UEN Security Office
Technical Services Support Center (TSSC)
Eccles Broadcast Center
101 Wasatch Drive
Salt Lake City, UT 84112
(801) 585-6105 (fax)
1 class periods of 45 minutes each
Globes, flashlights, and a light source are used to model the reason for the seasons.
In your preparations for this activity you will need to be familiar with the causes of the seasons. This background is an attempt to refresh your knowledge about the causes of the seasons.
A misconception that students often have is that because the Earth is closer to the sun in the summer and farther away in the winter, it is hotter in the summer. This answer seems to make perfect sense. If you are closer to a fire, you are warmer. But in relation to the Earth and the sun, this explanation is not correct, especially since the Earth is farther away from the sun in July than it is in January.
Why isn't the Earth's distance a factor in explaining the causes of the changing seasons? The most important reason is that the Earth's orbit or path around the sun is almost circular. The distance of the Earth from the sun does change, but it is so slight that it makes very little difference in the heat energy felt on the Earth. For example, if you were sitting 30 meters from the fireplace and moved 30 centimeters closer, you would not feel that much warmer than what you felt before. Therefore, it is not the Earth's distance from the sun that causes the change in our seasons.
What causes the changes in the seasons on Earth? The two things that make an impact on the seasons are the angle of the Sun above the horizon and how long the sun stays in the sky at a given latitude (the amount of daylight). When the sun is most nearly overhead, the ground gets the hottest. At noon, the sun is at an angle that is most nearly vertical. At sunrise or sunset, the angle from the horizon is smaller so the ground is cooler.
When daylight lasts longer, there is more time for the sun to warm the ground each day. (See attached Daylight Diagram below.)
The angle above the horizon at noontime is important because it determines how much concentrated light and energy the Earth receives at a specific point. An area that receives more light more directly overhead, gets the hottest. Also, the longer the sun is above the horizon on a given day, the longer it will radiate light and energy. This factor is not nearly as important as the angle of the sun above the horizon.
To help illustrate this idea, here is an example you might want to use with your students. Take two round, hollow toilet paper tubes. Point one tube toward the sun at a 90° angle and the other tube at a 45° angle and allow the sunlight to strike the ground. Which ground will be hotter? The 90° angle tube will get more direct, concentrated heat and light energy. With the 45° angle tube, the light is spread out over a larger area, so the light and heat energy is not as concentrated. This illustration demonstrates the sun's affect because of the Earth's tilt.
What causes the Earth to be at a different angle from the sun at different times of the year? The tilt of the Earth's axis is what makes this difference. The angle of the Earth's axis from the plane of its orbit is about 66.5° above the plane, which is 23.5° from being perpendicular to the plane of the Earth's orbit (90° - 66.5° = 23.5° ). The seasons are caused because the Earth is not perpendicular (90° angle) to the Earth's orbit around the sun. (See the attached Orbit Diagram below. Note: this diagram is not drawn to scale.) Though the orbit of the Earth, from this diagram, looks very elliptical, this is due to the nature of the angle of view portrayed. The Earths orbit is nearly circular. For instance, look at a paper plate from above. It looks like a circle. Hold the paper plate horizontal to the ground and slightly below eye level. From this view, the paper plate looks like a severe ellipse--as seen in this diagram. This difference is a source of many misconceptions. It is an important point to discuss with your students.
If your students have either studied the celestial sphere or have done some observations of the sun then it will help them be more prepared for this activity. Students should be made aware that the sun moves across the sky always staying above the same latitude on a given day.
In summary, the reason for the seasons is the angle at which the sun's rays strike the earth, caused the by the tilt of the Earth on its axis. The tilt of the Earth also causes the change in the number of daylight hours experienced throughout the year.
SMALL GROUP ACTIVITY #1
SMALL GROUP ACTIVITY #2
WHOLE CLASS ACTIVITY:
Review student journal entries using the rubric below to check for understanding.
This lesson plan was adapted from Operation Physical Science, NSF grant #8751216 by Dr. Donald Kirwan.