Regional Development Patterns in Canada
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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. -
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. -
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 -
Canadian Border Crossings
Canadian Border Crossings Port Canadian City/Town Province Highway Crossing U.S. City/Town Code 709 Chief Mountain Alberta Chief Mountain via Babb, MT 705 Coutts Alberta Hwy 4 Coutts Sweetgrass, MT 708 Del Bonita Alberta Del Bonita (via Cut Bank), MT 706 Aden Alberta Hwy 880 Whitlash, MT 711 Wild Horse Alberta Hwy 41 Simpson, MT 711 Wildhorse Alta. Hwy 41 Havre, MT 832 Paterson B. C. Northport, WA 841 Aldergrove British Columbia BC 13 Lynden, WA Boundary Bay British Columbia Boundary Bay Point Roberts, WA 840 Douglas British Columbia Peace Arch Blaine, WA 829 Flathead British Columbia Trail Creek, 817 Huntingdon British Columbia BC11 Huntingdon Sumas, WA 813 Pacific Highway British Columbia BC 15 Pacific Highway Blaine, WA 824 Roosville British Columbia Roosville Eureka, MT 822 Rykerts British Columbia Porthill, ID 816 Cascade British Columbia Hwy 3 Laurier, WA Grand Forks British Columbia Hwy 3 Danville, WA 818 Kingsgate British Columbia Hwy 3 Eastport, ID 835 Midway British Columbia Hwy 3 Ferry, WA 828 Nelway British Columbia Hwy 6 Metaline Falls, WA 819 Osoyoos British Columbia Hwy 97 Oroville, WA 507 Boissevain Manitoba Dunseith, ND Middleboro Manitoba Warroad, MN 506 South Junction Manitoba Roseau, MN 521 Cartwright Manitoba Hwy 5 Hansboro, ND 524 Coulter Manitoba Hwy 83 Westhope, ND 520 Crystal City Manitoba Hwy 34 Sarles, ND Hwy 75 / Manitoba 502 Emerson Highway 29 Emerson Pembina, ND Gainsborough Manitoba Hwy 256 Antler, ND Goodlands Manitoba Hwy 21 Carbury, ND 503 Gretna Manitoba Hwy 30 Neche, ND Haskett Manitoba Hwy 32 Walhalla, ND 522 Lena Manitoba Hwy 18 St. -
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. -
Privacy Proofing Your Retail Business: Tips for Protecting
Personal Information Protection Act (“PIPA”) Privacy-Proofing Your Retail Business Tips for Protecting Customers’ Personal Information1 More than ever before, retailers have to be prepared to deal with customers who ask questions about the type and amount of personal information retailers collect, what they intend to do with it, and how they will protect it from misuse. Customers have a right to limit what happens to their personal information—who gets it and what they do with it. Many customers are keen on exercising that right, and private sector personal information protection laws now give them the means to do so. The first step in privacy-proofing your retail operation is to know which personal information protection law is applicable. Provincially regulated retailers in Alberta, British Columbia and Quebec have to comply with the law in force in their province—Alberta and BC each have a Personal Information Protection Act (both came into effect in 2004); the Quebec law is entitled An Act Respecting the Protection of Personal Information in the Private Sector. The federal Personal Information Protection and Electronic Documents Act (“PIPEDA”) applies to retailers in provinces other than Alberta, BC and Quebec and to inter-provincial personal information transfers.2 All of these laws are substantially similar to one another, and all are based on ten privacy principles enshrined in the Canadian Standards Association’s Model Code for the Protection of Personal Information (see box). 1 This article is the product of a co-operative effort by the Retail Council of Canada, the offices of the Information and Privacy Commissioners for Alberta and British Columbia, and the Access and Privacy Branch of Service Alberta. -
Documents to Submit in Support of the Application for a Certificat De
Documents to submit in support of the Application for A-1520-AA a Certificat de sélection du Québec (2015-04) Skilled Workers (Regular Program) General Information You must complete this form and provide all the documents that apply to your situation, in the required format, or else your application will be rejected. The form entitled Documents to submit in support of the Application for a Certificat de sélection du Québec defines the requirements with respect to the nature, format and translation of the documents that you must send us. This form must be enclosed with your application for a selection certificate. Only you, as principal applicant, must fill it out, even if your spouse or a dependent child is accompanying you. Instructions 1. Tick the box corresponding to each of the documents that you are submitting. The entry N/A (Not Applicable) indicates that you do not need to submit this document. 2. Gather all the requested documents in the required format (original, certified true copy or photocopy). 3. Place all your documents in the order indicated in the form. 4. Enclose payment of the fee. 5. Send your application to the Ministère office responsible for your country or territory of residence. The mailing addresses of our offices can be found at www.immigration-quebec.gouv.qc.ca/addresses-countries. Important Certified true copy The “certified true copy” format indicates that the copy of the document that you submit must be certified true to the original either by the document issuer or by a recognized authority from the country or territory that issued the document. -
The Different Stratospheric Influence on Cold-Extremes in Eurasia and North America
The different stratospheric influence on cold-extremes in Eurasia and North America Article Published Version Creative Commons: Attribution 4.0 (CC-BY) Open Access Kretschmer, M. ORCID: https://orcid.org/0000-0002-2756- 9526, Cohen, J., Matthias, V., Runge, J. and Coumou, D. (2018) The different stratospheric influence on cold-extremes in Eurasia and North America. npj Climate and Atmospheric Science, 1 (1). ISSN 2397-3722 doi: https://doi.org/10.1038/s41612-018-0054-4 Available at http://centaur.reading.ac.uk/92433/ It is advisable to refer to the publisher’s version if you intend to cite from the work. See Guidance on citing . Published version at: http://dx.doi.org/10.1038/s41612-018-0054-4 To link to this article DOI: http://dx.doi.org/10.1038/s41612-018-0054-4 Publisher: Nature Publishing Group All outputs in CentAUR are protected by Intellectual Property Rights law, including copyright law. Copyright and IPR is retained by the creators or other copyright holders. Terms and conditions for use of this material are defined in the End User Agreement . www.reading.ac.uk/centaur CentAUR Central Archive at the University of Reading Reading’s research outputs online www.nature.com/npjclimatsci ARTICLE OPEN The different stratospheric influence on cold-extremes in Eurasia and North America Marlene Kretschmer1,2, Judah Cohen3, Vivien Matthias1, Jakob Runge4 and Dim Coumou1,5 The stratospheric polar vortex can influence the tropospheric circulation and thereby winter weather in the mid-latitudes. Weak vortex states, often associated with sudden stratospheric warmings (SSW), have been shown to increase the risk of cold-spells especially over Eurasia, but its role for North American winters is less clear. -
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