APPENDIX F ACTIVITY #1 - CALCULATION OF THE TILT OF THE EARTH S AXIS AND THE OBSERVER S LATITUDE

Similar documents
Gnomon (a thin, round stick at least a foot long and capable of being put into the ground or stood up vertically)

Motion of the Sun. motion relative to the horizon. rises in the east, sets in the west on a daily basis. Basis for the unit of time, the DAY

C) wavelength C) eastern horizon B) the angle of insolation is high B) increases, only D) thermosphere D) receive low-angle insolation

Practice Questions: Seasons #1

Earth s Orbit. Sun Earth Relationships Ridha Hamidi, Ph.D. ESCI-61 Introduction to Photovoltaic Technology

Appearance of the Sky Orientation Motion of sky Seasons Precession (?)

Which Earth latitude receives the greatest intensity of insolation when Earth is at the position shown in the diagram? A) 0 B) 23 N C) 55 N D) 90 N

Appearance of the Sky Orientation Motion of sky Seasons Precession (?)

The Celestial Sphere. Chapter 1. Constellations. Models and Science. Constellations. Diurnal vs. Annular Motion 9/16/2010

2.2 The Reason for Seasons

Sundials and the Celestial Sphere. Katie Hausknecht

For most observers on Earth, the sun rises in the eastern

Chapter 1 Image Slides. Copyright The McGraw-Hill Companies, Inc. Permission required for reproduction or display.

Practice Questions: Seasons #2

The Sun-Earth-Moon System

Daily Motions. Daily Motions. Solar and Sidereal Days. Annual Motions of the Sun. Coordinate system on Earth. Annual Motion of the Stars.

LAB: What Events Mark the Beginning of Each Season?

November 20, NOTES ES Rotation, Rev, Tilt.notebook. vertically. night. night. counterclockwise. counterclockwise. East. Foucault.

ZW2000 and Your Vertical Sundial Carl Sabanski

SOLAR ENERGY: THAT S HOT Grades 4-6

Photovoltaic Systems Solar Radiation

Earth s Motion. Lesson Outline LESSON 1. A. Earth and the Sun 1. The diameter is more than 100 times greater than

Observing the Universe for Yourself

Chapter 1: Discovering the Night Sky. The sky is divided into 88 unequal areas that we call constellations.

UNIT 3: EARTH S MOTIONS

Astronomy 291. Professor Bradley M. Peterson

C) the seasonal changes in constellations viewed in the night sky D) The duration of insolation will increase and the temperature will increase.

Before you Sit. Please Pick-up: Blue Information Sheet for Evening Observing. 1 Red and 1 Blue ticket for Observing/ Planetarium

Viewed from Earth's north pole, the rotation of Earth and its moon are counter-clockwise.!

Chapter 2 Discovering the Universe for Yourself

Seasons. What causes the seasons?

CA1 2.11: Designing an Equatorial Sundial Activity

(1) How does the annual average sun angle at solar noon (that is, the sun angle at noon averaged over a full year) depend on latitude?

Chapter 1 Solar Radiation

Polar Sundial. Cut carefully on this line. Cut on this line.

Earth Science Seasons Test Name Per Date

ZW2000 and Your Sundial

LAB 2: Earth Sun Relations

Brock University. Test 1, October 2016 Number of pages: 9 Course: ASTR 1P01 Number of Students: 500 Date of Examination: October 3, 2016

Which table correctly shows the dates on which the apparent paths of the Sun were observed? A) B) C) D)

Alien Skies. Todd Timberlake

Aileen A. O Donoghue Priest Associate Professor of Physics

Earth is rotating on its own axis

How can we describe the motion of the sun in the sky? Where is the Sun at noon today? What about the path of the Sun?


The following terms are some of the vocabulary that students should be familiar with in order to fully master this lesson.

Chapter 2 Discovering the Universe for Yourself

Chapter 2 Discovering the Universe for Yourself. What does the universe look like from Earth? Constellations. 2.1 Patterns in the Night Sky

Page 1. Name:

ME 476 Solar Energy UNIT THREE SOLAR RADIATION

Reminder: Seasonal Motion

HEATING THE ATMOSPHERE

Earth-Sun Relationships. The Reasons for the Seasons

[04] Seasons, Phases, and Eclipses (9/7/17)

Midterm Review #2-2018

drinking straw, protractor, string, and rock. observer on Earth. Sun across the sky on March 21 as seen by an

CHAPTER 2 A USER'S GUIDE TO THE SKY

Chapter 2 Discovering the Universe for Yourself. Copyright 2012 Pearson Education, Inc.

5 - Seasons. Figure 1 shows two pictures of the Sun taken six months apart with the same camera, at the same time of the day, from the same location.

(1) Over the course of a day, the sun angle at any particular place varies. Why?

2.1 Patterns in the Night Sky

C) D) 2. The diagram below shows a large pendulum in motion over an 8-hour period.

LOCATING CELESTIAL OBJECTS: COORDINATES AND TIME. a. understand the basic concepts needed for any astronomical coordinate system.

STANDARD. S6E1 d. Explain the motion of objects in the day/night sky in terms of relative position.

Vigyan Pratibha Learning Unit (Teacher version) Shadows

Astronomy 101: 9/18/2008

CHAPTER 3. The sun and the seasons. Locating the position of the sun

Geography Class 6 Chapters 3 and

Exploring more with seasons Name: Block

Seasons ASTR 101 2/12/2018

Sunlight and its Properties Part I. EE 446/646 Y. Baghzouz

Group 7 CHEN MING SHEN ALEXANDER (U041436L) CHENG SUH JENG (U042983R) GAO HE (U052142J) NG LIN YIN (U032435W) YANG JIE (U058644M)

ASTRO Fall 2012 LAB #2: Observing the Night Sky

Earth & Space Science, Interpreting Data DURATION Preparation: 5 minutes Activity: 40 minutes (total over one day)

The celestial sphere, the coordinates system, seasons, phases of the moon and eclipses. Chapters 2 and S1

Lecture #03. January 20, 2010, Wednesday

Physics Lab #4:! Starry Night Student Exercises I!

Sun Inclinometer. Curriculum Levels 3-4 Maths. Activity Description

Chapter 2 Lecture. The Cosmic Perspective Seventh Edition. Discovering the Universe for Yourself Pearson Education, Inc.

Planet Earth. Part 2

Sunlight and its Properties II. EE 446/646 Y. Baghzouz

March 21. Observer located at 42 N. Horizon

NAEP released item, grade 8. The following question refers to shadows created by sunlight.

A2 Principi di Astrofisica. Coordinate Celesti

Science : Introduction to Astronomy. Lecture 2 : Visual Astronomy -- Stars and Planets. Robert Fisher

Name: Exam 1, 9/30/05

Fundamentals of Satellite technology

Using Angles. Looking at the Night Sky. Rising and Setting Stars. Nightly Motion of the Stars. Nightly Motion of the Stars

Aim: What causes Seasons?

L.O: EARTH'S 23.5 DEGREE TILT ON ITS AXIS GIVES EARTH ITS SEASONS March 21 (SPRING), June 21(SUMMER), Sept 22 (AUTUMN) & Dec 21(WINTER)

Chapter S1 Celestial Timekeeping and Navigation. How do we define the day, month, year, and planetary time periods?

ClassAction: Coordinates and Motions Module Instructor s Manual

THE SUN. LENGTH: Course of the semester

Module 2: Mapping Topic 2 Content: Determining Latitude and Longitude Notes

Brock University. Test 1, October 2017 Number of pages: 9 Course: ASTR 1P01, Section 1 Number of Students: 470 Date of Examination: October 3, 2017

HNRS 227 Fall 2007 Chapter 14. Earth in Space presented by Prof. Geller 25 October 2007

Physics 312 Introduction to Astrophysics Lecture 3

1.4j interpret simple shadow stick data to determine local noon and observer s longitude

Chapter 2 Lecture. The Cosmic Perspective Seventh Edition. Discovering the Universe for Yourself

The Sun-Earth-Moon System

Transcription:

APPENDIX F ACTIVITY #1 - CALCULATION OF THE TILT OF THE EARTH S AXIS AND THE OBSERVER S LATITUDE The calculation of the Tilt of the Earth s Axis and the Observer s Latitude is essentially a reversal of the calculation sequence shown for the construction of the enclosure (Appendix A). In the discussion below, tip of the gnomon can usually be read in lieu of opening of the enclosure for participants who use a gnomon to cast a shadow instead of an enclosure with an opening to pass a light ray. Step 1: setup a coordinate system with: P(0,0,0) at the opening of the enclosure / tip of the gnomon. the x-axis as east / west (positive being eastward). the y-axis as north / south (positive being northward). the z-axis as up / down (positive being upward). Note that the analemma is in the x-/y-plane at z = -h. Step 2: Locate the point both directly below the opening in the enclosure and in the plane containing the analemma this point will be referred to as P(0,0,-h). For the construction described in Appendix A, a heavy sewing needle works well when suspended through the opening by a thread on a windless day with the enclosure in its observing position. Step 3: Make the following three measurements from P(0,0,-h) (determined in Step-1 above): Distance from the opening in the enclosure to the plane in which the analemma lies; in Appendix A, this distance is referred to as h Distance to the Summer Solstice point. This is the point on the analemma curve closest to the x-axis. Distance to the Winter Solstice point. This is the point on the analemma curve farthest from the x-axis.

Step 4: Using the measurements above, calculate the altitude of the Sun at both Summer and Winter Solstices: (AltSummerSolstice) = arctan(h / (DistanceToSummerSolsticePoint) ) (AltWinterSolstice) = arctan(h / (DistanceToWinterSolsticePoint) ) Step 5: Specify the relationships between the altitude of the Sun at Summer Solstice, the tilt of the Earth s axis, and the Observer s Latitude. With reference to the sketch below, specifically the 90 angle between the Observer s southern horizon and the Observer s zenith: (AltSummerSolstice) + (ObsLatitude) (TiltOfAxis) = 90 The altitude of the Sun at Summer Solstice (AltSummerSolstice) is calculated from the dimensions of the analemma and the observing apparatus (Step 3). (ObsLatitude) (TiltOfAxis) = 90 - (AltSummerSolstice)

Step 6: Specify the relationships between the altitude of the Sun at Winter Solstice, the tilt of the Earth s axis, and the Observer s Latitude. With reference to the sketch below, specifically the 90 angle between the Observer s southern horizon and the Observer s zenith: (AltWinterSolstice) + (ObsLatitude) + (TiltOfAxis) = 90 The altitude of the Sun at Winter Solstice (AltWinterSolstice) is calculated from the dimensions of the analemma and the observing apparatus (Step 3). (ObsLatitude) + (TiltOfAxis) = 90 - (AltWinterSolstice)

Step 7: Specify the Observing Latitude by adding the equations from Step 4 and Step 5, above: (ObsLatitude) (TiltOfAxis) + (ObsLatitude) + (TiltOfAxis) = 90 - (AltSummerSolstice) + 90 - (AltWinterSolstice) 2*(ObsLatitude) = 2*90 - (AltSummerSolstice) - (AltWinterSolstice) Again, rearranging the equation gives: (ObsLatitude) = 90 - ( (AltSummerSolstice) + (AltWinterSolstice) ) / 2 Use the solar altitudes calculated in Step 3, above. Step 8: Specify the Tilt of the Earth s Axis by subtracting the equation from Step 4, above, from the equation from Step 5, above: (ObsLatitude) + (TiltOfAxis) (ObsLatitude) + (TiltOfAxis) = 90 - (AltWinterSolstice) 90 + (AltSummerSolstice) 2*(TiltOfAxis) = (AltSummerSolstice) (AltWinterSolstice) Again, rearranging the equation gives: (TiltOfAxis) = ( (AltSummerSolstice) (AltWinterSolstice) ) / 2

Use the solar altitudes calculated in Step 3, above. Additional Links Printable Version of this page Return to Introduction page Appendix A Construction of an Enclosure Appendix B Overview of Non-Local Noon Observing Appendix C Unattended Photography Appendix D * * * Reserved for Future Use * * * Appendix E * * * Reserved for Future Use * * * Appendix G Activity #2 (Path of the Sun in the Sky) Appendix H Activity #3 (Equation of Time) Appendix I Activity #4 (Eccentricity of Orbit)