöa expedition under Captain Roald Amundsen 1904-1906.