Who Discovered the Northwest Passage? Janice Cavell1
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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). -
Crime, Law Enforcement, and Punishment
Shirley Papers 48 Research Materials, Crime Series Inventory Box Folder Folder Title Research Materials Crime, Law Enforcement, and Punishment Capital Punishment 152 1 Newspaper clippings, 1951-1988 2 Newspaper clippings, 1891-1938 3 Newspaper clippings, 1990-1993 4 Newspaper clippings, 1994 5 Newspaper clippings, 1995 6 Newspaper clippings, 1996 7 Newspaper clippings, 1997 153 1 Newspaper clippings, 1998 2 Newspaper clippings, 1999 3 Newspaper clippings, 2000 4 Newspaper clippings, 2001-2002 Crime Cases Arizona 154 1 Cochise County 2 Coconino County 3 Gila County 4 Graham County 5-7 Maricopa County 8 Mohave County 9 Navajo County 10 Pima County 11 Pinal County 12 Santa Cruz County 13 Yavapai County 14 Yuma County Arkansas 155 1 Arkansas County 2 Ashley County 3 Baxter County 4 Benton County 5 Boone County 6 Calhoun County 7 Carroll County 8 Clark County 9 Clay County 10 Cleveland County 11 Columbia County 12 Conway County 13 Craighead County 14 Crawford County 15 Crittendon County 16 Cross County 17 Dallas County 18 Faulkner County 19 Franklin County Shirley Papers 49 Research Materials, Crime Series Inventory Box Folder Folder Title 20 Fulton County 21 Garland County 22 Grant County 23 Greene County 24 Hot Springs County 25 Howard County 26 Independence County 27 Izard County 28 Jackson County 29 Jefferson County 30 Johnson County 31 Lafayette County 32 Lincoln County 33 Little River County 34 Logan County 35 Lonoke County 36 Madison County 37 Marion County 156 1 Miller County 2 Mississippi County 3 Monroe County 4 Montgomery County -
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. -
Statutory Report on Wildlife to the Nunavut Legislative Assembly Section 176 of the Wildlife Act
Statutory Report on Wildlife to the Nunavut Legislative Assembly Section 176 of the Wildlife Act 1.0 Review of Wildlife and Habitat Management Programs for Terrestrial Species in Nunavut…………………………………………………………….1 1.1 Wildlife Act and Wildlife Regulations………………………………………………..2 1.2 Qikiqtaaluk Region……………………………………………………………………2 1.2.1 Qikiqtaaluk Research Initiatives…………………………………………………….2 a. Peary caribou………………………………………………………………………….2 b. High Arctic muskox…………………………………………………………………...3 c. North Baffin caribou…………………………………………………………………..4 1.2.2 Qikiqtaaluk Management Initiatives………………………………………………...5 a. Peary Caribou Management Plan……………………………………………………...5 b. High Arctic Muskox…………………………………………………………………..5 c. South Baffin Management Plan……………………………………………………….6 1.3 Kitikmeot Region……………………………………………………………………...8 1.3.1 Kitikmeot Research Initiatives………………………………………………………9 a. Wolverine and Grizzly bear Hair Snagging………………………………………….. 9 b. Mainland Caribou Projects……………………………………………………………9 c. Boothia Caribou Project……………………………………………………………...10 d. Dolphin and Union Caribou Project……………………............................................10 e. Mainland and Boothia Peninsula Muskoxen………………………………………...11 f. Harvest and Ecological Research Operational System (HEROS)…………………...12 g. Vegetation Mapping……………………………………………………………….....12 1.3.2 Kitikmeot Management Initiatives…………………………………………………12 a. Grizzly Bear Management…………………………………………………………...12 b. Bluenose East Management Plan…………………………………………………….12 c. DU Caribou Management Plan………………………………………………………13 d. Muskox Status -
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. -
Using a Geospatial Approach to Evaluate the Impacts of Shipping Activity on Marine Mammals and Fish in Arctic Canada
Using a Geospatial Approach to Evaluate the Impacts of Shipping Activity on Marine Mammals and Fish in Arctic Canada Thesis Master of Science in Geography with Specialization in Science, Society and Policy Jenna Joyce April 2018 Submitted to: Dr. Jackie Dawson, Supervisor, Department of Geography, University of Ottawa Dr. Luke Copland, Department of Geography, University of Ottawa Dr. Michael Sawada, Department of Geography, University of Ottawa Department of Geography, Environment and Geomatics University of Ottawa © Jenna Joyce, Ottawa, Canada, 2018 Abstract A loss in sea ice cover, primarily attributed to climate change, is increasing the accessibility and navigability of the Arctic Ocean. This increased accessibility of the Canadian Arctic, and in particular the Northwest Passage, presents important global and national shipping and development opportunities. However, increased shipping in the region also present challenges related to the environmental sustainability, sovereignty and safety, and cultural sustainability. The Low Impact Shipping Corridors (the Corridors) is currently the foundational framework for governing ship traffic within the Canadian Arctic. However, the Corridors were largely established based on historic traffic patterns and thus they do not fully consider important areas for marine mammals and fish in the region. This research addresses this important research gap by spatially identifying important areas for marine mammals and fish in the Kitikmeot region of Nunavut using both Traditional Knowledge and western science, evaluating ship tracks from 1990-2015, and geospatially identifying and evaluating areas of potential disturbance for marine mammals and fish related to vessel noise from different ship types transiting the Corridors within the study region. The results of this study indicate that all vessel types have the potential to cause behavioural disturbance to marine mammals and fish when navigating through these important wildlife areas, and that louder vessels (i.e. -
Frederick J. Krabbé, Last Man to See HMS Investigator Afloat, May 1854
The Journal of the Hakluyt Society January 2017 Frederick J. Krabbé, last man to see HMS Investigator afloat, May 1854 William Barr1 and Glenn M. Stein2 Abstract Having ‘served his apprenticeship’ as Second Master on board HMS Assistance during Captain Horatio Austin’s expedition in search of the missing Franklin expedition in 1850–51, whereby he had made two quite impressive sledge trips, in the spring of 1852 Frederick John Krabbé was selected by Captain Leopold McClintock to serve under him as Master (navigation officer) on board the steam tender HMS Intrepid, part of Captain Sir Edward Belcher’s squadron, again searching for the Franklin expedition. After two winterings, the second off Cape Cockburn, southwest Bathurst Island, Krabbé was chosen by Captain Henry Kellett to lead a sledging party west to Mercy Bay, Banks Island, to check on the condition of HMS Investigator, abandoned by Commander Robert M’Clure, his officers and men, in the previous spring. Krabbé executed these orders and was thus the last person to see Investigator afloat. Since, following Belcher’s orders, Kellett had abandoned HMS Resolute and Intrepid, rather than their return journey ending near Cape Cockburn, Krabbé and his men had to continue for a further 140 nautical miles (260 km) to Beechey Island. This made the total length of their sledge trip 863½ nautical miles (1589 km), one of the longest man- hauled sledge trips in the history of the Arctic. Introduction On 22 July 2010 a party from the underwater archaeology division of Parks Canada flew into Mercy Bay in Aulavik National Park, on Banks Island, Northwest Territories – its mission to try to locate HMS Investigator, abandoned here by Commander Robert McClure in 1853.3 Two days later underwater archaeologists Ryan Harris and Jonathan Moore took to the water in a Zodiac to search the bay, towing a side-scan sonar towfish. -
Annual Report: October 1, 2014 Assessing the Impact of Small, Canadian Arctic River Flows to the Freshwater Budget of the Canadian Archipelago Matthew B
Annual Report: October 1, 2014 Assessing the impact of small, Canadian Arctic River flows to the freshwater budget of the Canadian Archipelago Matthew B. Alkire, University of Washington Assessing the impact of small, Canadian Arctic river flows to the freshwater budget of the Canadian Archipelago (or SCARFs) is a scientific research project funded by the National Science Foundation (USA). The purpose of this project is to collect water samples from seven different rivers and their adjoining estuaries throughout the Canadian Arctic Archipelago (see Fig. 1) in order to determine whether or not their chemical signatures differ from larger North American rivers such as the Mackenzie and Yukon Rivers. Five of the rivers are located within Nunavut, Canada: the Coppermine River (near Kugluktuk), Ellice River (~140 km southeast of Cambridge Bay), Back River (~180 km southeast of Gjoa Haven), Cunningham River (~77 km southeast of Resolute Bay on Somerset Island), and Kangiqtugaapik River (near Clyde River, Baffin Island). Two of the rivers are located within the Northwest Territories, Canada: the Kujjuua River (located approximately 67 km northeast of Ulukhaktok on Victoria Island) and Thomsen River (specifically near the mouth of the river where it empties into Castel Bay, on Banks Island). Figure 1. Map of the Canadian Arctic Archipelago. The red stars indicate the mouths of the rivers sampled during this study: (1) Coppermine R., (2) Ellice R., (3) Back R., (4) Kuujuua R. (Victoria Island), (5) Thomsen R. (Banks Island), (6) Cunningham R. (Somerset Island), and (7) Clyde R. (Baffin Island). The Coppermine, Ellice, and Back Rivers are located on the mainland of Nunavut. -
A Personal Narrative of the Origins of the British National Antarctic Expedition 1901-1904 by Sir Clements Markham, Edited and Introduced by Clive Holland
From The Introduction of Antarctic Obsession; A personal narrative of the origins of the British National Antarctic Expedition 1901-1904 by Sir Clements Markham, edited and introduced by Clive Holland. Alburgh, Harleston, Norfolk: Bluntisham Books - Erskine Press, 1986 Pages ix-xxiii I THE CAREER of Sir Clements Markham is almost unique in providing a living and active connection between several of the most outstanding periods of British polar exploration spanning nearly three-quarters of a century. As he is swift to point out in this Personal Narrative, he was acquainted with members of Sir James Clark Ross's pioneering Antarctic expedition of 1839-43 which discovered Ross Island and Victoria Land – regions which were to become the focus of Markham's attention in later life. He had no other direct connection with this expedition, however, for he was only nine years old when it sailed. His own first experience of polar exploration was in another major period of discovery: the search for Sir John Franklin's missing North-west Passage expedition of 1845-8, during which, over some 12 years, much of the Canadian Arctic archipelago was explored for the first time. His role was a modest one, as a midshipman on the Assistance during Captain H. T. Austin's search expedition of 1875-6, but the experience was evidently enough to confirm his enduring interest in the polar regions. His next Arctic role, to which he also refers in the Personal Narrative, was in the organization of the British Arctic Expedition of 1875-6, the primary objects of which were the attainment of the North Pole and the exploration of northern Greenland and Ellesmere Island. -
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’). -
Rather Than Imposing Thematic Unity Or Predefining a Common Theoretical
The Supernatural Arctic: An Exploration Shane McCorristine, University College Dublin Abstract The magnetic attraction of the North exposed a matrix of motivations for discovery service in nineteenth-century culture: dreams of wealth, escape, extreme tourism, geopolitics, scientific advancement, and ideological attainment were all prominent factors in the outfitting expeditions. Yet beneath this „exoteric‟ matrix lay a complex „esoteric‟ matrix of motivations which included the compelling themes of the sublime, the supernatural, and the spiritual. This essay, which pivots around the Franklin expedition of 1845-1848, is intended to be an exploration which suggests an intertextuality across Arctic time and geography that was co-ordinated by the lure of the supernatural. * * * Introduction In his classic account of Scott‟s Antarctic expedition Apsley Cherry- Garrard noted that “Polar exploration is at once the cleanest and most isolated way of having a bad time which has been devised”.1 If there is one single question that has been asked of generations upon generations of polar explorers it is, Why?: Why go through such ordeals, experience such hardship, and take such risks in order to get from one place on the map to another? From an historical point of view, with an apparent fifty per cent death rate on polar voyages in the long nineteenth century amid disaster after disaster, the weird attraction of the poles in the modern age remains a curious fact.2 It is a less curious fact that the question cui bono? also featured prominently in Western thinking about polar exploration, particularly when American expeditions entered the Arctic 1 Apsley Cherry-Garrard, The Worst Journey in the World.