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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). -
Air Quality Improving-Experience of Surabaya City-Indonesia[PDF 9.5MB]
Air Quality Improving - Experiences of Surabaya City Indonesia Prepared on The Sixteenth Asia Pasific Seminar on Climate Change “Asia Pasific Regional Approach to Climate Friendly and Climate Change - Resilient Society” Jakarta, Indonesia, 5 - 8 September 2006 Jump to first page Surabaya Total area = 32.636,69 Ha, 31 District and 163 Sub District Developed area (2002) = 61,9% Population (2005) = 2.739.624 Density = 8.394 per Km2 Surabaya Profile Surabaya • Surabaya is the capital city of East Java Province • Located 1120 121 -70 21 SL and 1120 361 - 1120 541 EL • Area 2,900.443 km2 • Population 2,739.624 • Surabaya Master Plan 2006, it is expected that Surabaya will be developed as City Service • Since years ago Surabaya has a potential to support the development of industrial environment • There are about 9,233 factories with 205,029 employees • SIER its serves an industrial area that is well organized • By development Surabaya have urban problems : Energy combustion in residential area, solid waste, transportation/traffic congestion that can be air pollution problems Air Pollution Sources : • Air pollution problem in Surabaya sources : a. Mobile Source - Transportation b. Non mobile source - Industry , Housing, Incinerator • Effort to Improving Air Quality : a. BLUE SKY PROGRAM b. SUSTAINABLE TRANSPORTATION c. INTEGRATED AMBIEN AIR QUALITY MONITORING CONTINUE d. PUBLIC CAMPAIGN AND INSPESTION & MAINTENANCE e. CNG ACTIVITY f. SURABAYA CAR FREE DAY g. YOUTH ECO EDUCATION h. PLANTATION Activity in CCP ICLEI - Surabaya 1. I & M for corporate -
The Foreign Service Journal, September 1952
Not too high, not too low, but exactly 90.9 proof the perfect proof for Canadian whisky. Now, age-mellowed to be the finest of Canadian whiskies, Canadian Schenley 909 is proudly offered to you at the one Proof of Perfection ,s MADIAS scHK.'tt' i Aged and bottled under the supervision ol the Canadian Government CANADIAN SCHENLEY LTD., VALLEYFIELD. P. Q.. CANADA ©19S2 CANADIAN SCHENLEY LTD. for the coming expansion TELEVISION WITHIN THE NEXT DECADE television will grow beyond all present-day conceptions. International Telephone and Telegraph Corporation is ready to help speed the new industry on its way—ready with new transmitters of advanced design, improved studio equipment, Transmitters, antennas, complete high-gain antennas, microwave links for studio-to-transmitter telecasting installations. and mobile pick-up—and ready with the finest instrument for home entertainment, the incomparable Capeliart. Look to IT&T, together with its associate companies, for tireless effort in television development. Studio equipment, control INTERNATIONAL TELEPHONE AND TELEGRAPH CORPORATION consoles, monitors. 67 Broad Street, New York 4, N. Y. The incomparable Capeliart Television picture-tubes for Capeliart The Selenium Rectifier, converting home television receiver. and other TV manufacturers. AC to DC ... pioneered by IT&T. You GET OUTof a Cigarette just what GOES INTO it! That’s whyyou should smoke Chesterfields— THEY’RE *N0 UNPLEASANT because- A. CHESTERFIELD uses the world's best, mild, ripe tobaccos, pre-tested for the most desirable smoking qualities. B. CHESTERFIELD keeps these tobaccos tasty and fresh with tried and tested moistening agents-pure natural sugars, costly glycerol . nothing else. C. -
50582-NGT Innmat Nr.4-03
NORWEGIAN JOURNAL OF GEOLOGY Carboniferous palynology of the Loppa High, Barents Sea 333 Carboniferous palynology of the Loppa High, Barents Sea, Norway Sofie Lindström Lindström, S.: Carboniferous palynology of the Loppa High, Barents Sea, Norway. Norwegian Journal of Geology,Vol. 83, pp. 333-349. Lund 2003. ISSN 029-196X. Nine palynological intervals, A-I in ascending order, are recognised in the Carboniferous succession of the well 7120/2-1 on the Loppa High in the western Barents Sea. Within the Billefjorden Group intervals A-E are correlated with the early Viséan to Serpukhovian Pu to TK Miospore Zones of western Europe. The known sedimentation break between the Billefjorden and Gipsdalen groups occurred in the Serpukhovian, as interval G of the lower part of the Gipsdalen Group is equivalent to the late Serpukhovian SO Miospore Zone. Lycospora pusilla and Densosporites spp. dominate these assemblages, indicating humid conditions. The topmost interval I correlates with early Moscovian palynofloras of the Arctic. It is at the oldest equivalent with the NJ Miospore Zone. Assemblages within this interval are dominated by the monosaccate pollen Florinites and Potonieisporites, with abundant taeniate and non-taeniate bisaccate pollen, indicating deposition under a dry climatic regime. S. Lindström, Department of Geology, University of Lund, Sölvegatan 12, SE-223 62 Lund, Sweden (E-mail: [email protected]). Introduction ding basins and more stable platforms (Stemmerik & Worsley 2000). The Atlantic rift system between Green- The Carboniferous palynostratigraphy of Western land and Norway was first initiated during the latest Europe presented by Clayton et al. (1977) is well esta- Devonian and earliest Carboniferous (Stemmerik et al. -
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. -
Te Tauihu O Ngā Wānanga
Tracing of old settlements and place names in a Sea Sámi region1 Marit B. Henriksen Sámi University College, Norway [email protected] Introduction The basis for this article is my work with an old land surveying document from Finnmark, in the north of Norway. The document is named Finnmarken Sorenskriveri Landmaalerprotokol, which in English would be The Landsurveying protocol of the County of Finnmark. The main objective for this presentation is to introduce some preliminary results of my work with the protocol and I will present parts of the process, as well as maps, figures and photos showing how the process turns out. About the region Finnmark is the northernmost county of Norway. Finnmark was the last area that became part of the Norwegian territory. The border between the Norwegian and Swedish area was drawn in 1751 and the border between the Norwegian and Russian area was drawn in 1826. Before the closing of the borders, several nation states were interested in this area, that is for taxation purposes. Because of this, the (mainly Sámi) population of the area had to pay taxes to at least three different nation states in periods (Denmark/Norway, Sweden and Russia). Norway was a dependency (satellite state) of Denmark from 1537 to 1814. From 1814, Norway was in union with Sweden, until Norway was declared an independent nation state in 1905. About the Sámi people and the Sámi languages The Sámi area covers parts of four different nation states, Norway, Sweden, Finland and Russia. There are ten different Sámi languages: South Sámi, Ume Sámi, Pite Sámi, Lule Sámi, North Sámi, Inari Sámi, Skolt Sámi, Akkala Sámi, Kildin Sámi and Ter Sámi. -
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. -
Arctic Report Card 2009
October 2009 Citing the complete report: Richter-Menge, J., and J.E. Overland, Eds., 2009: Arctic Report Card 2009, http://www.arctic.noaa.gov/reportcard. Citing an essay (example): Perovich, D., R. Kwok, W. Meier, S. V. Nghiem, and J. Richter-Menge, 2009: Sea Ice Cover [in Arctic Report Card 2009], http://www.arctic.noaa.gov/reportcard. Authors and Affiliations I. Ashik, Arctic and Antarctic Research Institute, St. Petersburg, Russia L.-S. Bai, Byrd Polar Research Center, The Ohio State University, Columbus, Ohio R. Benson, Byrd Polar Research Center, The Ohio State University, Columbus, Ohio U. S. Bhatt, Geophysical Institute, University of Alaska–Fairbanks, Fairbanks, Alaska I. Bhattacharya, Byrd Polar Research Center, The Ohio State University, Columbus, Ohio J. E. Box, Byrd Polar Research Center, The Ohio State University, Columbus, Ohio D. H. Bromwich, Byrd Polar Research Center, The Ohio State University, Columbus, Ohio R. Brown, Climate Research Division, Environment Canada J. Cappelen, Danish Meteorological Institute, Copenhagen, Denmark E. Carmack, Institute of Ocean Sciences, Sidney, Canada B. Collen, Institute of Zoology, Zoological Society of London, Regent’s Park, London, UK J. E. Comiso, NASA Goddard Space Flight Center, Greenbelt, Maryland D. Decker, Byrd Polar Research Center, The Ohio State University, Columbus, Ohio C. Derksen, Climate Research Division, Environment Canada N. DiGirolamo, Science Systems Applications Inc. and NASA Goddard Space Flight Center, Greenbelt, Maryland D. Drozdov, Earth Cryosphere Institute, Tumen, Russia B. Ebbinge, Alterra, Wageningen H. E. Epstein, University of Virginia, Charlottesville, Virginia X. Fettweis, Department of Geography, University of Liège, Liège, Belgium I. Frolov, Arctic and Antarctic Research Institute, St. -
Development of a Pan‐Arctic Monitoring Plan for Polar Bears Background Paper
CAFF Monitoring Series Report No. 1 January 2011 DEVELOPMENT OF A PAN‐ARCTIC MONITORING PLAN FOR POLAR BEARS BACKGROUND PAPER Dag Vongraven and Elizabeth Peacock ARCTIC COUNCIL DEVELOPMENT OF A PAN‐ARCTIC MONITORING PLAN FOR POLAR BEARS Acknowledgements BACKGROUND PAPER The Conservation of Arctic Flora and Fauna (CAFF) is a Working Group of the Arctic Council. Author Dag Vongraven Table of Contents CAFF Designated Agencies: Norwegian Polar Institute Foreword • Directorate for Nature Management, Trondheim, Norway Elizabeth Peacock • Environment Canada, Ottawa, Canada US Geological Survey, 1. Introduction Alaska Science Center • Faroese Museum of Natural History, Tórshavn, Faroe Islands (Kingdom of Denmark) 1 1.1 Project objectives 2 • Finnish Ministry of the Environment, Helsinki, Finland Editing and layout 1.2 Definition of monitoring 2 • Icelandic Institute of Natural History, Reykjavik, Iceland Tom Barry 1.3 Adaptive management/implementation 2 • The Ministry of Domestic Affairs, Nature and Environment, Greenland 2. Review of biology and natural history • Russian Federation Ministry of Natural Resources, Moscow, Russia 2.1 Reproductive and vital rates 3 2.2 Movement/migrations 4 • Swedish Environmental Protection Agency, Stockholm, Sweden 2.3 Diet 4 • United States Department of the Interior, Fish and Wildlife Service, Anchorage, Alaska 2.4 Diseases, parasites and pathogens 4 CAFF Permanent Participant Organizations: 3. Polar bear subpopulations • Aleut International Association (AIA) 3.1 Distribution 5 • Arctic Athabaskan Council (AAC) 3.2 Subpopulations/management units 5 • Gwich’in Council International (GCI) 3.3 Presently delineated populations 5 3.3.1 Arctic Basin (AB) 5 • Inuit Circumpolar Conference (ICC) – Greenland, Alaska and Canada 3.3.2 Baffin Bay (BB) 6 • Russian Indigenous Peoples of the North (RAIPON) 3.3.3 Barents Sea (BS) 7 3.3.4 Chukchi Sea (CS) 7 • Saami Council 3.3.5 Davis Strait (DS) 8 This publication should be cited as: 3.3.6 East Greenland (EG) 8 Vongraven, D and Peacock, E. -
East India Company - Wikipedia, the Free Encyclopedia
East India Company - Wikipedia, the free encyclopedia http://en.wikipedia.org/wiki/East_India_Company From Wikipedia, the free encyclopedia The English East India Company was an English and later (from 1707) East India Company British joint-stock company[1] formed for pursuing trade with the East Indies but which ended up trading mainly with the Indian subcontinent. The East India Company traded mainly in cotton, silk, indigo dye, salt, saltpetre, tea and opium. The Company was granted a Royal Charter in 1600,[2] making it the oldest among several similarly formed European East India Companies. Shares of the company were owned by wealthy merchants and aristocrats. The government owned no shares and had only indirect control. The Company eventually came to rule large areas of India Company flag after 1801 with its own private army, exercising military power and assuming Former type Public administrative functions.[3] Company rule in India effectively began in 1757 after the Battle of Plassey and lasted until 1858 when, following the Industry International trade Indian Rebellion of 1857, the Government of India Act 1858 led to the Fate Dissolved British Crown assuming direct control of India in the new British Raj. Founded 1600 The Company was dissolved in 1874 as a result of the East India Stock Defunct June 1, 1874 Dividend Redemption Act passed one year earlier, as the Government of India Act had by then rendered it vestigal, powerless and obsolete. Its Headquarters London, England functions had been fully absorbed into official government machinery in the British Raj and its private army had been nationalized by the British Colonial India Crown. -
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’). -
Biographical Appendix
Biographical Appendix The following women are mentioned in the text and notes. Abney- Hastings, Flora. 1854–1887. Daughter of 1st Baron Donington and Edith Rawdon- Hastings, Countess of Loudon. Married Henry FitzAlan Howard, 15th Duke of Norfolk, 1877. Acheson, Theodosia. 1882–1977. Daughter of 4th Earl of Gosford and Louisa Montagu (daughter of 7th Duke of Manchester and Luise von Alten). Married Hon. Alexander Cadogan, son of 5th Earl of Cadogan, 1912. Her scrapbook of country house visits is in the British Library, Add. 75295. Alten, Luise von. 1832–1911. Daughter of Karl von Alten. Married William Montagu, 7th Duke of Manchester, 1852. Secondly, married Spencer Cavendish, 8th Duke of Devonshire, 1892. Grandmother of Alexandra, Mary, and Theodosia Acheson. Annesley, Katherine. c. 1700–1736. Daughter of 3rd Earl of Anglesey and Catherine Darnley (illegitimate daughter of James II and Catherine Sedley, Countess of Dorchester). Married William Phipps, 1718. Apsley, Isabella. Daughter of Sir Allen Apsley. Married Sir William Wentworth in the late seventeenth century. Arbuthnot, Caroline. b. c. 1802. Daughter of Rt. Hon. Charles Arbuthnot. Stepdaughter of Harriet Fane. She did not marry. Arbuthnot, Marcia. 1804–1878. Daughter of Rt. Hon. Charles Arbuthnot. Stepdaughter of Harriet Fane. Married William Cholmondeley, 3rd Marquess of Cholmondeley, 1825. Aston, Barbara. 1744–1786. Daughter and co- heir of 5th Lord Faston of Forfar. Married Hon. Henry Clifford, son of 3rd Baron Clifford of Chudleigh, 1762. Bannister, Henrietta. d. 1796. Daughter of John Bannister. She married Rev. Hon. Brownlow North, son of 1st Earl of Guilford, 1771. Bassett, Anne. Daughter of Sir John Bassett and Honor Grenville.