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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. -
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). -
Info for Ankara Applicants
Information for Applicants and Reassignments to the Department of Defense Education Activity’s Ankara Elementary/High School in Ankara, Turkey Ankara Turkey is an UNACCOMPANIED DUTY LOCATION Is Ankara a good fit for you? When deciding, please consider that only the DoDEA employee is authorized to be in Turkey as part of this assignment, you are NOT permitted to have your dependents (family members) with you. This location offers an annual Renewal Agreement for Transportation, allowing employees the opportunity to travel back to the United States (US) to visit family. About Ankara, Turkey Ankara is the capital of Turkey, located in the central part of Anatolia with a population of about 4.5 million, it is Turkey's second-largest city after Istanbul. Ankara has a stable government and economy, it is on this strength, its NATO alliance, and its fairly well-developed infrastructure, it has become a leader in the region. Turkish is the official language; though English is widely understood and is used by some businesses. Islam is the predominant religion of Turkey although places of worship for other faiths exist in the city. Ankara has a continental climate with cold, snowy winters due to its inland location and elevation, and hot, dry summers. Monthly mean temperatures range from 0⁰C (32⁰F) in January to 23⁰C (74⁰F) in July. Ankara E/HS School Community Ankara school opened its doors in 1950 with a staff of 8 servicing a student body of 150 Kindergarten through 9th grade servicing children of US military families. In 1964, the present school buildings, located on a Turkish Military base in Ankara, were dedicated to former U.S. -
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. -
An Archaeological Survey of Newton County: Enhancement of a Data Deficient Region, Part II Grant # 18-15FFY-05
An Archaeological Survey of Newton County: Enhancement of a Data Deficient Region, Part II Grant # 18-15FFY-05 By: Jamie M. Leeuwrik, Christine Thompson, and Kevin C. Nolan Principal Investigators: Christine Thompson and Kevin C. Nolan Reports of Investigation 92 Volume 1 May 2016 Applied Anthropology Laboratories, Department of Anthropology Ball State University, Muncie, IN 47306-0439 Phone: 765-285-5328 Fax: 765-285-2163 Web Address: http://www.bsu.edu/aal i An Archaeological Survey of Newton County: Enhancement of a Data Deficient Region, Part II Grant # 18-15FFY-05 By: Jamie M. Leeuwrik, Christine Thompson, and Kevin C. Nolan Christine Thompson and Kevin C. Nolan Principal Investigators ________________________________ Reports of Investigation 92 Volume 1 May 2016 Applied Anthropology Laboratories, Department of Anthropology Ball State University, Muncie, IN 47306-0439 Phone: 765-285-5328 Fax: 765-285-2163 Web Address: http://www.bsu.edu/aal ii ACKNOWLEDGEMENT OF STATE AND FEDERAL ASSISTANCE This project has been funded in part by a grant from the U.S. Department of the Interior, National Park Service’s Historic Preservation Fund administered by the Indiana Department of Natural Resources, Division of Historic Preservation and Archaeology. The project received federal financial assistance for the identification, protection, and/or rehabilitation of historic properties and cultural resources in the State of Indiana. However, the contents and opinions contained in this publication do not necessarily reflect the views or policies of the U.S. Department of the Interior, nor does the mention of trade names or commercial products constitute endorsement or recommendation by the U.S. Department of the Interior. -
MULTICENTENNIAL CLIMATIC CHANGES in the TERE-Khol
Olga K. Borisova1*, Andrei V. Panin1,2 1 Institute of Geography, Russian Academy of Sciences, Moscow, Russia 2 Lomonosov Moscow State University, Moscow, Russia 02|2019 * Corresponding author: [email protected] GES Multicentennial Climatic CHANGES 148 IN THE TERE-KHOL BASIN, SOUTHERN SIBERIA, DURING THE Late Holocene Abstract. Pollen analysis was carried out on an 80-cm sedimentary section on the shore of Lake Tere-Khol (southeastern Tuva). The section consists of peat overlapping lake loams and covers the last 2800 years. The alternation of dry-wet and cold-warm epochs has been established, and changes in heat and moisture occurred non-simultaneously. The first half of the studied interval, from 2.8 to 1.35 kyr BP was relatively arid and warmer on average. Against this background, temperature fluctuations occurred: relatively cold intervals 2.8– 2.6 and 2.05–1.7 kyr BP and relatively warm 2.6-2.05 and 1.7-1.35 kyr BP. The next time interval 1.35-0.7 kyr BP was relatively humid. Against this background, the temperatures varied from cold 1.35-1.1 kyr BP to relatively warm 1.1–0.7 kyr BP. The last 700 years have been relatively cold with a short warming from 400 to 250 years ago. This period included a relatively dry interval 700–400 years ago and more humid climate in the last 400 years. The established climate variability largely corresponds to other climate reconstructions in the Altai-Sayan region. The general cooling trend corresponds to an astronomically determined trend towards a decrease in solar radiation in temperate latitudes of the Northern Hemisphere, and the centennial temperature fluctuations detected against this background correspond well to changes in solar activity reconstructed from 14C production and the concentration of cosmogenic isotopes in Greenland ice. -
Subarctic Passive House Study
July 11, 2013 Subarctic Passive House Case Study: A Superinsulated Foundation and Vapor Diffusion‐ Open Walls Cold Climate Housing Research Center Written by Bruno Grunau, PE July 11, 2013 Disclaimer: The research conducted or products tested used the methodologies described in this report. CCHRC cautions that different results might be obtained using different test methodologies. CCHRC suggests caution in drawing inferences regarding the research or products beyond the circumstances described in this report. i Subarctic Passive House Case Study: A Superinsulated Foundation and Vapor Diffusion‐Open Walls CONTENTS Summary .................................................................................................................................................................................................... 1 Introduction ............................................................................................................................................................................................... 2 Overview ................................................................................................................................................................................................ 2 Description of Wall System .................................................................................................................................................................... 3 Properties of Cellulose ..................................................................................................................................................................... -
Climate Classification Revisited: from Köppen to Trewartha
Vol. 59: 1–13, 2014 CLIMATE RESEARCH Published February 4 doi: 10.3354/cr01204 Clim Res FREEREE ACCESSCCESS Climate classification revisited: from Köppen to Trewartha Michal Belda*, Eva Holtanová, Tomáš Halenka, Jaroslava Kalvová Charles University in Prague, Dept. of Meteorology and Environment Protection, 18200 Prague, Czech Republic ABSTRACT: The analysis of climate patterns can be performed separately for each climatic vari- able or the data can be aggregated, for example, by using a climate classification. These classifi- cations usually correspond to vegetation distribution, in the sense that each climate type is domi- nated by one vegetation zone or eco-region. Thus, climatic classifications also represent a con - venient tool for the validation of climate models and for the analysis of simulated future climate changes. Basic concepts are presented by applying climate classification to the global Climate Research Unit (CRU) TS 3.1 global dataset. We focus on definitions of climate types according to the Köppen-Trewartha climate classification (KTC) with special attention given to the distinction between wet and dry climates. The distribution of KTC types is compared with the original Köp- pen classification (KCC) for the period 1961−1990. In addition, we provide an analysis of the time development of the distribution of KTC types throughout the 20th century. There are observable changes identified in some subtypes, especially semi-arid, savanna and tundra. KEY WORDS: Köppen-Trewartha · Köppen · Climate classification · Observed climate change · CRU TS 3.10.01 dataset · Patton’s dryness criteria Resale or republication not permitted without written consent of the publisher 1. INTRODUCTION The first quantitative classification of Earth’s cli- mate was developed by Wladimir Köppen in 1900 Climate monitoring is mostly based either directly (Kottek et al. -
Climate & Weather Continental Climate with Four Distinct
SOUTH KOREA - COUNTRY FACT SHEET GENERAL INFORMATION Climate & Weather Continental climate with four Time Zone GMT + 9 hours. distinct seasons. Language Korean Currency Won (KRW). Religion Buddhism, Protestantism, International 82 Catholicism, etc. Dialing Code Population About 50 million. Internet Domain .kr Political System Democracy. Emergency 112(Police) Numbers 119(Fire&Medical) Electricity 220 Voltage. Capital City Seoul. What documents Passport & Proof of Please confirm Monthly directly into a Bank required to open employment (after 3days of how salaries are Account. a local Bank arrival). paid? (eg monthly Account? directly into a Can this be done Bank Account) prior to arrival? 1 GENERAL INFORMATION Culture/Business Culture The traditional Confucian social structure is still prevalent. Age and seniority are important and juniors are expected to follow and obey their elders. It is also considered as an important manner at business. Therefore, people often ask you your age and sometimes your marital status to find out their position. These questions are not meant to intrude on one`s privacy. Health care/medical Hospitals and clinics in Korea are generally equipped with the latest treatment medical equipment, and the quality of medical service is quite high as well. Normally, hospitals open from 9 AM to 6 PM, but some hospitals operate a 24-hr emergency medical center offering advice and assistance over the phone and free interpretation service. Education As of May, 2015, there are 56 international schools in Korea: 21 in Seoul, 7 in Gyeonggi-do, 6 in Busan, 4 in Jeju island, and the rest in other provinces or cities. English is the main language in most international schools in Korea, and U.S style curricula are taught. -
Appendix 1: Database Matrix
Appendix 1: Database Matrix In reviewing each article, we inserted the data for each variable listed below into the ready- formulated Excel database. Where information was not provided or not clear, the data cells were left blank. Answers were mostly quantitative, pre-coded and categorized (as shown in Table A1 and A2 below) to ease subsequent data analysis. Similarly, as seen in Table 3, we used pre- defined categories (Mobility, Exchange, Rationing, Pooling, Diversification, Intensification, Innovation, Revitalization, and Other) to analyze adaptation type. We used basic statistics in Excel to analyze our results. Throughout, we critically examined data collection procedures and analytical methods used to support the information provided in the studies. Part I: Table A1. Descriptive characteristics Description Format Categories Variable Num Number of article (assigned Number --- by us: from 1 onwards) Ref Full scientific reference, eg: Text --- Author et al. (Year) Title, Journal, vol: (issue), pgs. Year Year that article published Number --- Jour Journal title Text --- Auth Lead author affiliation Text country Group Group studied Text Coded later into the following: Data year Year(s) that data were Number collected Cont Continent (classification of Number 1 = Africa 2 = Europe Encyclopedia Britannica 2006) 3 = Asia 4 = North America (including Central America) 5 = South America 6 = Australia 7 = Antarctica Region Region Number 101 = Northern Africa (Maghreb) 102 = Sahel 103 = Rest of Western Africa 104 = East Africa (excluding the Horn -
Climate Change 2020
Continental AG - Climate Change 2020 C0. Introduction C0.1 (C0.1) Give a general description and introduction to your organization. As of December 31, 2019 the Continental Corporation consists of 581 companies, including non-controlled companies in addition to the parent company Continental AG. The Continental team is made up of 241,458 employees at a total of 595 locations in 59 countries and markets. The postal addresses of companies under our control are defined as locations. Continental has been divided into the group sectors Automotive Technologies, Rubber Technologies and Powertrain Technologies since January 1, 2020. These sectors comprise five business areas with 23 business units. A business area or business unit is classified according to technologies, product groups and services. The business areas and business units have overall responsibility for their business, including their results. Overall responsibility for managing the company is borne by the Executive Board of Continental Aktiengesellschaft (AG). Each business area is represented by one Executive Board member. An exception is the Powertrain business area, which has had its own management since January 1, 2019, following its transformation into an independent legal entity. To ensure a unified business strategy in the Automotive Technologies group sector, the Automotive Board was established on April 1, 2019, with a member of the Executive Board as “spokesman.” The new board is intended to speed up decision-making processes and generate synergies from the closer ties between the Autonomous Mobility and Safety business area and the Vehicle Networking and Information business area. With the exception of Corporate Purchasing, the central functions of Continental AG are represented by the chairman of the Executive Board, the chief financial officer and the Executive Board member responsible for Human Relations.