4 the Four Hemispheres Key Words: Equator, Prime Meridian, North Pole, South Pole, Hemisphere
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North America Other Continents
Arctic Ocean Europe North Asia America Atlantic Ocean Pacific Ocean Africa Pacific Ocean South Indian America Ocean Oceania Southern Ocean Antarctica LAND & WATER • The surface of the Earth is covered by approximately 71% water and 29% land. • It contains 7 continents and 5 oceans. Land Water EARTH’S HEMISPHERES • The planet Earth can be divided into four different sections or hemispheres. The Equator is an imaginary horizontal line (latitude) that divides the earth into the Northern and Southern hemispheres, while the Prime Meridian is the imaginary vertical line (longitude) that divides the earth into the Eastern and Western hemispheres. • North America, Earth’s 3rd largest continent, includes 23 countries. It contains Bermuda, Canada, Mexico, the United States of America, all Caribbean and Central America countries, as well as Greenland, which is the world’s largest island. North West East LOCATION South • The continent of North America is located in both the Northern and Western hemispheres. It is surrounded by the Arctic Ocean in the north, by the Atlantic Ocean in the east, and by the Pacific Ocean in the west. • It measures 24,256,000 sq. km and takes up a little more than 16% of the land on Earth. North America 16% Other Continents 84% • North America has an approximate population of almost 529 million people, which is about 8% of the World’s total population. 92% 8% North America Other Continents • The Atlantic Ocean is the second largest of Earth’s Oceans. It covers about 15% of the Earth’s total surface area and approximately 21% of its water surface area. -
Geography Notes.Pdf
THE GLOBE What is a globe? a small model of the Earth Parts of a globe: equator - the line on the globe halfway between the North Pole and the South Pole poles - the northern-most and southern-most points on the Earth 1. North Pole 2. South Pole hemispheres - half of the earth, divided by the equator (North & South) and the prime meridian (East and West) 1. Northern Hemisphere 2. Southern Hemisphere 3. Eastern Hemisphere 4. Western Hemisphere continents - the largest land areas on Earth 1. North America 2. South America 3. Europe 4. Asia 5. Africa 6. Australia 7. Antarctica oceans - the largest water areas on Earth 1. Atlantic Ocean 2. Pacific Ocean 3. Indian Ocean 4. Arctic Ocean 5. Antarctic Ocean WORLD MAP ** NOTE: Our textbooks call the “Southern Ocean” the “Antarctic Ocean” ** North America The three major countries of North America are: 1. Canada 2. United States 3. Mexico Where Do We Live? We live in the Western & Northern Hemispheres. We live on the continent of North America. The other 2 large countries on this continent are Canada and Mexico. The name of our country is the United States. There are 50 states in it, but when it first became a country, there were only 13 states. The name of our state is New York. Its capital city is Albany. GEOGRAPHY STUDY GUIDE You will need to know: VOCABULARY: equator globe hemisphere continent ocean compass WORLD MAP - be able to label 7 continents and 5 oceans 3 Large Countries of North America 1. United States 2. Canada 3. -
Indigenous Peoples in Latin America: Statistical Information
Indigenous Peoples in Latin America: Statistical Information Updated August 5, 2021 Congressional Research Service https://crsreports.congress.gov R46225 SUMMARY R46225 Indigenous Peoples in Latin America: Statistical August 5, 2021 Information Carla Y. Davis-Castro This report provides statistical information on Indigenous peoples in Latin America. Data and Research Librarian findings vary, sometimes greatly, on all topics covered in this report, including populations and languages, socioeconomic data, land and natural resources, human rights and international legal conventions. For example the figure below shows four estimates for the Indigenous population of Latin America ranging from 41.8 million to 53.4 million. The statistics vary depending on the source methodology, changes in national censuses, the number of countries covered, and the years examined. Indigenous Population and Percentage of General Population of Latin America Sources: Graphic created by CRS using the World Bank’s LAC Equity Lab with webpage last updated in July 2021; ECLAC and FILAC’s 2020 Los pueblos indígenas de América Latina - Abya Yala y la Agenda 2030 para el Desarrollo Sostenible: tensiones y desafíos desde una perspectiva territorial; the International Bank for Reconstruction and Development and World Bank’s (WB) 2015 Indigenous Latin America in the twenty-first century: the first decade; and ECLAC’s 2014 Guaranteeing Indigenous people’s rights in Latin America: Progress in the past decade and remaining challenges. Notes: The World Bank’s LAC Equity Lab -
Impacts of Four Northern-Hemisphere Teleconnection Patterns on Atmospheric Circulations Over Eurasia and the Pacific
Theor Appl Climatol DOI 10.1007/s00704-016-1801-2 ORIGINAL PAPER Impacts of four northern-hemisphere teleconnection patterns on atmospheric circulations over Eurasia and the Pacific Tao Gao 1,2 & Jin-yi Yu2 & Houk Paek2 Received: 30 July 2015 /Accepted: 31 March 2016 # Springer-Verlag Wien 2016 Abstract The impacts of four teleconnection patterns on at- in summer could be driven, at least partly, by the Atlantic mospheric circulation components over Eurasia and the Multidecadal Oscillation, which to some degree might trans- Pacific region, from low to high latitudes in the Northern mit the influence of the Atlantic Ocean to Eurasia and the Hemisphere (NH), were investigated comprehensively in this Pacific region. study. The patterns, as identified by the Climate Prediction Center (USA), were the East Atlantic (EA), East Atlantic/ Western Russia (EAWR), Polar/Eurasia (POLEUR), and 1 Introduction Scandinavian (SCAND) teleconnections. Results indicate that the EA pattern is closely related to the intensity of the sub- As one of the major components of teleconnection patterns, tropical high over different sectors of the NH in all seasons, atmospheric extra-long waves influence climatic evolutionary especially boreal winter. The wave train associated with this processes. Abnormal oscillations of these extra-long waves pattern serves as an atmospheric bridge that transfers Atlantic generally result in regional or wider-scale irregular atmo- influence into the low-latitude region of the Pacific. In addi- spheric circulations that can lead to abnormal climatic tion, the amplitudes of the EAWR, SCAND, and POLEUR events elsewhere in the world. Therefore, because of their patterns were found to have considerable control on the importance in climate research, considerable attention is given “Vangengeim–Girs” circulation that forms over the Atlantic– to teleconnection patterns on various timescales. -
The New Strategic Framework of the United States for the Western Hemisphere Visit the WEBSITE Receive the E-NEWSLETTER
Analysis Paper 33/2020 21 October 2020 Andrés González Martín The New Strategic Framework of the United States for the Western Hemisphere Visit the WEBSITE Receive the E-NEWSLETTER The New Strategic Framework of the United States for the Western Hemisphere Abstract: Three months before the North American presidential elections, the president of the National Security Council (NSC), Robert O'Brien, presented the new strategic framework for the Western Hemisphere in Florida. Interestingly, the region is the only one that has concerned NSC public diplomacy so much to publish an area development document of the 2017 National Security Strategy. In principle, this special treatment of Latin America is surprising. Especially when the great novelty of 2017 was the express recognition of China and Russia as powers that challenge the power, influence and interest of the United States. However, when it is discovered what is new about the document with respect to the positions of previous administrations, everything ends up falling into place. In Latin America external everything is complicated because there are "adversary countries that exert an evil influence". Keywords: Western Hemisphere, Chinese Communist Party, predatory practices, debt trap, “Growth in the Americas”, "Back to the Americas", Inter-American Development Bank (IDB). *NOTE: The ideas contained in the Analysis Papers are the responsibility of their authors. They do not necessarily reflect the thinking of the IEEE or the Ministry of Defense. Analysis Paper 33/2020 1 The New Strategic Framework of the United States for the Western Hemisphere Andrés González Martín El nuevo marco estratégico de los Estados Unidos para el hemisferio occidental Resumen: Tres meses antes de las elecciones presidenciales norteamericanas, el presidente del Consejo de Seguridad Nacional (NSC), Robert O’Brien, presento en Florida el nuevo marco estratégico del hemisferio occidental. -
Kenya | Year 2| Important Questions Key Knowledge Vocabulary 1 Where Is Kenya on a a Large Solid Area of Land
Kenya | Year 2| Important Questions Key Knowledge Vocabulary 1 Where is Kenya on a A large solid area of land. Earth has Kenya is in East Africa. Nairobi is the 1 continent world map? seven continents. capital city and Mombasa is the largest An area set aside by a country’s 2 What is life like for city in Kenya. 2 National people living in Kenya? park government. The Tana river is the longest river in 3 Maasai one of the best-known groups of 3 What is a national Kenya. people in Africa. They live in park? southern Kenya Mount Kenya is the highest mountain in 4 Endangered Any type of plant or animal that is 4 Which are the main Kenya. in danger of disappearing forever. animals living in Kenya? 5 migrate Many mammals, birds, fishes, 5 What is Maasai insects, and other animals move culture? Kenya lies on the Equator, which means from one place to another at the climate is hot, sunny and dry for most certain times of the year. What is life like for a 6 of the year. ocean A large body of salt water, which Kenyan child compared 6 The Great Rift Valley is an enormous covers the majority of the earth’s to my life? valley of mountains which runs from the surface. north to south of Kenya. The valley has a 7 Capital A large town. Each country has a chain of volcanoes which are still ‘active’ . city capital city, which is usually one of Lake Victoria, the second largest the largest cities. -
Seventh Grade Social Studies, Eastern Hemisphere Course Essential Questions (From Phase I Report)
Davison Community Schools ADVISORY CURRICULUM COUNCIL Phase II, April 2012 Seventh Grade Social Studies, Eastern Hemisphere Course Essential Questions (from Phase I report): 1. How does the past link to the present and determine the future? 2. How does the United States fit into the global world and how is the United States impacted by other nations? 3. What is the relationship between people and the Earth? 4. How can information be used to make informed decisions about understanding the world around us? Phase II Curriculum Unit: Geography Essential Questions: Essential Understanding: How do we use maps and other geographic tools Physical features impact where and how people to acquire information about the world? live What methods of inquiry and analysis do we use Geography impacts population patterns to answer geographic questions? Latitude and elevations impact climate zones How do we use themes, connections and spatial Geographers use 5 themes of geography to patterns to describe and study the Earth? describe regions or places on earth How do we compare and describe natural regions? Human and physical characteristics are used to How do we use human characteristics to study study the earth places on the Earth? Map skills are necessary for understanding information for a variety of maps Recognize distortion in a variety of map scale/projections Economic indicators (GDP, Literacy rate …..) are used to evaluate a country Globalization has created a global interdependence among people There are different purposes of world organizations Curriculum Standards G1.1.1 Explain and use a variety of maps, globes, and web based geography technology to study the world, including global, interregional, regional, and local scales. -
Central America-United States Free United States
Administration of George W. Bush, 2005 / June 23 1061 CAFTA would continue the current trade ing about. That’s why they’re standing up benefits. That means good jobs and higher here and saying with common voice to the labor standards for their workers. And be- United States Congress, ‘‘Let’s get this bill cause of reduced tariffs on U.S. goods, con- passed.’’ See, CAFTA is more than a trade sumers in these countries would have access agreement; it is a signal of our Nation’s com- to better goods at lower prices. And that mitment to democracy and prosperity for the brings us a step closer to our goal of an Amer- entire Western Hemisphere. And I urge, and icas where the opportunities in San Jose, we urge, the United States Congress to pass Costa Rica, are as real as they are in San CAFTA. Jose, California. Thanks for coming. People have got to understand that by pro- moting policy that will help generate wealth NOTE: The President spoke at 1:43 p.m. in Room in Central America, we’re promoting policy 450 of the Dwight D. Eisenhower Executive Of- that will mean someone is less—more likely fice Building. The Office of the Press Secretary to stay at home to find a job. If you’re con- also released a Spanish language transcript of cerned about immigration to this country, these remarks. then you must understand that CAFTA and the benefits of CAFTA will help create new opportunity in Central American countries, Message to the Congress which will mean someone will be able to find Transmitting Legislation and good work at home, somebody will be able Supporting Documents To to provide for their family at home, as op- Implement the Dominican Republic- posed to having to make the long trip to the Central America-United States Free United States. -
Aerosol Optical Depth and Direct Radiative Forcing for INDOEX Derived from AVHRR: Observations, January–March 1996–2000 William R
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 107, NO. D19, 8010, 10.1029/2000JD000183, 2002 Aerosol optical depth and direct radiative forcing for INDOEX derived from AVHRR: Observations, January–March 1996–2000 William R. Tahnk and James A. Coakley Jr. College of Oceanic and Atmospheric Sciences, Oregon State University, Corvallis, Oregon, USA Received 20 November 2000; revised 13 July 2001; accepted 12 November 2001; published 20 August 2002. [1] Visible and near infrared reflectances from NOAA-14 Advanced Very High Resolution Radiometer (AVHRR) daytime passes are used to derive optical depths at 0.55 mm, an index of aerosol type, continental or marine, and the direct effect of the aerosol on the top of the atmosphere and surface solar radiative fluxes for the oceans in the Indian Ocean Experiment (INDOEX) region (30°Sto30°N and 50°–110°E) during the January–March 1996–2000 winter monsoons. Comparison of aerosol optical depth and radiative forcing in the Northern Hemisphere with those in the Southern Hemisphere suggests that the additional pollution sources augment the 0.55-mm optical depth by, on average, 0.1 in the Northern Hemisphere. As a result of the aerosol, the region of the Indian Ocean in the Northern Hemisphere loses about 1.6 WmÀ2 in reflected sunlight and the ocean surface loses about 5 WmÀ2 during the months of the winter monsoon. Aerosol burdens and the aerosol direct radiative forcing are a relatively constant feature of the Northern Hemisphere, although the southeastern Arabian Sea experienced considerably larger aerosol burdens during the February–March 1999 INDOEX Intensive Field Phase (IFP) than in other years. -
Coriolis Effect
Project ATMOSPHERE This guide is one of a series produced by Project ATMOSPHERE, an initiative of the American Meteorological Society. Project ATMOSPHERE has created and trained a network of resource agents who provide nationwide leadership in precollege atmospheric environment education. To support these agents in their teacher training, Project ATMOSPHERE develops and produces teacher’s guides and other educational materials. For further information, and additional background on the American Meteorological Society’s Education Program, please contact: American Meteorological Society Education Program 1200 New York Ave., NW, Ste. 500 Washington, DC 20005-3928 www.ametsoc.org/amsedu This material is based upon work initially supported by the National Science Foundation under Grant No. TPE-9340055. Any opinions, findings, and conclusions or recommendations expressed in this publication are those of the authors and do not necessarily reflect the views of the National Science Foundation. © 2012 American Meteorological Society (Permission is hereby granted for the reproduction of materials contained in this publication for non-commercial use in schools on the condition their source is acknowledged.) 2 Foreword This guide has been prepared to introduce fundamental understandings about the guide topic. This guide is organized as follows: Introduction This is a narrative summary of background information to introduce the topic. Basic Understandings Basic understandings are statements of principles, concepts, and information. The basic understandings represent material to be mastered by the learner, and can be especially helpful in devising learning activities in writing learning objectives and test items. They are numbered so they can be keyed with activities, objectives and test items. Activities These are related investigations. -
1 Climatology of South American Seasonal Changes
Vol. 27 N° 1 y 2 (2002) 1-30 PROGRESS IN PAN AMERICAN CLIVAR RESEARCH: UNDERSTANDING THE SOUTH AMERICAN MONSOON Julia Nogués-Paegle 1 (1), Carlos R. Mechoso (2), Rong Fu (3), E. Hugo Berbery (4), Winston C. Chao (5), Tsing-Chang Chen (6), Kerry Cook (7), Alvaro F. Diaz (8), David Enfield (9), Rosana Ferreira (4), Alice M. Grimm (10), Vernon Kousky (11), Brant Liebmann (12), José Marengo (13), Kingste Mo (11), J. David Neelin (2), Jan Paegle (1), Andrew W. Robertson (14), Anji Seth (14), Carolina S. Vera (15), and Jiayu Zhou (16) (1) Department of Meteorology, University of Utah, USA, (2) Department of Atmospheric Sciences, University of California, Los Angeles, USA, (3) Georgia Institute of Technology; Earth & Atmospheric Sciences, USA (4) Department of Meteorology, University of Maryland, USA, (5) Laboratory for Atmospheres, NASA/Goddard Space Flight Center, USA, (6) Department of Geological and Atmospheric Sciences, Iowa State University, USA, (7) Department of Earth and Atmospheric Sciences, Cornell University, USA, (8) Instituto de Mecánica de Fluidos e Ingeniería Ambiental, Universidad de la República, Uruguay, (9) NOAA Atlantic Oceanographic Laboratory, USA, (10) Department of Physics, Federal University of Paraná, Brazil, (11) Climate Prediction Center/NCEP/NWS/NOAA, USA, (12) NOAA-CIRES Climate Diagnostics Center, USA, (13) Centro de Previsao do Tempo e Estudos de Clima, CPTEC, Brazil, (14) International Research Institute for Climate Prediction, Lamont Doherty Earth Observatory of Columbia University, USA, (15) CIMA/Departmento de Ciencias de la Atmósfera, University of Buenos Aires, Argentina, (16) Goddard Earth Sciences Technology Center, University of Maryland, USA. (Manuscript received 13 May 2002, in final form 20 January 2003) ABSTRACT A review of recent findings on the South American Monsoon System (SAMS) is presented. -
Smithsonian Miscellaneous Collections
-&? SMITHSONIAN MISCELLANEOUS COLLECTIONS VOLUME 82. NUMBER 6 THE PAST CLIMATE OF THE NORTH POLAR REGION BY EDWARD W. BERRY The Johns Hopkins University (Publication 3061) CITY OF WASHINGTON PUBLISHED BY THE SMITHSONIAN INSTITUTION APRIL 9, 1930 SMITHSONIAN MISCELLANEOUS COLLECTIONS VOLUME 82, NUMBER 6 THE PAST CLIMATE OF THE NORTH POLAR REGION BY EDWARD W. BERRY The Johns Hopkins University Publication 306i i CITY OF WASHINGTON PUBLISHED BY THE SMITHSONIAN INSTITUTION APRIL 9, 1930 ZU £or& (gafttmore (prees BALTIMORE, MD., U. S. A. THE PAST CLIMATE OF THE NORTH POLAR REGION 1 By EDWARD W. BERRY THE JOHNS HOPKINS UNIVERSITY The plants, coal beds, hairy mammoth and woolly rhinoceros ; the corals, ammonites and the host of other marine organisms, chiefly invertebrate but including ichthyosaurs and other saurians, that have been discovered beneath the snow and ice of boreal lands have always made a most powerful appeal to the imagination of explorers and geologists. We forget entirely the modern whales, reindeer, musk ox, polar bear, and abundant Arctic marine life, and remember only the seemingly great contrast between the present and this subjective past. Nowhere on the earth is there such an apparent contrast between the present and geologic climates as in the polar regions and the mental pictures which have been aroused and the theories by means of which it has been sought to explain the fancied conditions of the past are all, at least in large part, highly imaginary. Occasionally a student like Nathorst (1911) has refused to be carried away by his imagination and has called to mind the mar- velously rich life of the present day Arctic seas, but for the most part those who have speculated on former climates have entirely ignored the results of Arctic oceanography.