There are 9 planets thus far discovered in our solar system. The first
four planets are tiny, rocky globes called terrestrial
planets:Mercury, Venus, Earth, and Mars. Of these, the Earth is
the largest. Rocky but not a planet is the Asteroid Belt, the clumpy
remains of a failed planet.
Jupiter is the 5th planet out from the Sun, just past the asteroid
belt. It is 5.2 times further away from the Sun than is the Earth. At 11 times the
diameter of Earth, Jupiter dwarfs the Earth
in size, yet is in turn dwarfed by the Sun which is 10 times larger in
diameter than it. Saturn is the only planet
which comes close to equaling Jupiter's impressive size, and even then it is
still less than one third the mass and only 60% of the volume of Jupiter. The
outer gas
giants, Uranus
and Neptune, are even smaller yet, being only 4 times larger in
diameter than Earth!
Pluto resembles little more than a double comet with its moon,
Charon. Smaller than even our Moon, PLuto is almost 40 times further
from the Sun than is our Earth.
The table below shows you the actual values of
diameter and distance from the Sun for all of the known planets.
The story of Jupiter has already told you
much about the planet Jupiter and its moons, and how they all relate
to the other bodies of the Solar System. However, the information may
or may not have made much sense without knowing more about the other
bodies in the Solar System. 
| Planet | Distance
(from Sun) km...A.U. | Diameter |
|---|---|---|
| Mercury | 57,910km...0.39 | 2,439km |
| Venus | 108,200km...0.72 | 6,052km |
| Earth | 149,600km...1.00 | 6,378km |
| Mars | 227,940km...1.50 | 3,397km |
| Jupiter | 778,330km...5.20 | 71,492km |
| Saturn | 1,429,400km...9.50 | 60,268km |
| Uranus | 2,870,990km...19.20 | 25,559km |
| Neptune | 4,504,300km...30.10 | 24,764km |
| Pluto | 5,913,520km...39.50 | 1,160km |
ACTIVITY 1 Part 1: A Classroom Solar System
If it takes around twelve hundred Earths to fill up Jupiter and about twelve hundred Jupiters to fill the Sun, it becomes difficult to represent this in a clear model! However, if we imagine the Sun is a ball 9 feet across, we can build a scaled down representation of our solar system.
To make this model, the ceiling of the classroom or nearby room must be able to support a few pounds of weight spread over a small distance. Teachers may want to investigate the strength of the ceiling and its physical ability for attaching a hanging mobile. Paneled tile ceilings are great as they have nooks for hooks, wooden ceilings allow minor hook & eyes to be installed, and rooms with lots of overhead pipes are ideal for slinging strings around. Please consider which method of fixture before attempting this activity.
The following objects are appropriate in size to help us visualize the relative proportions of sizes of one planet to another:
| Planet | Scale Object |
|---|---|
| Mercury | marble |
| Venus | walnut |
| Earth | golf ball |
| Mars | acorn |
| Jupiter | basketball |
| Saturn | soccer ball |
| Uranus | soft ball |
| Neptune | small grapefruit |
| Pluto | kidney bean |
MATERIALS:Items listed above; paper mache, paper; pencils; markers, paint, string, long pipe cleaners or thin wire, spherical rubber balloons, and small paper clips.
bend some pipe
cleaner or thin wire into a circle made to the diameter of the rings,
but bend one end of the circle inwards, like G, enough that it reaches
the paper mache ball and can be (but NOT yet!) inserted CAREFULLY into
the side via a hole pricked there by a sharp object. For
sturdiness, students may want to loop two wires and bend the wire on the other side
inwards as well to look like an O with a belt on. Place the ring of
wire on to a big piece of paper folded in half and trace around it --
but 1 inch away from it on both sides, so you make a big
doughnut. Because the paper is folded, two doughnuts will be
available. Cut these doughnut out after painting thenm as rings to
satisfaction, and sandwich glue them around the wire. When the glue has dried, slip the rings over the planet and insert the bent bits into the pricked holes in the side. Glue these bits if necessary. NOTE: Uranus is a planet which is kicked over on its side, so its rings are vertical, not horizontal!
DISCUSSION:
Students may see a pattern in the sizes and groupings of the planets. What happens to the size with distance from the Sun? The color? Rings? Which planet does not seem to fit into the pattern? Do students see how Jupiter is the dominant planet? Students should recall what the Sun would look like if placed in their classroom using this scale. It would have to be nine feet high and nine feet wide!
MATERIALS: Playground or field; letter-sized sheet of paper for each planet; markers.
DISCUSSION:
Are the planets evenly spaced? Is there some pattern you can find which seems to fit what is seen? Could you find some mathematical equation which would fit the pattern? How does a planet's distance from the Sun relate to its temperature? Should planets nearer the Sun be hotter or cooler than those farther away? The next activity will help answer this question.
Gravity and Jupiter
Newton's First Law of Motion states that an object at rest will tend to stay at rest and an object in motion will tend to stay in motion in a straight line, unless acted upon by an external, unbalanced force. If one rolls a ball on a level surface, it will travel in a straight line until the force of friction stops it. There's no air or carpeting to slow the planets in their orbits, but the planets don't travel in straight lines through space; they travel around in nearly circular orbits. There must be another force acting upon them. That other force is gravity. When we experience gravity in our everyday lives, i.e.; why we don't float around, the force is usually between two objects of very different masses: one very massive (like the Earth) and another with negligible mass (like a person). Because of this fact, we often simply think of gravity as some property of very massive objects like planets and stars. In reality, though, gravity is a characteristic of mass. All mass has gravity, and the amount of gravity is governed by the amount of mass. Thus, any mass can feel all other masses because of the common fact that any mass has gravity; however, the combined gravity will govern the amount of tug on the masses. So, eventhough the Earth is enormous compared to you, the Earth pulls on you only as much as you pull on the Earth. Since the Earth is much more massive than you, though, you won't notice the infinitesimal amount the Earth moves towards you, but you can't help but notice how you fall to Earth! There is also gravitational attraction between you and, say, your desk, but neither you nor your desk have enough mass to make that force noticeable. The gravitational force between two bowling balls can be measured in the laboratory with very sensitive instruments, however!
In the formation of the solar system, every object formed with a speed in some direction; however, every object also has an amount of mass equal to the amount of stuff inside of them. For example, Jupiter's mass tugs on the mass of its moons like the mass of the Earth tugs on us and keeps us on the ground. So why don't the moons just fall on to Jupiter and stick there? The gravity of Jupiter pulls the moons towards it but each of its moons is trying to speed past it in some direction. As Jupiter tugs inward, the moon has its own speed sideways -- the combination is the moons orbit around Jupiter in nearly circular orbits.
If the Sun is so incredibly massive, why should anything want to orbit around a less massive planet like Jupiter? Gravity is very powerful, but is actually limited: you will feel it less and less the further away from the mass you get.
Since gravity's force decreases as you move further away from the source of mass, a little moon which is born really close to a planet will orbit that planet, eventhough the planet is less massive than the Sun.
The students can understand this with a simple activity.
ACTIVITY 2: Gravity and Orbit Simulation
DISCUSSION:Each group should have discovered that the ball orbits much faster when the length of tights is shortened and much slower when the length of tights is increased. In physics, this is because your hand is giving the ball a speed to set it in motion but the tights are keeping the ball in place. However, the tights act as a force tugging the ball towards your hand. The stronger the tug (the shorter the tights) the faster the ball has to spin to keep itself from just getting tugged in. In contrast, the weaker the tug (the longer the tights) the ball does not need to orbit so quickly. So what does this have to do with Jupiter and its moons? Those moons which are closer to the planet orbit much faster than those further away, just like the faster spinning ball on the shorter length of tights. Thus, Io, one of the closest moons to Jupiter, orbits the huge planet in a little under two days, while Callisto, one of the furthest of Jupiter's moons, takes more than 16 days to complete an orbit.
This is also the same with the planets around the Sun. Where it takes the Earth one year to orbit the Sun, it takes Jupiter about 12 years. Can you imagine now the distances required to make something which is orbiting at almost 30,000 mph to take 12 years to go around?
Jupiter, like all of the planets, possesses a magnetosphere, or a spherical region of magnetic influence. This means that Jupiter resembles a large bar magnet, so the magnetic characteristics of a large bar magnet are true for Jupiter. But what are the characteristics of a large bar magnet?
Magnetism is another one of those forces (like gravity) which can be felt by those materials which can make it. Magnets are materials whose particles are aligned rigidly and can force alignment in magnetically sensitive materials which come in contact with them. Like gravity, magnetic force diminishes with distance, but in a specific pattern. Since Jupiter acts like a huge bar magnet, it also shares a similar pattern of magnetic force around it like the bar magnet. The pattern is called a set of magnetic field lines.
DISCUSSION:
What can you see in the pattern? How extensive is this pattern and where are the moons in all of this? What about the other planets?
Students should discover that the pattern reaches well into the orbit of Saturn! The most intense portions of the pattern are in the area of space where the little Galilean moons orbit. What implications does this have for these moons?
Io, since it is volcanic, is often effusing particles into space. These particles get caught up along the magnetic field lines and travel to the atmosphere of Jupiter. There, these particles disturb the atmosphere which in turn gives off radio waves. The final and most complex activity involves the building of a radio telescope to pick up these emissions.
ACTIVITY
3: The Jovian Basketball Hoop
MATERIALS:short-wave radio, 66 inches of stiff copper wire, a length of coaxial cable, 2ft square of metal screen or chicken wire, dowels enough to make 4, 12-inch lengths, wood saw, knife, and tape.

DISCUSSION:
What have students learned about astronomical observing? Is it possible to make detailed observations with even the crudest of instruments? Were students surprised to be able to make observations in the daytime? Why can the Jovian Hoop "see" Jupiter but our eyes cannot? Hint: why is the sky blue? Which was more fun -- making the Jovian Hoop, predicting the results, or listening to Jupiter? Do answers to this question show students that astronomy can be engineering, theory, and observation?


By Jove, I Think
We've Got It!: Jupiter ResourcesBack to the Introduction to the Jupiter Pages
About the Astronomy in Motion Project
To the HEAD Science Education Page
Comments? Suggestions? Questions? Please contact our project group at: STAR These pages designed by Tania Ruiz. Last updated Oct. 2, 1995.