The Globe Latitudes and Longitudes
|
|
- Cleopatra Chandler
- 7 years ago
- Views:
Transcription
1 INDIAN SCHOOL MUSCAT MIDDLE SECTION DEPARTMENT OF SOCIAL SCIENCE The Globe Latitudes and Longitudes NAME: CLASS VI SEC: ROLL NO: DATE: I NAME THE FOLLOWING: 1. A small spherical model of the Earth: 2. It is 0 0 latitude and is a great circle: 3. The hottest zone: 4. The zone between Tropic of Cancer and Arctic Circle in the north and Tropic of Capricorn and Antarctic Circle in the south: 5. The zone between Arctic Circle and N Frigid zone and Antarctic Circle and S Frigid zone: 6. Lines of latitude and longitude form a network of lines: 7. It helps us to determine the time at a place: 8. The standard meridian for India: 9. The time followed all over India : 10. The time difference between Greenwich Mean Time(GMT) and Indian Standard Time(IST): II FILL IN THE BLANKS: 1. The earth is spherical in shape, slightly flattened at the and bulging at the 2. The shape of the earth is best described by the term which means earthshaped. 3. The earth rotates on its axis from to 4. The northern end of the axis is the and the southern end, the 5. The horizontal lines (east-west lines) are called 6. The is a great circle. 7. The vertical lines (north-south lines) are called
2 8. There are lines of latitude in the northern hemisphere as well as in the southern hemisphere. 9. On the basis of the distance from the equator, the earth is divided into the following zones. 10. There are a total of lines of longitude. 11. All lines of longitude converge or meet at the two 12. The is the shortest route between two places on the earth. 13. The world is divided into zones. III STATE WHETHER THE STATEMENTS ARE TRUE OR FALSE: 1. We write E or W with longitude: 2. A great circle divides the earth into two halves: 3. The earth rotates in an anti-clockwise direction: 4. The axis of the earth is tilted at an angle of 23 ½ 0 to the vertical: 5. A country cannot have more than one standard time: IV MATCH THE FOLLOWING: S.No. Column A S.No. Column B Responses 1. Vertical rays of the sun a Southern Hemisphere Slanting rays of the sun b Northern Hemisphere Tropic of Cancer c Equator South Frigid d Important latitude Antarctic Circle e Poles Arctic Circle f Heat zone 6. V OBSERVE THE DIAGRAM AND LABEL IT: A B A C. C D. E.
3 VI ANSWER THE FOLLOWING QUESTIONS IN ONE POINT EACH : 1. Define Axis. 2. What are parallels? 3. Why the heating does becomes less as we move from equator to the poles? 4. What are meridians? 5. What is the International Date Line? 6. Why are shipping and airline routes plotted along great circle? VII ANSWER THE FOLLOWING QUESTIONS IN TWO POINTS EACH : 7. What do you mean by latitude? 8. What do you understand by longitudes? 9. What is the importance of longitudes? 10. Distinguish between local time and standard time. VIII ANSWER THE FOLLOWING QUESTIONS IN FOUR POINTS EACH : 11. Explain how time and date change when one crosses the International Date Line. 12. How is local time determined? IX.A ON THE OUTLINE MAP OF THE WORLD MARK 0 0 LATITUDE AND 0 0 LONGITUDE: X CALCULATE THE TIME OF THE FOLLOWING PLACES USING LONGITUDES: 1) What is the time in Muscat (60 0 E), when it is 12 Noon in London? 2) What is the time in Bridge town (60 0 W), when it is 12 Noon in London? 3) What is the time in Chicago (90 0 W), when it is 12 Noon in London? 4) What is the time in Shanghai (120 0 E), when it is 12 Noon in London?
4 XI. IN THE OUTLINE MAP OF INDIA MARK AND LABEL 82½ 0 E LONGITUDE AND 23 ½ 0 N LATITUDE: SOME GEOGRAPHICAL FACTS The location of a place in relation to another place or nearby land marks is Relative Location. The location of a place using the coordinate system formed by Latitudes and Longitudes is Absolute Location GMT is now officially known as UTC- Universal Time Coordinate As the Earth Moves from west to East, the Places which are to the East of India are ahead of India Time and the places which are to the West of India are behind India Time. The shadow of an object will be shortest at Noon and longest at Sunrise or Sunset
5 INDIAN SCHOOL MUSCAT MIDDLE SECTION DEPARTMENT OF SOCIAL SCIENCE The Globe Latitudes and Longitudes TASK SHEET- 10 M NAME: CLASS VI SEC: ROLL NO: DATE: I FILL IN THE BLANKS: (½ x 10 = 5marks) 1. Lines of Latitude run (horizontally/vertically) 2. Lines of Longitude run (vertically/horizontally) 3. The country which has highest number of time zones is (Russia/USA) 4. Lines of Latitude locate places North or South of the 5. The Prime Meridian is degree Longitude. 6. Lines of Longitude locate places East or West of the 7. It is drawn approximately along the Meridian: 8. The axis is tilted at an angle of to the vertical 9. The lines of Latitude and Longitude combine to make a 10. The time difference between Greenwich Mean Time(GMT) and Indian Standard Time(IST): II ANSWER THE FOLLOWING QUSTIONS AS DIRECTED: 1. Distinguish between local time and standard time. (2marks) LOCAL TIME STANDARD TIME
6 2. Why does the heating becomes less as we move from the equator to the poles? (1mark) IIIOBSERVE THE GIVEN PICTURE AND ANSWER THE FOLLOWING QUESTIONS: (½ + ½ + 1) a) The heat zone that lies between North Pole and Antarctic Circle and between South Pole and Arctic Circle is b) The heat zone that lies between Tropic of Cancer and Tropic of Capricorn is c) Colour the Heat Zones
7 INDIAN SCHOOL MUSCAT MIDDLE SECTION DEPARTMENT OF SOCIAL SCIENCE The Globe Latitudes and Longitudes TASK SHEET- 10 M NAME: CLASS VI SEC: ROLL NO: DATE: I FILL IN THE BLANKS: (½ x 10 = 5marks) 1. Lines of Latitude run horizontally(horizontally/vertically) 2. Lines of Longitude run verticallty(vertically/horizontally) 3. The country which has highest number of time zones is Russia (Russia/USA) 4. Lines of Latitude locate places North or South of the Equator 5. The Prime Meridian is 0 degree Longitude. 6. Lines of Longitude locate places East or West of the Prime Meridian 7. It is drawn approximately along the Meridian: International Date Line 8. The axis is tilted at an angle of 23 ½ 0 to the vertical 9. The lines of Latitude and Longitude combine to make a grid. 10. The time difference between Greenwich Mean Time(GMT) and Indian Standard Time(IST): 5½ hours II ANSWER THE FOLLOWING QUSTIONS AS DIRECTED: 1. Why the heating does becomes less as we move from equator to the poles? (1mark) As we move from equator to the poles the rays of the sun become increasingly slanting and therefore heating becomes less. 2. Distinguish between local time and standard time.(2marks) Each longitude has its own time which is called the local time of that longitude The middle/central longitude of each time zone is taken as the standard meridian and the local time on that meridian is generally followed all over as the standard meridian
8 III OBSERVE THE GIVEN PICTURE AND ANSWER THE FOLLOWING QUESTIONS: (½ + ½ + 1) d) The heat zone that lies between North Pole and Antarctic Circle and between South Pole and Arctic Circle is FRIGID ZONE e) The heat zone that lies between Tropic of Cancer and Tropic of Capricorn is TORRID/TROPICAL ZONE f) Colour the Heat Zones SOME GEOGRAPHICAL FACTS: The location of a place in relation to another place or nearby land marks is Relative Location. The location of a place using the coordinate system formed by Latitudes and Longitudes is Absolute Location GMT is now officially known as UTC- Universal Time Coordinate As the Earth Moves from west to East, the Places which are to the East of India are ahead of India Time and the places which are to the West of India are behind India Time. The shadow of an object will be shortest at Noon and longest at Sunrise or Sunset
Sun Earth Relationships
1 ESCI-61 Introduction to Photovoltaic Technology Sun Earth Relationships Ridha Hamidi, Ph.D. Spring (sun aims directly at equator) Winter (northern hemisphere tilts away from sun) 23.5 2 Solar radiation
More informationSolar Angles and Latitude
Solar Angles and Latitude Objectives The student will understand that the sun is not directly overhead at noon in most latitudes. The student will research and discover the latitude ir classroom and calculate
More informationEarth-Sun Relationships. The Reasons for the Seasons
Earth-Sun Relationships The Reasons for the Seasons Solar Radiation The earth intercepts less than one two-billionth of the energy given off by the sun. However, the radiation is sufficient to provide
More informationWhere on Earth are the daily solar altitudes higher and lower than Endicott?
Where on Earth are the daily solar altitudes higher and lower than Endicott? In your notebooks, write RELATIONSHIPS between variables we tested CAUSE FIRST EFFECT SECOND EVIDENCE As you increase the time
More informationSolar energy and the Earth s seasons
Solar energy and the Earth s seasons Name: Tilt of the Earth s axis and the seasons We now understand that the tilt of Earth s axis makes it possible for different parts of the Earth to experience different
More informationCelestial Observations
Celestial Observations Earth experiences two basic motions: Rotation West-to-East spinning of Earth on its axis (v rot = 1770 km/hr) (v rot Revolution orbit of Earth around the Sun (v orb = 108,000 km/hr)
More informationCoordinate Systems. Orbits and Rotation
Coordinate Systems Orbits and Rotation Earth orbit. The earth s orbit around the sun is nearly circular but not quite. It s actually an ellipse whose average distance from the sun is one AU (150 million
More information1. In the diagram below, the direct rays of the Sun are striking the Earth's surface at 23 º N. What is the date shown in the diagram?
1. In the diagram below, the direct rays of the Sun are striking the Earth's surface at 23 º N. What is the date shown in the diagram? 5. During how many days of a calendar year is the Sun directly overhead
More informationTropical Horticulture: Lecture 2
Lecture 2 Theory of the Tropics Earth & Solar Geometry, Celestial Mechanics The geometrical relationship between the earth and sun is responsible for the earth s climates. The two principal movements of
More informationSECOND GRADE 1 WEEK LESSON PLANS AND ACTIVITIES
SECOND GRADE 1 WEEK LESSON PLANS AND ACTIVITIES UNIVERSE CYCLE OVERVIEW OF SECOND GRADE UNIVERSE WEEK 1. PRE: Discovering stars. LAB: Analyzing the geometric pattern of constellations. POST: Exploring
More informationNoon Sun Angle = 90 Zenith Angle
Noon Sun Angle Worksheet Name Name Date Subsolar Point (Latitude where the sun is overhead at noon) Equinox March 22 nd 0 o Equinox September 22 nd 0 o Solstice June 22 nd 23.5 N Solstice December 22 nd
More informationPre and post-visit activities - Navigating by the stars
Pre and post-visit activities - Navigating by the stars Vocabulary List Adult Education at Scienceworks Pre-visit Activity 1: What is longitude and latitude? Activity 2: Using the Southern Cross to find
More informationLab Activity on the Causes of the Seasons
Lab Activity on the Causes of the Seasons 2002 Ann Bykerk-Kauffman, Dept. of Geological and Environmental Sciences, California State University, Chico * Objectives When you have completed this lab you
More informationGeography I Pre Test #1
Geography I Pre Test #1 1. The sun is a star in the galaxy. a) Orion b) Milky Way c) Proxima Centauri d) Alpha Centauri e) Betelgeuse 2. The response to earth's rotation is a) an equatorial bulge b) polar
More informationFIRST GRADE 1 WEEK LESSON PLANS AND ACTIVITIES
FIRST GRADE 1 WEEK LESSON PLANS AND ACTIVITIES UNIVERSE CYCLE OVERVIEW OF FIRST GRADE UNIVERSE WEEK 1. PRE: Describing the Universe. LAB: Comparing and contrasting bodies that reflect light. POST: Exploring
More informationBasic Coordinates & Seasons Student Guide
Name: Basic Coordinates & Seasons Student Guide There are three main sections to this module: terrestrial coordinates, celestial equatorial coordinates, and understanding how the ecliptic is related to
More informationWhat Causes Climate? Use Target Reading Skills
Climate and Climate Change Name Date Class Climate and Climate Change Guided Reading and Study What Causes Climate? This section describes factors that determine climate, or the average weather conditions
More informationUse WITH Investigation 4, Part 2, Step 2
INVESTIGATION 4 : The Sundial Project Use WITH Investigation 4, Part 2, Step 2 EALR 4: Earth and Space Science Big Idea: Earth in Space (ES1) Projects: Tether Ball Pole Sundial Globe and a Light Indoors
More informationShadows, Angles, and the Seasons
Shadows, Angles, and the Seasons If it's cold in winter, why is Earth closer to the Sun? This activity shows the relationship between Earth-Sun positions and the seasons. From The WSU Fairmount Center
More informationModule 11: The Cruise Ship Sector. Destination #3
Module 11: The Cruise Ship Sector Destination #3 Cruise Destinations Welcome to your third destination. Use the following resource article to learn about the different oceans and time zones. Seen from
More information4 The Rhumb Line and the Great Circle in Navigation
4 The Rhumb Line and the Great Circle in Navigation 4.1 Details on Great Circles In fig. GN 4.1 two Great Circle/Rhumb Line cases are shown, one in each hemisphere. In each case the shorter distance between
More informationThe following words and their definitions should be addressed before completion of the reading:
Seasons Vocabulary: The following words and their definitions should be addressed before completion of the reading: sphere any round object that has a surface that is the same distance from its center
More informationFull credit for this chapter to Prof. Leonard Bachman of the University of Houston
Chapter 6: SOLAR GEOMETRY Full credit for this chapter to Prof. Leonard Bachman of the University of Houston SOLAR GEOMETRY AS A DETERMINING FACTOR OF HEAT GAIN, SHADING AND THE POTENTIAL OF DAYLIGHT PENETRATION...
More informationThe Earth Really is Flat! The Globe and Coordinate Systems. Long History of Mapping. The Earth is Flat. Long History of Mapping
The Earth Really is Flat! The Globe and Coordinate Systems Intro to Mapping & GIS The Earth is Flat Day to day, we live life in a flat world sun rises in east, sets in west sky is above, ground is below
More informationWhich month has larger and smaller day time?
ACTIVITY-1 Which month has larger and smaller day time? Problem: Which month has larger and smaller day time? Aim: Finding out which month has larger and smaller duration of day in the Year 2006. Format
More informationRelationship Between the Earth, Moon and Sun
Relationship Between the Earth, Moon and Sun Rotation A body turning on its axis The Earth rotates once every 24 hours in a counterclockwise direction. Revolution A body traveling around another The Earth
More informationStage 4. Geography. Blackline Masters. By Karen Devine
1 Devine Educational Consultancy Services Stage 4 Geography Blackline Masters By Karen Devine Updated January 2010 2 This book is intended for the exclusive use in NSW Secondary Schools. It is meant to
More informationGrades 3-5. Benchmark A: Use map elements or coordinates to locate physical and human features of North America.
Grades 3-5 Students use knowledge of geographic locations, patterns and processes to show the interrelationship between the physical environment and human activity, and to explain the interactions that
More informationLines on Maps and Globes. Cross Curricular Writing Activity Social Studies Grade 4
Lines on Maps and Globes Cross Curricular Writing Activity Social Studies Grade 4 Fourth Grade Social Studies Standard Map: Chart/Globe The learner will be able to use maps, charts, graphs, and globes
More informationEarth, Sun and Moon. Table of Contents
Earth, Sun and Moon Table of Contents 0. Unit Challenge 1. Earth and Its Motion 2. Earth s Rotation and Revolution 3. Earth s Tilt and Seasons 4. Seasons 5. The Moon 6. The Lunar Cycle 7. Lunar Geography
More informationEarth, Moon, and Sun Study Guide. (Test Date: )
Earth, Moon, and Sun Study Guide Name: (Test Date: ) Essential Question #1: How are the Earth, Moon, and Sun alike and how are they different? 1. List the Earth, Moon, and Sun, in order from LARGEST to
More informationWorld Map Lesson 4 - The Global Grid System - Grade 6+
World Map Lesson 4 - The Global Grid System - Grade 6+ Activity Goal To use the global grid system of latitude and longitude to find specific locations on a world map. Materials Needed: A pencil, a ruler,
More informationASTR 1030 Astronomy Lab 65 Celestial Motions CELESTIAL MOTIONS
ASTR 1030 Astronomy Lab 65 Celestial Motions CELESTIAL MOTIONS SYNOPSIS: The objective of this lab is to become familiar with the apparent motions of the Sun, Moon, and stars in the Boulder sky. EQUIPMENT:
More informationStellarium a valuable resource for teaching astronomy in the classroom and beyond
Stellarium 1 Stellarium a valuable resource for teaching astronomy in the classroom and beyond Stephen Hughes Department of Physical and Chemical Sciences, Queensland University of Technology, Gardens
More informationExploring Solar Energy Variations on Earth: Changes in the Length of Day and Solar Insolation Through the Year
Exploring Solar Energy Variations on Earth: Changes in the Length of Day and Solar Insolation Through the Year Purpose To help students understand how solar radiation varies (duration and intensity) during
More informationAnswers for the Study Guide: Sun, Earth and Moon Relationship Test
Answers for the Study Guide: Sun, Earth and Moon Relationship Test 1) It takes one day for the Earth to make one complete on its axis. a. Rotation 2) It takes one year for the Earth to make one around
More informationThe Celestial Sphere. Questions for Today. The Celestial Sphere 1/18/10
Lecture 3: Constellations and the Distances to the Stars Astro 2010 Prof. Tom Megeath Questions for Today How do the stars move in the sky? What causes the phases of the moon? What causes the seasons?
More informationReasons for Seasons. Question: TRUE OR FALSE. Question: TRUE OR FALSE? What causes the seasons? What causes the seasons?
Reasons for Seasons Question: TRUE OR FALSE? Earth is closer to the Sun in summer and farther from the Sun in winter. Question: TRUE OR FALSE? Earth is closer to the Sun in summer and farther from the
More informationNavigation: Latitude and Longitude
Sextants and Chronometers Help Sailors Find Their Position at Sea Latitude lines run horizontally across the globe and are used to measure distances north and south of the equator. Sailors used a sextant
More informationASTRONOMY 161. Introduction to Solar System Astronomy
ASTRONOMY 161 Introduction to Solar System Astronomy Seasons & Calendars Monday, January 8 Season & Calendars: Key Concepts (1) The cause of the seasons is the tilt of the Earth s rotation axis relative
More informationThe Reasons for the Seasons
The Reasons for the Seasons (The Active Learning Approach) Materials: 4 Globes, One light on stand with soft white bulb, 4 flashlights, Four sets of "Seasons" Cards, Four laminated black cards with 1 inch
More informationCELESTIAL CLOCK - THE SUN, THE MOON, AND THE STARS
INTRODUCTION CELESTIAL CLOCK - THE SUN, THE MOON, AND THE STARS This is a scientific presentation to provide you with knowledge you can use to understand the sky above in relation to the earth. Before
More informationMeasuring the Earth Using a GPS M. Scott Wilkerson & M. Beth Wilkerson, DePauw University, May 10, 2007
Measuring the Earth Using a GPS M. Scott Wilkerson & M. Beth Wilkerson, DePauw University, May 10, 2007 Modified from: Kerski, J.J., 2007, Measuring the Earth s Circumference with GPS, Copyright ESRI,
More informationLatitude, Longitude, and Time Zones
Latitude, Longitude, and Time Zones Typical Graph This is an example of a typical graph. It is made up of points that are connected by a line. Y axis Typical Graph Each point has two values: (4,7) An X
More informationCycles in the Sky. Teacher Guide: Cycles in the Sky Page 1 of 8 2008 Discovery Communications, LLC
Cycles in the Sky What is a Fun damental? Each Fun damental is designed to introduce your younger students to some of the basic ideas about one particular area of science. The activities in the Fun damental
More informationMeasuring Your Latitude from the Angle of the Sun at Noon
Measuring Your Latitude from the Angle of the Sun at Noon Background: You can measure your latitude in earth's northern hemisphere by finding out the altitude of the celestial equator from the southern
More informationEarth Coordinates & Grid Coordinate Systems
Earth Coordinates & Grid Coordinate Systems How do we model the earth? Datums Datums mathematically describe the surface of the Earth. Accounts for mean sea level, topography, and gravity models. Projections
More informationToday. Solstices & Equinoxes Precession Phases of the Moon Eclipses. Ancient Astronomy. Lunar, Solar FIRST HOMEWORK DUE NEXT TIME
Today Solstices & Equinoxes Precession Phases of the Moon Eclipses Lunar, Solar Ancient Astronomy FIRST HOMEWORK DUE NEXT TIME The Reason for Seasons Hypothesis check: How would seasons in the northern
More informationSeasonal & Daily Temperatures. Seasons & Sun's Distance. Solstice & Equinox. Seasons & Solar Intensity
Seasonal & Daily Temperatures Seasons & Sun's Distance The role of Earth's tilt, revolution, & rotation in causing spatial, seasonal, & daily temperature variations Please read Chapter 3 in Ahrens Figure
More informationGeometry and Geography
Geometry and Geography Tom Davis tomrdavis@earthlink.net http://www.geometer.org/mathcircles March 12, 2011 1 Pedagogical Advice I have been leading mathematical circles using this topic for many years,
More informationSolar Energy Systems. Matt Aldeman Senior Energy Analyst Center for Renewable Energy Illinois State University
Solar Energy Solar Energy Systems Matt Aldeman Senior Energy Analyst Center for Renewable Energy Illinois State University 1 SOLAR ENERGY OVERVIEW 1) Types of Solar Power Plants 2) Describing the Solar
More informationLines of Latitude and Longitude
ED 5661 Mathematics & Navigation Teacher Institute Keith Johnson Lesson Plan Lines of Latitude and Longitude Lesson Overview: This lesson plan will introduce students to latitude and longitude along with
More informationWeek 1. Week 2. Week 3
Week 1 1. What US city has the largest population? 2. Where is Aachen? 3. What is the capitol of Florida? 4. What is the longest mountain range in Spain? 5. What countries border Equador? Week 2 1. What
More informationEARTH'S MOTIONS. 2. The Coriolis effect is a result of Earth's A tilted axis B orbital shape C revolution D rotation
EARTH'S MOTIONS 1. Which hot spot location on Earth's surface usually receives the greatest intensity of insolation on June 21? A Iceland B Hawaii C Easter Island D Yellowstone 2. The Coriolis effect is
More informationChapter 3 Earth - Sun Relations
3.1 Introduction We saw in the last chapter that the short wave radiation from the sun passes through the atmosphere and heats the earth, which in turn radiates energy in the infrared portion of the electromagnetic
More informationEarth In Space Chapter 3
Earth In Space Chapter 3 Shape of the Earth Ancient Greeks Earth casts a circular shadow on the moon during a lunar eclipse Shape of the Earth Ancient Greeks Ships were observed to disappear below the
More informationThe Map Grid of Australia 1994 A Simplified Computational Manual
The Map Grid of Australia 1994 A Simplified Computational Manual The Map Grid of Australia 1994 A Simplified Computational Manual 'What's the good of Mercator's North Poles and Equators, Tropics, Zones
More informationEssential Question. Enduring Understanding
Earth In Space Unit Diagnostic Assessment: Students complete a questionnaire answering questions about their ideas concerning a day, year, the seasons and moon phases: My Ideas About A Day, Year, Seasons
More informationIntroduction to Geography
High School Unit: 1 Lesson: 1 Suggested Duration: 3 days Introduction to Lesson Synopsis: The purpose of this lesson is to introduce students to geography and geography terminology, to teach students about
More informationSOLAR CALCULATIONS (2)
OLAR CALCULATON The orbit of the Earth is an ellise not a circle, hence the distance between the Earth and un varies over the year, leading to aarent solar irradiation values throughout the year aroximated
More informationName Period 4 th Six Weeks Notes 2015 Weather
Name Period 4 th Six Weeks Notes 2015 Weather Radiation Convection Currents Winds Jet Streams Energy from the Sun reaches Earth as electromagnetic waves This energy fuels all life on Earth including the
More informationHeat Transfer. Energy from the Sun. Introduction
Introduction The sun rises in the east and sets in the west, but its exact path changes over the course of the year, which causes the seasons. In order to use the sun s energy in a building, we need to
More informationTopographic Maps Practice Questions and Answers Revised October 2007
Topographic Maps Practice Questions and Answers Revised October 2007 1. In the illustration shown below what navigational features are represented by A, B, and C? Note that A is a critical city in defining
More informationToday FIRST HOMEWORK DUE NEXT TIME. Seasons/Precession Recap. Phases of the Moon. Eclipses. Lunar, Solar. Ancient Astronomy
Today FIRST HOMEWORK DUE NEXT TIME Seasons/Precession Recap Phases of the Moon Eclipses Lunar, Solar Ancient Astronomy How do we mark the progression of the seasons? We define four special points: summer
More informationChapter Overview. Seasons. Earth s Seasons. Distribution of Solar Energy. Solar Energy on Earth. CHAPTER 6 Air-Sea Interaction
Chapter Overview CHAPTER 6 Air-Sea Interaction The atmosphere and the ocean are one independent system. Earth has seasons because of the tilt on its axis. There are three major wind belts in each hemisphere.
More informationThe Analemma for Latitudinally-Challenged People
The Analemma for Latitudinally-Challenged People Teo Shin Yeow An academic exercise presented in partial fulfillment for the degree of Bachelor of Science with Honours in Mathematics Supervisor : Associate
More informationRenewable Energy. Solar Power. Courseware Sample 86352-F0
Renewable Energy Solar Power Courseware Sample 86352-F0 A RENEWABLE ENERGY SOLAR POWER Courseware Sample by the staff of Lab-Volt Ltd. Copyright 2009 Lab-Volt Ltd. All rights reserved. No part of this
More informationActivity 10 - Universal Time
Activity 10 - Universal Time Teacher s Guide Scientists use the Universal Time reference to talk about data that is taken around the globe. Universal Time is the time kept in the time zone centered on
More informationThe Orbit TelleriumThe Orbit TelleriumThe Orbit Tellerium
The Orbit TelleriumThe Orbit TelleriumThe Orbit Tellerium 16 Appendix 4 Moon Chart: For each day draw the shape of the Moon, record the time and mark the position of the Moon in the sky in relation to
More informationCELESTIAL MOTIONS. In Charlottesville we see Polaris 38 0 above the Northern horizon. Earth. Starry Vault
CELESTIAL MOTIONS Stars appear to move counterclockwise on the surface of a huge sphere the Starry Vault, in their daily motions about Earth Polaris remains stationary. In Charlottesville we see Polaris
More informationUTM: Universal Transverse Mercator Coordinate System
Practical Cartographer s Reference #01 UTM: Universal Transverse Mercator Coordinate System 180 174w 168w 162w 156w 150w 144w 138w 132w 126w 120w 114w 108w 102w 96w 90w 84w 78w 72w 66w 60w 54w 48w 42w
More informationCHAPTER 5 Lectures 10 & 11 Air Temperature and Air Temperature Cycles
CHAPTER 5 Lectures 10 & 11 Air Temperature and Air Temperature Cycles I. Air Temperature: Five important factors influence air temperature: A. Insolation B. Latitude C. Surface types D. Coastal vs. interior
More informationSunlight and its Properties. EE 495/695 Y. Baghzouz
Sunlight and its Properties EE 495/695 Y. Baghzouz The sun is a hot sphere of gas whose internal temperatures reach over 20 million deg. K. Nuclear fusion reaction at the sun's core converts hydrogen to
More informationStudy Guide: Sun, Earth and Moon Relationship Assessment
I can 1. Define rotation, revolution, solstice and equinox. *Rotation and Revolution Review Worksheet 2. Describe why we experience days and years due to the rotation and r evolution of the Earth around
More informationLecture 2. Map Projections and GIS Coordinate Systems. Tomislav Sapic GIS Technologist Faculty of Natural Resources Management Lakehead University
Lecture 2 Map Projections and GIS Coordinate Systems Tomislav Sapic GIS Technologist Faculty of Natural Resources Management Lakehead University Map Projections Map projections are mathematical formulas
More informationAn Introduction to Coordinate Systems in South Africa
An Introduction to Coordinate Systems in South Africa Centuries ago people believed that the earth was flat and notwithstanding that if this had been true it would have produced serious problems for mariners
More informationEPSG. Coordinate Reference System Definition - Recommended Practice. Guidance Note Number 5
European Petroleum Survey Group EPSG Guidance Note Number 5 Coordinate Reference System Definition - Recommended Practice Revision history: Version Date Amendments 1.0 April 1997 First release. 1.1 June
More informationPHSC 3033: Meteorology Seasons
PHSC 3033: Meteorology Seasons Changing Aspect Angle Direct Sunlight is more intense and concentrated. Solar Incidence Angle is Latitude and Time/Date Dependent Daily and Seasonal Variation Zenith There
More informationGeography affects climate.
KEY CONCEPT Climate is a long-term weather pattern. BEFORE, you learned The Sun s energy heats Earth s surface unevenly The atmosphere s temperature changes with altitude Oceans affect wind flow NOW, you
More informationThe Basics of Navigation
The Basics of Navigation Knowledge of map reading and the use of the compass is an indispensable skill of bushcraft. Without this skill, a walker is a passenger and mere follower on a trip. To become a
More informationNewton s Law of Gravity
Gravitational Potential Energy On Earth, depends on: object s mass (m) strength of gravity (g) distance object could potentially fall Gravitational Potential Energy In space, an object or gas cloud has
More informationSeasons on Earth LESSON
LESSON 4 Seasons on Earth On Earth, orange and red autumn leaves stand out against the blue sky. NATIONAL OCEANIC AND ATMOSPHERIC ADMINISTRATION (NOAA) PHOTO LIBRARY/NOAA CENTRAL LIBRARY INTRODUCTION Nearly
More information6. The greatest atmospheric pressure occurs in the 1) troposphere 3) mesosphere 2) stratosphere 4) thermosphere
1. The best evidence of the Earth's nearly spherical shape is obtained through telescopic observations of other planets photographs of the Earth from an orbiting satellite observations of the Sun's altitude
More informationEarth, Sun and Moon is a set of interactives designed to support the teaching of the QCA primary science scheme of work 5e - 'Earth, Sun and Moon'.
is a set of interactives designed to support the teaching of the QCA primary science scheme of work 5e - ''. Learning Connections Primary Science Interactives are teaching tools which have been created
More informationES 106 Laboratory # 3 INTRODUCTION TO OCEANOGRAPHY. Introduction The global ocean covers nearly 75% of Earth s surface and plays a vital role in
ES 106 Laboratory # 3 INTRODUCTION TO OCEANOGRAPHY 3-1 Introduction The global ocean covers nearly 75% of Earth s surface and plays a vital role in the physical environment of Earth. For these reasons,
More informationExercise 5.0 LUNAR MOTION, ELONGATION, AND PHASES
Exercise 5.0 LUNAR MOTION, ELONGATION, AND PHASES I. Introduction The Moon's revolution in orbit around the center of gravity (barycenter) of the Earth- Moon System results in an apparent motion of the
More informationMoon Phases and Tides in the Planning the D-Day Invasion Part I: The Phases of the Moon
The Science and Technology of WWII Moon Phases and Tides in the Planning the D-Day Invasion Part I: The Phases of the Moon Objectives: 1. Students will determine what causes the moon to go through a cycle
More informationEDMONDS COMMUNITY COLLEGE ASTRONOMY 100 Winter Quarter 2007 Sample Test # 1
Instructor: L. M. Khandro EDMONDS COMMUNITY COLLEGE ASTRONOMY 100 Winter Quarter 2007 Sample Test # 1 1. An arc second is a measure of a. time interval between oscillations of a standard clock b. time
More informationcompass Encyclopedic Entry
This website would like to remind you: Your browser (Apple Safari 7) is out of date. Update your browser for more security, comfort and the best experience on this site. Encyclopedic Entry compass For
More informationActivity 1 Reading Universal Time Level 2 http://www.uni.edu/storm/activities/level2/index.shtml
Activity 1 Reading Universal Time Level 2 http://www.uni.edu/storm/activities/level2/index.shtml National Science Education Standards: As a result of activities in grades 5-8, all students should develop
More informationShadows and Solar Zenith
Shadows and Solar Zenith Name Lab Partner Section Introduction: The solar zenith angle is defined to be the angle between the sun and a line that goes straight up (to the zenith) In reality the sun is
More informationMAPS AND GLOBES: WHERE IN THE WORLD ARE WE?
MAPS AND GLOBES: WHERE IN THE WORLD ARE WE? Grade Level: Kindergarten Presented by: Karen Davis and Tamara Young, Tate Elementary, Van Buren, AR Length of unit:5 lessons I. ABSTRACT A. This unit focuses
More informationPlotting Earthquake Epicenters an activity for seismic discovery
Plotting Earthquake Epicenters an activity for seismic discovery Tammy K Bravo Anne M Ortiz Plotting Activity adapted from: Larry Braile and Sheryl Braile Department of Earth and Atmospheric Sciences Purdue
More informationWhere in the World is the arctic?
Where in the World is the arctic? Summary: Students map the arctic in relation to their home in order to learn the location and countries of the arctic. Grade Level: 3-4; 5-8; K-2 Time one class period.
More informationTry to answer all of these questions. Be prepared to share your answers with a partner, and with the rest of the class.
U1YESCO Module 21: Photovoltaic systems - 'Photovoltaic' (or PV for short) means turning light into electricity Solar PV systems provide electricity from sunlight They can provide power for a wide variety
More informationActivities: The Moon is lit and unlit too
Activities: The Moon is lit and unlit too Key objectives: This activity aims to help student to: Identify the different phases of the Moon Know that the Moon does not produce its own light, but reflects
More informationSolar Flux and Flux Density. Lecture 3: Global Energy Cycle. Solar Energy Incident On the Earth. Solar Flux Density Reaching Earth
Lecture 3: Global Energy Cycle Solar Flux and Flux Density Planetary energy balance Greenhouse Effect Vertical energy balance Latitudinal energy balance Seasonal and diurnal cycles Solar Luminosity (L)
More informationSeasonal Temperature Variations
Seasonal and Daily Temperatures Fig. 3-CO, p. 54 Seasonal Temperature Variations What causes the seasons What governs the seasons is the amount of solar radiation reaching the ground What two primary factors
More informationMATHEMATICS Y6 Geometry 6750 Use co-ordinates and extend to 4 quadrants Equipment MathSphere www.mathsphere.co.uk
MATHEMATICS Y6 Geometry 675 Use co-ordinates and etend to quadrants Paper, pencil, ruler Equipment MathSphere 675 Use co-ordinates and etend to quadrants. Page Concepts Children should be familiar with
More information