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Activity: Portable Sundial
Learning Objectives (Return to Contents)
Materials List (Return to Contents) Shadow Plot:
Horizontal Sundial
Diptych Sundial:
Introduction/Motivation (Return to Contents) Humans feel it necessary to mark the passage of time. And everyone has noticed shadows changing throughout the day. Someone unknown in the past found out that if a shadow was cast by a sloping object pointing to the celestial pole, it would cast a consistent shadow that would be in the same place at the same time every day. Though it has been suggested that this may have been 2000 years ago, it is more likely that it would have been around 500 years ago; before the development of clocks, it would have been difficult to determine what "the same time each day" meant. Practically everybody knows what a sundial is. Most people have a residual idea that, if they had to, they could make one. But most people's practical knowledge of sundials is confined to having seen standard brass horizontal dials on plinths in gardens. And there is a widespread (though totally wrong) belief that sundials are not very good at telling the time. The poor reputation of sundials is ill deserved, and has arisen mostly because we have all accepted "clock time" as an absolute standard, without devoting any thought to the nature of the time it is measuring. Vocabulary/Definitions (Return to Contents)
Procedure (Return to Contents) Background Sundials measure time as it is. Noon is when the sun is highest in the sky (when it crosses the meridian). Watches measure time as we would like it to be, with noon tomorrow exactly 24 hours, 0 minutes, and 0 seconds away from noon today. But noon on December 26th is actually 24 hours, 0 minutes, and 29 seconds away from noon on Christmas Day. And noon on September 15th is only 23 hours, 59 minutes, and 39 seconds away from noon on the following day. In the winter the days are short and the sun is low in the sky. Each day after the winter solstice, which occurs on December 21st, the sun's path becomes a little higher in the southern sky. The sun also begins to rise closer to the east and set closer to the west until we reach the day when it rises exactly east and sets exactly west. This day is called the equinox. We have the Spring Equinox on March 21st. There is also a Fall Equinox on September 21st. The sun is at its lowest path in the sky on the Winter Solstice. After that day the sun follows a higher and higher path through the sky each day until it is in the sky for exactly 12 hours. Every place on earth experiences a 12-hour day twice a year on the Spring and Fall Equinox. On the Summer Solstice the sun is at its highest path through the sky and the day is the longest. Because the day is so long the sun does not rise exactly in the east, but rises to the north of east and sets to the north of west allowing it to be in the sky for a longer period of time. After the Summer Solstice the sun follows a lower and lower path through the sky each day until it reaches the point where it is in the sky for exactly 12 hours again. This is the Fall Equinox. Just like the Spring Equinox, the sun will rise exactly east and set exactly west on this day and everyone in the world will experience a 12-hour day. After the Fall Equinox the sun will continue to follow a lower and lower path through the sky and the days will grow shorter and shorter until it reaches its lowest path and then we are back at the Winter Solstice where we started. Recommended Resources: http://webexhibits.org/daylightsaving/index.html http://www-istp.gsfc.nasa.gov/stargaze/Secliptc.htm http://www.hps.cam.ac.uk/starry/sundials.html http://www.math.nus.edu.sg/aslaksen/projects/ll-abstract.pdf Preparation Shadow Plot:
Horizontal Sundial:
Diptych Sundial:
Directions There are infinite possibilities for the number of topics this activity can fit with. One suggestion is to discuss/talk with the students about the way time is measured, the history of clocks and the way that we tell time. Construction & Testing: PART I. FINDING GEOGRAPHIC NORTH TO POSITION YOUR SUNDIAL: The sundial must be orientated with the gnomon pointing north/south and, of course, the dial must be located where a shadow will be cast by the gnomon most of the day. Use one of these methods to find geographic north for your latitude. METHOD I: (The Purist's Method) To determine the orientation without reference to other mechanical devices, North can be found by observing Polaris, the North Star, at night. In orientating the sundial, the gnomon is actually being pointed to the North Celestial Pole which is within 1-degree of the North Star. Thus, if you can find Polaris at the end of the Little Dipper, line up your dial by pointing the gnomon towards Polaris. You might want to record the orientation for you dial for future reference. Those in southern latitudes will not be able to use this method. METHOD II: (The Practical Method) A magnetic compass may be used to determine the north/south line, but, because of the difference between magnetic north and true north, the dial reading could be off by an hour or more depending on the local difference between magnetic and true north. METHOD III: (The Lazy Method) To a first approximation, the orientation can be found by finding the orientation at any time from a clock or watch and orientating the dial so the shadow shows the correct time. However, if left in this position, there could be an error of up to 30 minutes over the year as a result of what is known as the "equation of time". Because of the Earth's orbital motion around the sun, the solar day (approximately 24 hours) is not exactly the same length from day to day varying by up to +/- 16 minutes a day. PART II. BUILDING THE SUNDIAL: A. SHADOW PLOT: CONSTRUCTION: (see the Worksheet for images if you need assistance) A shadow plot can also help you obtain a feel for how the sun's path changes across the sky from day to day. To see this effect it is best to work on the shadow plot for several weeks.
USING YOUR SHADOW PLOT:
B. HORIZONTAL SUNDIAL: CONSTRUCTION: To align our gnomon we must position it such that it makes an angle equal to the latitude angle where it will be used with the horizontal face of the sundial (see the Worksheet for images if need assistance). The easiest way to get the nail into the wooden disk at this angle is to do the following:
USING YOUR HORIZONTAL SUNDIAL:
C. DIPTYCH SUNDIAL CONSTRUCTION: (see the Worksheet for images if need assistance) The folding sundial you are about to make is called a diptych sundial. Such dials have been made for four or five centuries and were traditionally made of ivory or boxwood. The diptych dial provided here was designed by Dr. Allan Mills, Astronomy Group, Leicester University, UK. The scanned images and text have been prepared by Dr. Randall Brooks, National Museum of Science and Technology, Ottawa, Canada.
Investigating Questions (Return to Contents)
References (Return to Contents) http://www.sundials.co.uk http://www.sundials.co.uk - Sundials on the internet Yohkoh Public Outreach Project, The Solar Classroom http://solar.physics.montana.edu - Yohkoh Public Outreach Project, The Solar Classroom To find your latitude and longitude. http://www.topozone.com - To find your latitude and longitude. Copyright © 2004 by Worcester Polytechnic Institute including copyrighted works of other educational institutions; all rights reserved.Supporting Program (Return to Contents) Center for Engineering Educational Outreach, Tufts UniversityLast Modified: April 23, 2009
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