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Canada East Equipment Dealers' Association (CEEDA)
Industry Update from Canada: Canada East Equipment Dealers' Association (CEEDA) Monday, 6 July 2020 In partnership with Welcome Michael Barton Regional Director, Canada Invest Northern Ireland – Americas For up to date information on Invest Northern Ireland in the Americas, follow us on LinkedIn & Twitter. Invest Northern Ireland – Americas @InvestNI_USA 2 Invest Northern Ireland – Americas: Export Continuity Support in the Face of COVID-19 Industry Interruption For the Canadian Agri-tech sector… Industry Updates Sessions with industry experts to provide Northern Ireland manufacturers with updates on the Americas markets to assist with export planning and preparation Today’s Update We are delighted to welcome Beverly Leavitt, President & CEO of the Canada East Equipment Dealers' Association (CEEDA). CEEDA represents Equipment Dealers in the Province of Ontario, and the Atlantic Provinces in the Canadian Maritimes. 3 Invest Northern Ireland – Americas: Export Continuity Support in the Face of COVID-19 Industry Interruption For the Canadian Agri-tech sector… Virtual Meet-the-Buyer programs designed to provide 1:1 support to connect Northern Ireland manufacturers with potential Canadian equipment dealers Ongoing dealer development in Eastern & Western Canada For new-to-market exporters, provide support, industry information and routes to market For existing exporters, market expansion and exploration of new Provinces 4 Invest Northern Ireland – Americas: Export Continuity Support in the Face of COVID-19 Industry Interruption For the Canadian -
Canada GREENLAND 80°W
DO NOT EDIT--Changes must be made through “File info” CorrectionKey=NL-B Module 7 70°N 30°W 20°W 170°W 180° 70°N 160°W Canada GREENLAND 80°W 90°W 150°W 100°W (DENMARK) 120°W 140°W 110°W 60°W 130°W 70°W ARCTIC Essential Question OCEANDo Canada’s many regional differences strengthen or weaken the country? Alaska Baffin 160°W (UNITED STATES) Bay ic ct r le Y A c ir u C k o National capital n M R a 60°N Provincial capital . c k e Other cities n 150°W z 0 200 400 Miles i Iqaluit 60°N e 50°N R YUKON . 0 200 400 Kilometers Labrador Projection: Lambert Azimuthal TERRITORY NUNAVUT Equal-Area NORTHWEST Sea Whitehorse TERRITORIES Yellowknife NEWFOUNDLAND AND LABRADOR Hudson N A Bay ATLANTIC 140°W W E St. John’s OCEAN 40°W BRITISH H C 40°N COLUMBIA T QUEBEC HMH Middle School World Geography A MANITOBA 50°N ALBERTA K MS_SNLESE668737_059M_K.ai . S PRINCE EDWARD ISLAND R Edmonton A r Canada legend n N e a S chew E s kat Lake a as . Charlottetown r S R Winnipeg F Color Alts Vancouver Calgary ONTARIO Fredericton W S Island NOVA SCOTIA 50°WFirst proof: 3/20/17 Regina Halifax Vancouver Quebec . R 2nd proof: 4/6/17 e c Final: 4/12/17 Victoria Winnipeg Montreal n 130°W e NEW BRUNSWICK Lake r w Huron a Ottawa L PACIFIC . t S OCEAN Lake 60°W Superior Toronto Lake Lake Ontario UNITED STATES Lake Michigan Windsor 100°W Erie 90°W 40°N 80°W 70°W 120°W 110°W In this module, you will learn about Canada, our neighbor to the north, Explore ONLINE! including its history, diverse culture, and natural beauty and resources. -
The Soviet Doctrine of the Closed Sea
The Soviet Doctrine of the Closed Sea JOSEPH J. DARBY* The Soviet Union's maritime borders include several enclosed and semi-enclosed seas. In order to strengthen its military defenses, Russian jurists, both Tsarist and Soviet, developed and offered to the community of nations the doctrine of the closed sea. According to this doctrine, which has never become part of customary inter- national law, the warships of all nonlittoral countries of certain designated peripheralseas would have no right to enter and navi- gate on those seas. Professor Darby analyzes the application of the doctrine to one of the most important of the peripheralseas on the borders of the USSR, namely the Black Sea, in light of recent history and contemporary developments in the Law of the Sea. SOVIET PUBLIC INTERNATIONAL LAW Writing in 1959, Gregorii Tunkin, who is generally recognized as the most authoritative spokesman of Soviet international law, stated that the international law position of a country is "determined by the basic principles of its foreign policy."' As far as it goes, this state- ment appears to be an accurate reflection of how the leaders of the Soviet Union perceive the nature and function of international law. International law is a means to be used by legal technicians to ad- vance the foreign policy goals of the Soviet state. Soviet legal schol- ars, whose writings are often obtuse and highly generalized, have al- ways been quite clear on this-no rule of international law is binding on the Soviet Union unless, through an unequivocal sovereign act, the Soviet Union has expressly and formally given its consent to be bound by it. -
Radioactivity in the Arctic Seas
IAEA-TECDOC-1075 XA9949696 Radioactivity in the Arctic Seas Report for the International Arctic Seas Assessment Project (IASAP) ffl INTERNATIONAL ATOMIC ENERGY AGENCA / Y / 1JrrziZr^AA 30-16 The originating Section of this publication in the IAEA was: Radiometrics Section International Atomic Energy Agency Marine Environment Laboratory B.P. 800 MC 98012 Monaco Cedex RADIOACTIVITY IN THE ARCTIC SEAS IAEA, VIENNA, 1999 IAEA-TECDOC-1075 ISSN 1011-4289 ©IAEA, 1999 Printe IAEe th AustriAn y i d b a April 1999 FOREWORD From 199 o 1993t e Internationa6th l Atomic Energy Agency's Marine Environment Laboratory (IAEA-MEL s engage IAEA'e wa ) th n di s International Arctic Seas Assessment Project (IASAP whicn i ) h emphasi bees ha sn place criticaa n do l revie f environmentawo l conditions in the Arctic Seas. IAEA-MEe Th L programme, organize framewore th n dIASAi e th f ko P included: (i) an oceanographic and an ecological description of the Arctic Seas; provisioe th (ii )centra a f no l database facilitIASAe th r yfo P programm collectione th r efo , synthesi interpretatiod san datf nmarino n ao e radioactivit Arctie th n yi c Seas; (iii) participation in official expeditions to the Kara Sea organized by the joint Russian- Norwegian Experts Group (1992, 1993 and 1994), the Russian Academy of Sciences (1994), and the Naval Research Laboratory and Norwegian Defence Research Establishment (1995); (iv) assistance wit d n laboratorsiti han u y based radiometric measurement f curreno s t radionuclide concentrations in the Kara Sea; (v) organization of analytical quality assurance intercalibration exercises among the participating laboratories; (vi) computer modellin e potentiath f o g l dispersa f radionuclideo l s released froe mth dumped f assessmeno wast d associatee ean th f o t d radiological consequencee th f o s disposals on local, regional and global scales; (vii) in situ and laboratory based assessment of distribution coefficients (Kd) and concentration factor sArctie (CFth r c)fo environment. -
U.S.-Canada Cross- Border Petroleum Trade
U.S.-Canada Cross- Border Petroleum Trade: An Assessment of Energy Security and Economic Benefits March 2021 Submitted to: American Petroleum Institute 200 Massachusetts Ave NW Suite 1100, Washington, DC 20001 Submitted by: Kevin DeCorla-Souza ICF Resources L.L.C. 9300 Lee Hwy Fairfax, VA 22031 U.S.-Canada Cross-Border Petroleum Trade: An Assessment of Energy Security and Economic Benefits This report was commissioned by the American Petroleum Institute (API) 2 U.S.-Canada Cross-Border Petroleum Trade: An Assessment of Energy Security and Economic Benefits Table of Contents I. Executive Summary ...................................................................................................... 4 II. Introduction ................................................................................................................... 6 III. Overview of U.S.-Canada Petroleum Trade ................................................................. 7 U.S.-Canada Petroleum Trade Volumes Have Surged ........................................................... 7 Petroleum Is a Major Component of Total U.S.-Canada Bilateral Trade ................................. 8 IV. North American Oil Production and Refining Markets Integration ...........................10 U.S.-Canada Oil Trade Reduces North American Dependence on Overseas Crude Oil Imports ..................................................................................................................................10 Cross-Border Pipelines Facilitate U.S.-Canada Oil Market Integration...................................14 -
Fire Regimes of Southern Alberta, Canada
Fire regimes of southern Alberta, Canada by Marie-Pierre Rogeau A thesis submitted in partial fulfilment of the requirements for the degree of Doctor of Philosophy in Forest Biology and Management Department of Renewable Resources University of Alberta © Marie-Pierre Rogeau, 2016 ABSTRACT After decades of recent fire exclusion in southern Alberta, Canada, forests are progressively aging and landscape mosaics are departing from their historical conditions. A large-scale fire history study spanning three natural subregions: Subalpine, Montane and Upper Foothills, was undertaken to understand fire return intervals (FRI) prior to the period of effective fire suppression (pre-1948). This thesis presents an approach to conducting field-based fire history studies in remote landscapes. A paired-plot sampling approach was used to deal with landscapes regulated by large-scale, fully lethal, and mixed severity fires, where fire scar evidence is lost over time. For each natural subregion, point FRIs were used to conduct a fire frequency (i.e. survival) analysis that considers both FRI and time-since-fire data. A total of 3123 tree samples were collected at 814 sampling sites, from which 583 fire scars were identified. Results showed natural subregions had different fire interval distributions before 1948 and some level of FRI variance was also observed within a subregion. The median FRI for the Montane and Foothills sampling units ranged from 26 to 39 years, while the sampling unit located in the most rugged portion of the Subalpine had a median FRI of 85 years. Other aspects of the fire regime were also documented for the three natural subregions including: severity, seasonality and cause. -
The Northern Appalachian/Acadian Ecoregion Priority Locations for Conservation Action the Science Working Group of Two Countries, One Forest/Deux Pays, Une Forêt
Two Countries, One Forest Special Report No. 1 .................................................................................................................................................... The Northern Appalachian/Acadian Ecoregion Priority Locations for Conservation Action The Science Working Group of Two Countries, One Forest/Deux Pays, Une Forêt is comprised of, in alphabetical order: Mark G. Anderson (The Eastern Resource Office, The Nature Conservancy), Robert F. Baldwin (Two Countries, One Forest and Clemson University), Karen Beazley (Dalhousie University), Charlie Bettigole (Wildlands Project), Graham Forbes (University of New Brunswick), Louise Gratton (Nature Conservancy of Canada), Justina C. Ray (Wildlife Conservation Society Canada), Conrad Reining (Wildlands Project), Stephen C. Trombulak (Middlebury College), and Gillian Woolmer (Wildlife Conservation Society Canada). Correct citation for this report: Trombulak, S.C., M.G. Anderson, R.F. Baldwin, K. Beazley, J.C. Ray, C. Reining, G. Woolmer, C. Bettigole, G. Forbes, and L. Gratton. 2008. The Northern Appalachian/Acadian Ecoregion: Priority Locations for Conservation Action. Two Countries, One Forest Special Report No. 1. www.2c1forest.org [email protected] 603.456.3239 P.O. Box 421 Warner, NH 03278 USA ©2008 Two Countries, One Forest Contents .......................................................................................................................... Executive Summary . 2 English . 2 Français . 4 1. Introduction . 6 2. Ecological Description of the Northern -
DRAINAGE BASINS of the WHITE SEA, BARENTS SEA and KARA SEA Chapter 1
38 DRAINAGE BASINS OF THE WHITE SEA, BARENTS SEA AND KARA SEA Chapter 1 WHITE SEA, BARENTS SEA AND KARA SEA 39 41 OULANKA RIVER BASIN 42 TULOMA RIVER BASIN 44 JAKOBSELV RIVER BASIN 44 PAATSJOKI RIVER BASIN 45 LAKE INARI 47 NÄATAMÖ RIVER BASIN 47 TENO RIVER BASIN 49 YENISEY RIVER BASIN 51 OB RIVER BASIN Chapter 1 40 WHITE SEA, BARENT SEA AND KARA SEA This chapter deals with major transboundary rivers discharging into the White Sea, the Barents Sea and the Kara Sea and their major transboundary tributaries. It also includes lakes located within the basins of these seas. TRANSBOUNDARY WATERS IN THE BASINS OF THE BARENTS SEA, THE WHITE SEA AND THE KARA SEA Basin/sub-basin(s) Total area (km2) Recipient Riparian countries Lakes in the basin Oulanka …1 White Sea FI, RU … Kola Fjord > Tuloma 21,140 FI, RU … Barents Sea Jacobselv 400 Barents Sea NO, RU … Paatsjoki 18,403 Barents Sea FI, NO, RU Lake Inari Näätämö 2,962 Barents Sea FI, NO, RU … Teno 16,386 Barents Sea FI, NO … Yenisey 2,580,000 Kara Sea MN, RU … Lake Baikal > - Selenga 447,000 Angara > Yenisey > MN, RU Kara Sea Ob 2,972,493 Kara Sea CN, KZ, MN, RU - Irtysh 1,643,000 Ob CN, KZ, MN, RU - Tobol 426,000 Irtysh KZ, RU - Ishim 176,000 Irtysh KZ, RU 1 5,566 km2 to Lake Paanajärvi and 18,800 km2 to the White Sea. Chapter 1 WHITE SEA, BARENTS SEA AND KARA SEA 41 OULANKA RIVER BASIN1 Finland (upstream country) and the Russian Federation (downstream country) share the basin of the Oulanka River. -
Arctic Report Card 2018 Effects of Persistent Arctic Warming Continue to Mount
Arctic Report Card 2018 Effects of persistent Arctic warming continue to mount 2018 Headlines 2018 Headlines Video Executive Summary Effects of persistent Arctic warming continue Contacts to mount Vital Signs Surface Air Temperature Continued warming of the Arctic atmosphere Terrestrial Snow Cover and ocean are driving broad change in the Greenland Ice Sheet environmental system in predicted and, also, Sea Ice unexpected ways. New emerging threats Sea Surface Temperature are taking form and highlighting the level of Arctic Ocean Primary uncertainty in the breadth of environmental Productivity change that is to come. Tundra Greenness Other Indicators River Discharge Highlights Lake Ice • Surface air temperatures in the Arctic continued to warm at twice the rate relative to the rest of the globe. Arc- Migratory Tundra Caribou tic air temperatures for the past five years (2014-18) have exceeded all previous records since 1900. and Wild Reindeer • In the terrestrial system, atmospheric warming continued to drive broad, long-term trends in declining Frostbites terrestrial snow cover, melting of theGreenland Ice Sheet and lake ice, increasing summertime Arcticriver discharge, and the expansion and greening of Arctic tundravegetation . Clarity and Clouds • Despite increase of vegetation available for grazing, herd populations of caribou and wild reindeer across the Harmful Algal Blooms in the Arctic tundra have declined by nearly 50% over the last two decades. Arctic • In 2018 Arcticsea ice remained younger, thinner, and covered less area than in the past. The 12 lowest extents in Microplastics in the Marine the satellite record have occurred in the last 12 years. Realms of the Arctic • Pan-Arctic observations suggest a long-term decline in coastal landfast sea ice since measurements began in the Landfast Sea Ice in a 1970s, affecting this important platform for hunting, traveling, and coastal protection for local communities. -
How to Use the Digital History Reader
Module 03: 1917 — Did the War Cause a Revolution? Evidence 29: "Workers' Marseillaise" Introduction Based on the anthem of the French Revolution of 1789, the "Workers' Marseillaise" served as the unofficial anthem of the Provisional Government after the Revolution. While the tune of the song provided a symbolic link to a successful tradition of international revolutionary struggle, the words of the Russian variant appealed directly to a brotherhood of working people "from the Dnepr to the White Sea," and "from the Volga to the Caucasus." Document "Workers' Marseillaise" Verse 1: Let us renounce the ancient world! Let us shake its dust from our feet! We've no need for a golden idol, The tsar's palace we do so hate. The tsar needs soldiers for his forces, So, give up your native sons The tsar needs feasts and he needs palaces, So, why not give up your very own blood? Chorus: Arise, arise working people! Rise up against the foe hungry brother! Sound the cry of the people's vengeance! Forward march, forward march, forward march, march, march. Verse 2: The greedy pack of wealthy kulaks, Steal your own hard labor. Then your work fattens up those gluttons, Who will steal the last bit from your mouth. Have we not enough eternal misery? We'll rise brothers against the spreading plague ? From the Dnepr to the White Sea, And from the Volga to the Caucauses. Chorus: Arise, arise working people! Rise up against the foe hungry brother! Sound the cry of the people's vengeance! Forward march, forward march, forward march, march, march. -
The Baltic-White Sea Canal
A GULAG: THE WHITE SEA CANAL A Photo Essay by Donald N. Miller Ever since I was a little boy I heard about the Baltic-White Sea Canal. My uncle Heinrich M. Muller was sentenced to a Gulag there in May 1934. Over the years I learned bits and pieces about the canal from various books and articles, and from Sofie Schmalz, Heinrich’s adopted daughter. But my greatest discovery was made in the State Archives in Zhitomir while working on my book, Under Arrest, and in a personal visit I made to the canal with my wife Nancy in June 2004. Heinrich and Berta Muller and their adopted daughter, Sophie What I learned is that the construction of the canal was begun in November 1931. The plan, largely at the insistence of Stalin, was to build a 227 km long (141 miles), 37 km out of solid rock and the remaining 188 km consisting of dammed-up lakes and flooded riverbeds, linking the White Sea to the Baltic Sea. The purpose was to connect the two seas enabling ships carrying timber and minerals from the White Sea to the commercial ports of the Baltic without making the 370-mile journey through the Artic Ocean, and to provide military access to the area in event of war. It was an old idea, first proposed by trade merchants in the 16th C. During the 20 months it took to build the canal, the number of workers reached in excess of 300,000 at its peak. Of these, over 100,000 were devoured by the fierce winters, abysmal living conditions and stringent labor requirements, although some historians put the number of deaths at a substantially higher figure. -
Integrating Biophysical and Eco-Cultural Fire in Canada Doi: 10.4996/Fireecology.0701074 Page 74
Fire Ecology Volume 7, Issue 1, 2011 White et al.: Integrating Biophysical and Eco-Cultural Fire in Canada doi: 10.4996/fireecology.0701074 Page 74 FORUM ARTICLE BURNING AT THE EDGE: INTEGRATING BIOPHYSICAL AND ECO-CULTURAL FIRE PROCESSES IN CANADA’S PARKS AND PROTECTED AREAS Clifford A. White1*, Daniel D.B. Perrakis2, Victor G. Kafka3, and Timothy Ennis4 1Parks Canada Agency, P.O. Box 900, Banff National Park, Banff, Alberta, Canada T1L 1K2 2 British Columbia Ministry of Natural Resource Operations, Wildfire Management Branch, P.O. Box 9502 Station Provincial Government Victoria, British Columbia, Canada V8W 9C1 3Parks Canada Agency, Ecosystem Conservation Service, 3 passage du Chien d’Or, C.P. 6060, Haute-Ville, Québec, Province of Québec, Canada G1R 4V7 4 Nature Conservancy of Canada, 200-825 Broughton Street, Victoria, British Columbia, Canada V8W 1E5 *Corresponding author: Tel.: 001-403-760-0203; e-mail: [email protected] ABSTRACT Currently, high intensity, large-area lightning fires that burn during droughts dominate Canada’s fire regimes. However, studies from several disciplines clearly show that hu- mans historically ignited burns within this matrix of large fires. Two approaches for fire research and management have arisen from this pattern: a “large-fire biophysical para- digm” related to lightning-ignited fires, and an “eco-cultural paradigm” related to human- caused burning. Working at the edge between biophysically driven fires and eco-cultural burns, and their associated management and research paradigms, presents unique chal- lenges to land managers. We proceed by describing fire frequency trends across Canada, and how an interaction between changing climatic and cultural factors may provide better causal explanations for observed patterns than either group of factors alone.