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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 -
Assessing Snow Phenology Over the Large Part of Eurasia Using Satellite Observations from 2000 to 2016
remote sensing Article Assessing Snow Phenology over the Large Part of Eurasia Using Satellite Observations from 2000 to 2016 Yanhua Sun 1, Tingjun Zhang 1,2,*, Yijing Liu 1, Wenyu Zhao 1 and Xiaodong Huang 3 1 Key Laboratory of West China’s Environment (DOE), College of Earth and Environment Sciences, Lanzhou University, Lanzhou 730000, China; [email protected] (Y.S.); [email protected] (Y.L.); [email protected] (W.Z.) 2 University Corporation for Polar Research, Beijing 100875, China 3 School of Geographical Sciences, Nanjing University of Information Science and Technology, Nanjing 210044, China; [email protected] * Correspondence: [email protected]; Tel.: +86-138-9337-2955 Received: 25 May 2020; Accepted: 23 June 2020; Published: 26 June 2020 Abstract: Snow plays an important role in meteorological, hydrological and ecological processes, and snow phenology variation is critical for improved understanding of climate feedback on snow cover. The main purpose of the study is to explore spatial-temporal changes and variabilities of the extent, timing and duration, as well as phenology of seasonal snow cover across the large part of Eurasia from 2000 through 2016 using a Moderate Resolution Imaging Spectroradiometer (MODIS) cloud-free snow product produced in this study. The results indicate that there are no significant positive or negative interannual trends of snow cover extent (SCE) from 2000 to 2016, but there are large seasonal differences. SCE shows a significant negative trend in spring (p = 0.01) and a positive trend in winter. The stable snow cover areas accounting for 78.8% of the large part of Eurasia, are mainly located north of latitude 45◦ N and in the mountainous areas. -
Determining Carbon Stocks in Cryosols Using the Northern and Mid Latitudes Soil Database
Permafrost, Phillips, Springman & Arenson (eds) © 2003 Swets & Zeitlinger, Lisse, ISBN 90 5809 582 7 Determining carbon stocks in Cryosols using the Northern and Mid Latitudes Soil Database C. Tarnocai Agriculture and Agri-Food Canada, Ottawa, Ontario, Canada J. Kimble USDA-NRCS-NSSC, Lincoln, Nebraska, USA G. Broll Institute of Landscape Ecology, University of Muenster, Muenster, Germany ABSTRACT: The distribution of Cryosols and their carbon content and mass in the northern circumpolar area were estimated by using the Northern and Mid Latitudes Soil Database (NMLSD). Using this database, it was estimated that, in the Northern Hemisphere, Cryosols cover approximately 7769 ϫ 103 km2 and contain approxi- mately 119 Gt (surface, 0–30 cm) and 268 Gt (total, 0–100 cm) of soil organic carbon. The 268 Gt organic carbon is approximately 16% of the world’s soil organic carbon. Organic Cryosols were found to have the highest soil organic carbon mass at both depth ranges while Static Cryosols had the lowest. The accuracy of these carbon val- ues is variable and depends on the information available for the area. Since these soils contain a significant por- tion of the Earth’s soil organic carbon and will probably be the soils most affected by climate warming, new data is required so that more accurate estimates of their carbon budget can be made. 1 INTRODUCTION which is in Arc/Info format, the Soils of Northern and Mid Latitudes (Tarnocai et al. 2002a) and Northern Soils are the largest source of organic carbon in ter- Circumpolar Soils (Tarnocai et al. 2002b) maps were restrial ecosystems. -
Taiga Plains
ECOLOGICAL REGIONS OF THE NORTHWEST TERRITORIES Taiga Plains Ecosystem Classification Group Department of Environment and Natural Resources Government of the Northwest Territories Revised 2009 ECOLOGICAL REGIONS OF THE NORTHWEST TERRITORIES TAIGA PLAINS This report may be cited as: Ecosystem Classification Group. 2007 (rev. 2009). Ecological Regions of the Northwest Territories – Taiga Plains. Department of Environment and Natural Resources, Government of the Northwest Territories, Yellowknife, NT, Canada. viii + 173 pp. + folded insert map. ISBN 0-7708-0161-7 Web Site: http://www.enr.gov.nt.ca/index.html For more information contact: Department of Environment and Natural Resources P.O. Box 1320 Yellowknife, NT X1A 2L9 Phone: (867) 920-8064 Fax: (867) 873-0293 About the cover: The small photographs in the inset boxes are enlarged with captions on pages 22 (Taiga Plains High Subarctic (HS) Ecoregion), 52 (Taiga Plains Low Subarctic (LS) Ecoregion), 82 (Taiga Plains High Boreal (HB) Ecoregion), and 96 (Taiga Plains Mid-Boreal (MB) Ecoregion). Aerial photographs: Dave Downing (Timberline Natural Resource Group). Ground photographs and photograph of cloudberry: Bob Decker (Government of the Northwest Territories). Other plant photographs: Christian Bucher. Members of the Ecosystem Classification Group Dave Downing Ecologist, Timberline Natural Resource Group, Edmonton, Alberta. Bob Decker Forest Ecologist, Forest Management Division, Department of Environment and Natural Resources, Government of the Northwest Territories, Hay River, Northwest Territories. Bas Oosenbrug Habitat Conservation Biologist, Wildlife Division, Department of Environment and Natural Resources, Government of the Northwest Territories, Yellowknife, Northwest Territories. Charles Tarnocai Research Scientist, Agriculture and Agri-Food Canada, Ottawa, Ontario. Tom Chowns Environmental Consultant, Powassan, Ontario. Chris Hampel Geographic Information System Specialist/Resource Analyst, Timberline Natural Resource Group, Edmonton, Alberta. -
Climate and Vegetation • Almost Every Type of Climate Is Found in the 50 United States Because They Extend Over Such a Large Area North to South
123-126-Chapter5 10/16/02 10:16 AM Page 123 Main Ideas Climate and Vegetation • Almost every type of climate is found in the 50 United States because they extend over such a large area north to south. • Canada’s cold climate is related to its location in the far northern latitudes. A HUMAN PERSPECTIVE A little gold and bitter cold—that is what Places & Terms thousands of prospectors found in Alaska and the Yukon Territory dur- permafrost ing the Klondike gold rushes of the 1890s. Most of these fortune prevailing westerlies hunters were unprepared for the harsh climate and inhospitable land of Everglades the far north. Winters were long and cold, the ground frozen. Ice fogs, blizzards, and avalanches were regular occurrences. You could lose fin- Connect to the Issues gers and toes—even your life—in the cold. But hardy souls stuck it out. urban sprawl The rapid Legend has it that one miner, Bishop Stringer, kept himself alive by boil- spread of urban sprawl has led US & CANADA ing his sealskin and walrus-sole boots and then drinking the broth. to the loss of much vegetation in both the United States and Canada. Shared Climates and Vegetation The United States and Canada have more in common than just frigid winter temperatures where Alaska meets northwestern Canada. Other shared climate and vegetation zones are found along their joint border at the southern end of Canada and the northern end of the United States. If you look at the map on page 125, you will see that the United MOVEMENT The snowmobile States has more climate zones than Canada. -
Challenges in the Paleoclimatic Evolution of the Arctic and Subarctic Pacific Since the Last Glacial Period—The Sino–German
challenges Concept Paper Challenges in the Paleoclimatic Evolution of the Arctic and Subarctic Pacific since the Last Glacial Period—The Sino–German Pacific–Arctic Experiment (SiGePAX) Gerrit Lohmann 1,2,3,* , Lester Lembke-Jene 1 , Ralf Tiedemann 1,3,4, Xun Gong 1 , Patrick Scholz 1 , Jianjun Zou 5,6 and Xuefa Shi 5,6 1 Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung Bremerhaven, 27570 Bremerhaven, Germany; [email protected] (L.L.-J.); [email protected] (R.T.); [email protected] (X.G.); [email protected] (P.S.) 2 Department of Environmental Physics, University of Bremen, 28359 Bremen, Germany 3 MARUM Center for Marine Environmental Sciences, University of Bremen, 28359 Bremen, Germany 4 Department of Geosciences, University of Bremen, 28359 Bremen, Germany 5 First Institute of Oceanography, Ministry of Natural Resources, Qingdao 266061, China; zoujianjun@fio.org.cn (J.Z.); xfshi@fio.org.cn (X.S.) 6 Pilot National Laboratory for Marine Science and Technology, Qingdao 266061, China * Correspondence: [email protected] Received: 24 December 2018; Accepted: 15 January 2019; Published: 24 January 2019 Abstract: Arctic and subarctic regions are sensitive to climate change and, reversely, provide dramatic feedbacks to the global climate. With a focus on discovering paleoclimate and paleoceanographic evolution in the Arctic and Northwest Pacific Oceans during the last 20,000 years, we proposed this German–Sino cooperation program according to the announcement “Federal Ministry of Education and Research (BMBF) of the Federal Republic of Germany for a German–Sino cooperation program in the marine and polar research”. Our proposed program integrates the advantages of the Arctic and Subarctic marine sediment studies in AWI (Alfred Wegener Institute) and FIO (First Institute of Oceanography). -
The Comparative Analysis of the Ruminal Bacterial Population in Reindeer (Rangifer Tarandus L.) from the Russian Arctic Zone: Regional and Seasonal Effects
animals Article The Comparative Analysis of the Ruminal Bacterial Population in Reindeer (Rangifer tarandus L.) from the Russian Arctic Zone: Regional and Seasonal Effects Larisa A. Ilina 1,*, Valentina A. Filippova 1 , Evgeni A. Brazhnik 1 , Andrey V. Dubrovin 1, Elena A. Yildirim 1 , Timur P. Dunyashev 1, Georgiy Y. Laptev 1, Natalia I. Novikova 1, Dmitriy V. Sobolev 1, Aleksandr A. Yuzhakov 2 and Kasim A. Laishev 2 1 BIOTROF + Ltd., 8 Malinovskaya St, Liter A, 7-N, Pushkin, 196602 St. Petersburg, Russia; fi[email protected] (V.A.F.); [email protected] (E.A.B.); [email protected] (A.V.D.); [email protected] (E.A.Y.); [email protected] (T.P.D.); [email protected] (G.Y.L.); [email protected] (N.I.N.); [email protected] (D.V.S.) 2 Department of Animal Husbandry and Environmental Management of the Arctic, Federal Research Center of Russian Academy Sciences, 7, Sh. Podbel’skogo, Pushkin, 196608 St. Petersburg, Russia; [email protected] (A.A.Y.); [email protected] (K.A.L.) * Correspondence: [email protected] Simple Summary: The reindeer (Rangifer tarandus) is a unique ruminant that lives in arctic areas characterized by severe living conditions. Low temperatures and a scarce diet containing a high Citation: Ilina, L.A.; Filippova, V.A.; proportion of hard-to-digest components have contributed to the development of several adaptations Brazhnik, E.A.; Dubrovin, A.V.; that allow reindeer to have a successful existence in the Far North region. These adaptations include Yildirim, E.A.; Dunyashev, T.P.; Laptev, G.Y.; Novikova, N.I.; Sobolev, the microbiome of the rumen—a digestive organ in ruminants that is responsible for crude fiber D.V.; Yuzhakov, A.A.; et al. -
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 -
Crop Production in a Northern Climate Pirjo Peltonen-Sainio, MTT Agrifood Research Finland, Plant Production, Jokioinen, Finland
Crop production in a northern climate Pirjo Peltonen-Sainio, MTT Agrifood Research Finland, Plant Production, Jokioinen, Finland CONCEPTS AND ABBREVIATIONS USED IN THIS THEMATIC STUDY In this thematic study northern growing conditions represent the northernmost high latitude European countries (also referred to as the northern Baltic Sea region, Fennoscandia and Boreal regions) characterized mainly as the Boreal Environmental Zone (Metzger et al., 2005). Using this classification, Finland, Sweden, Norway and Estonia are well covered. In Norway, the Alpine North is, however, the dominant Environmental Zone, while in Sweden the Nemoral Zone is represented by the south of the country as for the western parts of Estonia (Metzger et al., 2005). According to the Köppen-Trewartha climate classification, these northern regions include the subarctic continental (taiga), subarctic oceanic (needle- leaf forest) and temperate continental (needle-leaf and deciduous tall broadleaf forest) zones and climates (de Castro et al., 2007). Northern growing conditions are generally considered to be less favourable areas (LFAs) in the European Union (EU) with regional cropland areas typically ranging from 0 to 25 percent of total land area (Rounsevell et al., 2005). Adaptation is the process of adjustment to actual or expected climate and its effects, in order to moderate harm or exploit beneficial opportunities (IPCC, 2012). Adaptive capacity is shaped by the interaction of environmental and social forces, which determine exposures and sensitivities, and by various social, cultural, political and economic forces. Adaptations are manifestations of adaptive capacity. Adaptive capacity is closely linked or synonymous with, for example, adaptability, coping ability and management capacity (Smit and Wandel, 2006). -
Frequency and Characteristics of Arctic Tundra Fires
Frequency and Characteristics of Arctic Tundra Fires ABSTRACT. Characteristics of over 50 tundra fires, located primarily in the west- em Arctic, are summarized. In general, only recent records were available and the numbers of fires were closely related to the accessibility of the area. Most of them covered areas of less than one square kilometre (in contrast to forest fires which are frequently larger) but three tundra fires on the Seward Peninsula of Alaska burned, in aggregate, 16,000 square kilometres of cottongrass tussocks. Though tundra fires can occur as early as May, most of them break out in July and early August. Biomass decreases,and so fires are more easily stopped by discontinuities in vegetation, with distance northward. &UM&. Friquence et curacttWstiques des incendies de toundra de l'Arctique. L'auteur rbume les caractiristiques de 50 incendies de toundra ayant eu lieu princi- palement dans l'Arctique de l'ouest. Eh g6nnk.al il disposait seulement d'une docu- mentation rhnte et le nombre des incendies &ait 6troitementlit$ B PaccessibilitC de la r6gion. La plupart des incendies couvrait des surfaces inf6rieures A un kilombtre carré (en contraste avec les incendiesde fori%), mais une totalit6 de 1600 kilom&tres cm&de tussach de linaigrette brQlhrent au cours de trois incendie? sur la phinsulc de Seward en Alaska. Même si d6jB en mai des incendies de toundra peuvent s'allu- mer, la plupart ont lieu en juillet et au d6but d'aoQt. Au fur et B mesure que l'on monte vers le Nord la quantit6 de vbg6tation (CA"de combustible) diminue et les incendies sont ainsi plus facilement arrêtb par lesintervalles qui sbarent les surfaces couvertes de vhgétation. -
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. -
Description of the Ecoregions of the United States
(iii) ~ Agrl~:::~~;~":,c ullur. Description of the ~:::;. Ecoregions of the ==-'Number 1391 United States •• .~ • /..';;\:?;;.. \ United State. (;lAn) Department of Description of the .~ Agriculture Forest Ecoregions of the Service October United States 1980 Compiled by Robert G. Bailey Formerly Regional geographer, Intermountain Region; currently geographer, Rocky Mountain Forest and Range Experiment Station Prepared in cooperation with U.S. Fish and Wildlife Service and originally published as an unnumbered publication by the Intermountain Region, USDA Forest Service, Ogden, Utah In April 1979, the Agency leaders of the Bureau of Land Manage ment, Forest Service, Fish and Wildlife Service, Geological Survey, and Soil Conservation Service endorsed the concept of a national classification system developed by the Resources Evaluation Tech niques Program at the Rocky Mountain Forest and Range Experiment Station, to be used for renewable resources evaluation. The classifica tion system consists of four components (vegetation, soil, landform, and water), a proposed procedure for integrating the components into ecological response units, and a programmed procedure for integrating the ecological response units into ecosystem associations. The classification system described here is the result of literature synthesis and limited field testing and evaluation. It presents one procedure for defining, describing, and displaying ecosystems with respect to geographical distribution. The system and others are undergoing rigorous evaluation to determine the most appropriate procedure for defining and describing ecosystem associations. Bailey, Robert G. 1980. Description of the ecoregions of the United States. U. S. Department of Agriculture, Miscellaneous Publication No. 1391, 77 pp. This publication briefly describes and illustrates the Nation's ecosystem regions as shown in the 1976 map, "Ecoregions of the United States." A copy of this map, described in the Introduction, can be found between the last page and the back cover of this publication.