National Geographic Geography Handbook

Total Page:16

File Type:pdf, Size:1020Kb

National Geographic Geography Handbook 01-15 GEO HNBK TWIP-860976 4/8/04 12:36 AM Page 1 The Gui River, Guilin, China ▼ The story of the world begins with geog- raphy—the study of the earth in all of its variety. Geography describes the earth’s land, water, and plant and animal life. It is the study of places and the complex relationships between people and their environment. The resources in this handbook will help you get the most out of your textbook—and provide you with skills you will use for the rest of your life. ▼ Saharan sand dunes, Morocco The Amazon, Brazil ▼ Geography Handbook 1 01-15 GEO HNBK TWIP-860976 4/8/04 12:37 AM Page 2 Places and Regions Place has a special mean- ing in geography. It is not just a geographic location. It o understand how our world is connected, some also describes characteristics. T geographers have broken down the study of geography into five themes. The Five Themes of It might describe physical Geography are (1) location, (2) place, (3) human/ characteristics such as land- environment interaction, (4) movement, and forms, climate, and plant or (5) regions. You will see these themes highlighted animal life. Or it might in the Section and Chapter Assessments in The describe human characteris- World and Its People. tics, including language and way of life. Six Essential Elements To help organize their study, geographers often Recently, geographers have broken down the group places into regions. study of geography into Six Essential Elements, Regions are united by which are explained here. Being aware of these one or more common elements will help you sort out what you are characteristics. learning about geography. The World in Spatial Terms Geographers first take a look at where a place is located. Location serves as a starting point by asking “Where is it?” Knowing the loca- tion of places helps you Physical Systems develop an awareness of When studying places the world around you. and regions, geographers analyze how physical systems—such as hurri- canes, volcanoes, and glaciers—shape the earth’s surface. They also look at communities of plants and animals that depend upon one another and their surroundings for survival. 2 Geography Handbook 01-15 GEO HNBK TWIP-860976 4/8/04 12:37 AM Page 3 Geography Handbook Human Systems Geographers also examine human systems, or how people have shaped our world. They look at how boundary lines are deter- mined and analyze why people settle in certain places and not in others. A key theme in geography is the continual movement of people, ideas, and goods. Environment and Society How does the relation- ship between people and their natural surroundings influence the way people live? Geographers study how people use the environment and how their actions affect the environment. The Uses of Geography Knowledge of geography helps us understand the relationships among people, places, and environments over time. Applying geo- graphic skills helps you understand the past and prepare for the future. Geography Handbook 3 01-15 GEO HNBK TWIP-860976 7/8/04 3:01 AM Page 4 Hemispheres To locate places on the earth, geographers use Another imaginary line runs from north to a system of imaginary lines that crisscross the south. It helps divide the earth into half globe. One of these lines, the Equator, circles spheres in the other direction. Find this line— the middle of the earth like a belt. It divides called the Prime Meridian—on a globe. the earth into “half spheres,” or hemispheres. Everything east of the Prime Meridian for Everything north of the Equator is in the 180 degrees is in the Eastern Hemisphere. Northern Hemisphere. Everything south of the Everything west of the Prime Meridian for Equator is in the Southern Hemisphere. 180 degrees is in the Western Hemisphere. Hemispheres Northern Hemisphere Southern Hemisphere Indian Ocean Asia Australia Africa Africa North Pole Europe South Pole Atlantic Pacific Ocean Antarctica Ocean Atlantic Ocean Pacific Ocean North South America America Western Hemisphere Eastern Hemisphere North Europe America Asia Atlantic Ocean Africa Pacific South Ocean America Indian Ocean Australia 4 Geography Handbook 01-15 GEO HNBK TWIP-860976 4/8/04 12:40 AM Page 5 ines on globes and maps provide information L that can help you easily locate places on the earth. These lines—called latitude and longi- tude—cross one another, forming a pattern called a grid system. Latitude Lines of latitude, or parallels, circle the earth parallel to the Equator and measure the distance north or south of the Equator in degrees. The Equator is at 0° latitude, while the North Pole lies at latitude 90°N (north). Longitude Lines of longitude, or meridians, circle the earth from Pole to Pole. These lines measure distances east or west of the starting line, which is at 0° longitude and is called the Prime Meridian. The Prime Meridian runs through the Royal Observatory in Greenwich, England. Absolute Location The grid system formed by lines of latitude and longitude makes it possible to find the absolute location of a place. Only one place can be found at the point where a specific line of latitude crosses a specific line of longitude. By using degrees (°) and minutes (′) (points between degrees), people can pinpoint the precise spot where one line of latitude crosses one line of longitude—an absolute location. Geography Handbook 5 01-15 GEO HNBK TWIP-860976 4/8/04 12:41 AM Page 6 he most accurate way to depict the earth is as a Mapmaking with Technology globe, a round scale model of the earth. A globe T Technology has changed the way maps are gives a true picture of the continents’ relative sizes made. Most cartographers use software pro- and the shapes of landmasses and bodies of water. grams called geographic information systems Globes accurately represent distance and direction. (GIS). This software layers map data from A map is a flat drawing of all or part of the satellite images, printed text, and statistics. A earth’s surface. Unlike globes, maps can show small Global Positioning System (GPS) helps map- areas in great detail. Maps can also display political makers and consumers locate places based on boundaries, population densities, or even voting coordinates broadcast by satellites. returns. From Globes to Maps Great Circle Route Maps, however, do have their limitations. As Map A you can imagine, drawing a round object on a 120°E 180° N 120°W flat surface is very difficult. Cartographers, or W E mapmakers, use mathematical formulas to S transfer information from the round globe to a flat map. However, when the curves of a 60°N globe become straight lines on a map, the size, shape, distance, or area can change or Great Circle Distance 5,450 mi. (8,769 km) Los be distorted. AngelesTokyo 30°N True Direction Distance 5,795 mi. (9,324 km) Great Circle Routes 0° Mapmakers have solved some problems of PACIFIC going from a globe to a map. A great circle is OCEAN an imaginary line that follows the curve of the 30°S 3,0000 mi. 3,0000 earth. A line drawn along the Equator is an 0 km 3,000 example of a great circle. Traveling along a Mercator projection great circle is called following a great circle ° Map B 0 route. Airplane pilots use great circle routes because they represent the shortest distances from one city to another. 60°E The idea of a great circle shows one impor- N ° 60°W 40 tant difference between a globe and a map. °N 60 Because a globe is round, it accurately shows North Pole great circles. On a flat map, however, the great circle route between two points may not appear N E S 120°E W to be the shortest distance. See the maps to the Los Great Circle Route Angeles right. Tokyo PACIFIC 120°W OCEAN Tru te e Direction Rou 3,0000 mi. 3,0000 180° 0 km 3,000 Polar Gnomonic projection 6 Geography Handbook 01-15 GEO HNBK TWIP-860976 7/8/04 3:08 AM Page 7 magine taking the whole peel from an orange and Winkel Tripel Projection I trying to flatten it on a table. You would either have to cut it or stretch parts of it. Mapmakers face 120°W 60°W0° 60° E 120° E ARC TIC CIRCLE a similar problem in showing the surface of the 60°N round earth on a flat map. When the earth’s surface is flattened, big gaps open up. To fill in the gaps, 30°N TROPIC OF CANCER mapmakers stretch parts of the earth. They choose EQUATOR to show either the correct shapes of places or their 0° correct sizes. It is impossible to show both. As a N TROPIC OF CAPRICOR result, mapmakers have developed different projec- 30°S tions, or ways of showing the earth on a flat piece LE °S TIC CIRC MERIDIAN OF GREENWICH (LONDON) of paper. 60 ANTARC Goode’s Interrupted ▼ The Winkel Tripel projection gives a good overall view of Equal-Area Projection the continents’ shapes and sizes. Land areas in a Winkel Tripel projection are not as distorted near the Poles as they are in the ARCTIC CIRCLE Robinson projection. 60°N 30°N TROPIC OF CANCER EQUATOR 0° Mercator Projection TROPIC OF CAPRICORN 30°S 90°E120°E150°E 180° 150° W 120° W 90° W 60°W6030°W300° ° E ° E 60°S ANTARCTIC CIRCLE ▼ Take a second look at your peeled, flattened orange. You might have something that looks like a map based on Goode’s Interrupted Equal-Area projection.
Recommended publications
  • 2. Disc Resources
    An early map of the world Resource D1 A map of the world drawn in 1570 shows ‘Terra Australis Nondum Cognita’ (the unknown south land). National Library of Australia Expeditions to Antarctica 1770 –1830 and 1910 –1913 Resource D2 Voyages to Antarctica 1770–1830 1772–75 1819–20 1820–21 Cook (Britain) Bransfield (Britain) Palmer (United States) ▼ ▼ ▼ ▼ ▼ Resolution and Adventure Williams Hero 1819 1819–21 1820–21 Smith (Britain) ▼ Bellingshausen (Russia) Davis (United States) ▼ ▼ ▼ Williams Vostok and Mirnyi Cecilia 1822–24 Weddell (Britain) ▼ Jane and Beaufoy 1830–32 Biscoe (Britain) ★ ▼ Tula and Lively South Pole expeditions 1910–13 1910–12 1910–13 Amundsen (Norway) Scott (Britain) sledge ▼ ▼ ship ▼ Source: Both maps American Geographical Society Source: Major voyages to Antarctica during the 19th century Resource D3 Voyage leader Date Nationality Ships Most southerly Achievements latitude reached Bellingshausen 1819–21 Russian Vostok and Mirnyi 69˚53’S Circumnavigated Antarctica. Discovered Peter Iøy and Alexander Island. Charted the coast round South Georgia, the South Shetland Islands and the South Sandwich Islands. Made the earliest sighting of the Antarctic continent. Dumont d’Urville 1837–40 French Astrolabe and Zeelée 66°S Discovered Terre Adélie in 1840. The expedition made extensive natural history collections. Wilkes 1838–42 United States Vincennes and Followed the edge of the East Antarctic pack ice for 2400 km, 6 other vessels confirming the existence of the Antarctic continent. Ross 1839–43 British Erebus and Terror 78°17’S Discovered the Transantarctic Mountains, Ross Ice Shelf, Ross Island and the volcanoes Erebus and Terror. The expedition made comprehensive magnetic measurements and natural history collections.
    [Show full text]
  • PRIME MERIDIAN a Place Is
    Lines of Latitude and Longitude help us to answer a key geographical question: “Where am I?” What are Lines of Latitude and Longitude? Lines of Latitude and Longitude refer to the grid system of imaginary lines you will find on a map or globe. PARALLELS of Latitude and MERIDIANS of Longitude form an invisible grid over the earth’s surface and assist in pinpointing any location on Earth with great accuracy; everywhere has its own unique grid location, and this is expressed in terms of LATITUDE and LONGITUDE COORDINATES. Lines of LATITUDE are the ‘horizontal’ lines. They tell us whether a place is located in the NORTHERN or the SOUTHERN HEMISPHERE as well as how far North or South from the EQUATOR it is. Lines of LONGITUDE are the ‘vertical’ lines. They indicate how far East or West of the PRIME MERIDIAN a place is. • The EQUATOR is the 0° LATITUDE LINE. o North of the EQUATOR is the NORTHERN HEMISPHERE. o South of the EQUATOR is the SOUTHERN HEMISPHERE. • Lines of Latitude cross the PRIME MERIDIAN (longitude line) at right angles (90°). • Lines of Latitude circle the globe/world in an east- west direction. • Lines of Latitude are also known as PARALLELS. o As they are parallel to the Equator and apart always at the same distance. • Lines of Latitude measure distance north or south from the equator i.e. how far north or south a point lies from the Equator. • The distance between degree lines is about 69 miles (or about 110km). o A DEGREE (°) equals 60 minutes - 60’.
    [Show full text]
  • Social Studies Class 5 Lesson 3 Latitudes and Longitudes
    Social Studies Class 5 Lesson 3 Latitudes And Longitudes Learning Objectives; Parallels or Latitudes Important Latitudes Meridians or Longitudes Locating Places Since the Earth is spherical in shape, it is difficult to locate a place on Earth. So our mapmakers devised a system of imaginary lines to form a net or grid on maps and globes Thus there are a number of horizontal and vertical lines drawn on maps and globes to help us locate a place. Any location on Earth is described by two numbers--- its Latitude and its Longitude. The imaginary lines that run from East to West are called Parallels or Lines of Latitude. The imaginary lines that run North to South from the poles are called Meridians or the lines of Longitude. LATITUDES Lines of Latitude are east-west circles around the globe. Equator is the 0˚ latitude. It runs through the centre of the globe, halfway between the north pole and the south pole which are at 90˚. Equator 0 North pole 90˚N South pole 90˚S The Equator divides the Earth into two equal halves called hemispheres. 1. Northern Hemisphere: The upper half of the Earth to the north of the equator is called Northern Hemisphere. 2. Southern Hemisphere:The lower half of the earth to the south of the equator is called Southern Hemisphere. Features of Latitude These lines run parallel to each other. They are located at an equal distance from each other. They are also called Parallels. All Parallels form a complete circle around the globe. North Pole and South Pole are however shown as points.
    [Show full text]
  • Frozen Kingdoms the Polar Regions
    Frozen Kingdoms Arctic region Antarctic region The Arctic region consists of the Arctic Ocean and the Antarctica is the world’s fifth-largest continent and is The polar regions northern parts of Canada, Alaska, Russia, Finland, Sweden, covered in an ice sheet that is up to 4800m thick. It is the sphere North Pole 90° N emi Norway, Greenland and Iceland. Winter temperatures can coldest, driest, highest and windiest continent on Earth. n H The Earth has two polar er th reach -50°C and summer temperatures can reach 10°C. Temperatures can drop to -89°C, there is little precipitation, regions: the Arctic or N The Arctic region has a varied landscape including and wind speeds can reach 80km per hour. There are only Circle in the Northern Arctic Circle mountains, tundra and boreal forest. It is home to two native species of flowering plants in Antarctica, but there Hemisphere and 66.5° N small populations of people and an amazing variety is a rich sea life, including the emperor penguin, humpback the Antarctic Circle of plants and animals including the polar bear, whale and leopard seal. No people live permanently in the in the Southern Arctic fox, Arctic hare and walrus. Antarctic. However, scientists stay for part of the year to Hemisphere. Polar Tropic of Cancer e carry out research and tourists visit in the summer months to r regions have long, e 23.5° N h see the landscape and wildlife. p s cold winters and i m e H Equator 0° temperatures mostly n r below freezing.
    [Show full text]
  • Latitude & Longitude Review
    Latitude & Longitude Introduction Latitude Lines of Latitude are also called parallels because they are parallel to each other. They NEVER touch. The 0° Latitude line is called the Equator. They measure distance north and south of the Equator How to remember? Longitude Lines of Longitude are also called meridians. The 0° Longitude line is called the Prime Meridian. It runs through Greenwich England They measure distance east and west of the Prime Meridian until it gets to 180° How to remember? Hemispheres The Prime Meridian divides the earth in half into the Eastern and Western Hemispheres. Hemispheres The Equator divides the earth in half into the Northern and Southern Hemispheres. .When giving the absolute location of a place you first say the Latitude followed by the Longitude. .Boise is located at 44 N., 116W .Both Latitude and Longitude are measured in degrees. .Always make sure you are in the correct hemisphere: North or South – East or West. Latitude and Longitude Part 2 66 ½° N Arctic Circle 23 ½° N Tropic of Cancer Equator 23 ½° S Tropic of Capricorn 66 ½° S Antarctic Circle Prime Meridian Things To Remember • You always read or say the Latitude 1st then the Longitude (makes sense – it is alphabetical. ) – (30°N, 108°W) • Use your pointer finger on both hands to follow each line. • Don’t get hung up on 1 or 2 degrees. • Latitude and Longitude lines are the GRID on the map – smaller area maps may use a different grid. 1. Find 20°N & 100°W – Put a Dot & label 1 2. Find 20°S & 140°E – Put a Dot & label 2 3.
    [Show full text]
  • Across the Antarctic Circle
    Across the Antarctic Circle 02 – 11 March 2019 | Polar Pioneer About Us Aurora Expeditions embodies the spirit of adventure, travelling to some of the most wild and adventure and discovery. Our highly experienced expedition team of naturalists, historians and remote places on our planet. With over 27 years’ experience, our small group voyages allow for destination specialists are passionate and knowledgeable – they are the secret to a fulfilling a truly intimate experience with nature. and successful voyage. Our expeditions push the boundaries with flexible and innovative itineraries, exciting wildlife Whilst we are dedicated to providing a ‘trip of a lifetime’, we are also deeply committed to experiences and fascinating lectures. You’ll share your adventure with a group of like-minded education and preservation of the environment. Our aim is to travel respectfully, creating souls in a relaxed, casual atmosphere while making the most of every opportunity for lifelong ambassadors for the protection of our destinations. DAY 1 | Saturday 2 March 2019 Puerto Williams Position: 21:30 hours Course: 139° Wind Speed: 18 knots Barometer: 997.3 hPa Latitude: 55°05’ S Speed: 111.8 knots Wind Direction: NNW Air Temp: 8°C Longitude: 66°59’ W Sea Temp: 8°C After months of planning, weeks of anticipation and long-haul flights from around the globe, The sound of seven-short-one-long rings from the ship’s signal system was our cue to don we took a final flight from Punta Arenas to arrive at Puerto Williams, Chile, raring to begin our warm clothes, bulky orange lifejackets and gather at the muster stations to sample the ambi- Antarctic adventure.
    [Show full text]
  • Name Date Activity Page 1.2 Use with Chapter 1 Imaginary Lines
    Name Date Activity Page 1.2 Use with Chapter 1 Imaginary Lines Study the map. Then complete the items below. 80°N ARCTIC OCEAN 70°N 60°N 50°N EUROPE NORTH ASIA 40°N AMERICA ATLANTIC 30°N OCEAN PACIFIC 20°N OCEAN 10°N AFRICA 0° 10°S 180° 140°W 100°W SOUTH 20°W 0° 20°E 60°E 100°E 140°E 180° AMERICA INDIAN 20°S OCEAN AUSTRALIA 30°S PACIFIC 40°S OCEAN 50°S 60°S 70°S 80°S ANTARCTICA 1. The numbers that go across the center of the map from left to right indicate lines of . 2. The numbers on the side of the map indicate lines of . 3. On the map, label the following: equator Arctic Circle Tropic of Capricorn North Pole Antarctic Circle prime meridian South Pole Tropic of Cancer international date line TEACHER RESOURCES 61 Name Date Activity Page 1.3 Use with Chapter 1 Latitude as Climate Indicator North Pole ARCTIC OCEAN Polar Arctic Circle 60°N Temperate EUROPE NORTH ASIA Zone AMERICA ATLANTIC 30°N Tropic of Cancer OCEAN PACIFIC OCEAN AFRICA Tropical Zone 0° Equator 180° 150°W 120°W 90°W 60°W 30°W 0° 30°E 60°E 90°E 120°E 150°E 180° SOUTH INDIAN AMERICA OCEAN Tropic of Capricorn AUSTRALIA 30°S Temperate PACIFIC Zone OCEAN Prime Meridian 60°S Antarctic Circle Polar ANTARCTICA South Pole 1. Color the area between the Tropic of Cancer and the Tropic of Capricorn red. This area is known as the zone.
    [Show full text]
  • Unit 3. Antarctic Oceanography Lesson 1
    ANTARCTIC Unit 3. Antarctic Oceanography Lesson 1. – Overview and Research Stations Lesson Objectives: • Introduces the continent of Antarctica and the oceans that surround it • The student will learn about the geography, history and climate. • The second section of this chapter discusses research stations and the scientists who live on the frozen continent. Antarctica is a continent located form 25 million years ago. The at the southern-most point of ice in Antarctica locks up more the globe. Millions of years ago, than two-thirds of the planet's this landmass was attached to fresh water. If the Antarctic ice a giant landmass that consisted were to melt, the sea would rise of modern-day South America, almost 200 feet. It is the only India and Africa. Powerful underground forces ripped a large piece of land from this giant landmass, which then drifted to its current position at the bottom of the globe. It is surrounded on all sides by the Indian, Pacific and Atlantic Oceans. continent that man had left untouched for Antarctica's cold, thick hard millions of years. covering, called an Antarctica is ice considered the sheet, coldest and driest continent on began to earth. Temperatures decrease regions inland. Temperatures as one moves from the coastal during the long, dark winters ©PROJECT OCEANOGRAPHY ANTARCTIC OCEANOGRAPHY 87 ANTARCTIC range from –4° F to –22° F on Blizzards are produced not by the coast, -40° F to –90° F falling snow, but when high inland. During the summers, winds (100- 200mph) blow coastal temperatures average ground snow around, creating 32° F (occasionally climbing to blinding conditions and 50° F), while the inland summer snowdrifts that can cover local temperatures range from –4° F research stations in an hour.
    [Show full text]
  • Across the Antarctic Circle
    Across the Antarctic Circle 4 – 15 February 2020 | Greg Mortimer About Us Aurora Expeditions embodies the spirit of adventure, travelling to some of the most wild opportunity for adventure and discovery. Our highly experienced expedition team of and remote places on our planet. With over 28 years’ experience, our small group voyages naturalists, historians and destination specialists are passionate and knowledgeable – they allow for a truly intimate experience with nature. are the secret to a fulfilling and successful voyage. Our expeditions push the boundaries with flexible and innovative itineraries, exciting Whilst we are dedicated to providing a ‘trip of a lifetime’, we are also deeply committed to wildlife experiences and fascinating lectures. You’ll share your adventure with a group education and preservation of the environment. Our aim is to travel respectfully, creating of like-minded souls in a relaxed, casual atmosphere while making the most of every lifelong ambassadors for the protection of our destinations. DAY 1 | Tuesday 4 February 2020 Ushuaia Position: 20:22 hours Course: 290.6° Wind Speed: 19 knots Barometer: 756 MB & steady Latitude: 54°48.00’ S Speed: At Anchor Wind Direction: NW Air Temp: 15° C Longitude: 068°18.03’ W Sea Temp: 214 C Dare to live the life you have dreamed for yourself. Go forward and make your We learned of some unexpected news: that we would have a bonus day in Ushuaia as dreams come true. — Ralph Waldo Emerson we awaited additional fortifications to our hull from minor damage incurred earlier ni the season. While it came as a bit of surprise, this is a mark of true expedition and adventure.
    [Show full text]
  • Working with Maps, Globes, and Other
    CK_4_TH_HG_P087_242.QXD 10/6/05 9:01 AM Page 93 At a Glance The most important ideas for you are: ◗ Students can use scales on maps and globes to measure distance. ◗ Students can use longitude and latitude coordinates to locate places on maps and globes. ◗ The Prime Meridian is located at 0º longitude, and the International Date Line, which generally corresponds to 180º longitude, marks the change in days from east to west. ◗ Relief maps are special-purpose maps that indicate elevations and depressions in land height. ◗ Major mountain ranges by continent include the Andes (South America), Rockies and Appalachians (North America), Himalayas and Urals (Asia), Atlas (Africa), and Alps (Europe). ◗ High mountains of the world by continent are Everest (Asia), McKinley (North America), Aconcagua (South America), Mont Blanc (Europe), and Kilimanjaro (Africa). What Teachers Need to Know Teaching Idea Background Review map-reading skills and The study of geography embraces many topics throughout the Core concepts from previous grades Knowledge Sequence, including topics in history and science. Geographic as needed. knowledge includes a spatial sense of the world, an awareness of the physical processes to which people culturally adapt, a sense of the interactions between humans and their environment, an understanding of the relations between place and culture, and an awareness of the characteristics of specific regions and cultures. Many geographic topics are listed throughout the World History Cross-curricular and Geography Sequence in connection with historical topics. Teaching Idea Throughout this section, students should connect the “abstract” concepts Compare the distance using map to something more concrete, such as a country of interest or a topic of histor- scale (usually measured in a straight ical study in this grade.
    [Show full text]
  • Polar Regions (Arctic and Antarctic)
    16 Polar Regions (Arctic and Antarctic) OLEG ANISIMOV (RUSSIA) AND BLAIR FITZHARRIS (NEW ZEALAND) Lead Authors: J.O. Hagen (Norway), R. Jefferies (Canada), H. Marchant (Australia), F. Nelson (USA), T. Prowse (Canada), D.G. Vaughan (UK) Contributing Authors: I. Borzenkova (Russia), D. Forbes (Canada), K.M. Hinkel (USA), K. Kobak (Russia), H. Loeng (Norway), T. Root (USA), N. Shiklomanov (Russia), B. Sinclair (New Zealand), P. Skvarca (Argentina) Review Editors: Qin Dahe (China) and B. Maxwell (Canada) CONTENTS Executive Summary 80 3 16 . 2 . 6 . Arctic Hydrology 82 1 16 . 2 . 6 . 1 . Changes in Precipitation, Snow 16 . 1 . Po l a r Re g i o n s 80 7 Accumulation, and Spring Melt 82 3 16 . 1 . 1 . Previous Work—Summary of Special Report 16 . 2 . 6 . 2 . Surface Water Budgets on Regional Impacts of Climate Change 80 7 and Wet l a n d s 82 3 16 . 1 . 2 . Distinctive Characteristics of Polar Regions 80 9 16 . 2 . 6 . 3 . Ecological Impact of 16 . 1 . 3 . Climate Change in the 20th Century 81 0 Changing Runoff Regimes 82 3 16 . 1 . 3 . 1 . The Arctic 81 0 16 . 2 . 6 . 4 . Sensitivity of Arctic Ocean 16 . 1 . 3 . 2 . The An t a r c t i c 81 2 to River Flow 82 4 16 . 1 . 4 . Scenarios of Future Change 81 3 16 . 2 . 7 . Changes in Arctic Biota 82 4 16 . 2 . 7 . 1 . Impacts of Climate Change on 16 . 2 . Key Regional Concerns 81 4 Arctic Terrestrial Environments 82 4 16 . 2 . 1 .
    [Show full text]
  • Tierra Meridianos Y Paralelos
    THE EARTH. MERIDIANS AND PARALLELS 1=Circle of latitude 2=Meridian (geography) A circle of latitude , on the Earth , is an imaginary east -west circle connecting all locations (not taking into account elevation) that share a given latitude . A location's position along a circle of latitude is given by its longitude . Circles of latitude are often called parallels because they are parallel to each other. On some map projections, including the Equirectangular projection , they are drawn at equidistant intervals. Circles of latitude become smaller the farther they are from the equator and the closer they are to the poles . A circle of latitude is perpendicular to all meridians at the points of intersection, and is hence a special case of a loxodrome . Contrary to what might be assumed from their straight-line representation on some map projections, a circle of latitude is not, with the sole exception of the Equator, the shortest distance between two points lying on the Earth. In other words, circles of latitude (except for the Equator) are not great circles (see also great-circle distance ). It is for this reason that an airplane traveling between a European and North American city that share the same latitude will fly farther north, over Greenland for example. Arcs of circles of latitude are sometimes used as boundaries between countries or regions where distinctive natural borders are lacking (such as in deserts), or when an artificial border is drawn as a "line on a map", as happened in Korea . Longitude (λ) Lines of longitude appear vertical with varying curvature in this projection; but are actually halves of great ellipses, with identical radii at a given latitude.
    [Show full text]