Some of the basics

This page isn't really about the basics of astronomy. It's really just an eclectic mix of topics that interest me. On this page you will find:

Eclipse

 A total lunar eclipse

We have two varieties of eclipses - lunar and solar eclipse. An eclipse happens when one object passes through the shadow of another. Let's look first at the most common eclipse, the lunar eclipse.

A lunar eclipse happens when the moon passes through the Earth's shadow. The light from the sun is blocked. The moon is so bright because it reflects the sunlight that shines on it. During an eclipse that light doesn't reach the moon. The reason that the moon often looks red during an eclipse, like the picture above, is because some sunlight does reach the moon after being refracted (bent) through the Earth's atmosphere.

There are two parts to the shadow, the umbra and the penumbra. The umbra is a total shadow whereas only some of the light has been blocked in the penumbra. We can hardly notice when the moon passes through the penumbra. A partial eclipse happens when only part of the moon passes through the umbra. Everyone on the night side of the Earth can see a lunar eclipse.

A diagram showing how the moon slips behind the Earth's umbra, or shadow, during a lunar eclipse

A solar eclipse occurs when the moon passes in front of the Earth, but it requires much more precise alignment. As you can see in the diagram below, only a small part of the Earth can see the total eclipse because the umbra of the moon is so very small. There is also an eclipse known as an annular eclipse. This happens when the moon doesn't quite cover the sun and you can still see an outer ring of the sun. By looking at the diagram, the point of the umbra would actually fall above the Earth's surface rather than one the surface.

A diagram showing how a solar eclipse is caused by the moon's shadow

Kepler's Laws

Before we talk about Kepler's Laws we need to first go over some of the basics of an ellipse.
 
A diagram showing the basics of an ellipse: the semimajor and semiminor axes and the focus The major axis of an ellipse is the long axis, and the minor axis is the shorter axis. A circle is a special case ellipse, with both foci in the center of the circle. The foci are special points in an ellipse. The distance from one point on the ellipse to a focus plus the distance from the same point to the other focus remains constant no matter where you are on the ellipse. In astronomy, we talk about the semimajor and semiminor axes and the eccentricity of the ellipse. The semimajor and semiminor axes are just half the major and minor axes. Eccentricity is a measure of the elongation of an ellipse.

Kepler's 1st Law: The orbit of a planet is an ellipse with the sun at one focus

Both orbits have a semimajor axis a = 1 AU (half the long axis of the orbit), but one orbit is circular and the other is very elliptical. The eccentricity, e, equals 0 for the circular orbit while the elliptical orbit has an eccentricity of about 1/2. Note that a more eccentric (elongated) orbit has a much smaller semiminor (b) axis. The other focus in an elliptical orbit is empty; there is nothing there. A diagram of two orbits with the same semimajor axis but different eccentricities
Here are some orbits that have the star as its focus and the same semimajor axis. The circular orbit stays at the same distance from the star while the highly elliptical orbit approaches extremely close to the star then travels far from the star. Multiple orbits with the same semimajor axis and focus but highly different eccentricities

Kepler's 2nd Law: A line joining the sun and the planet sweeps out an equal area in an equal time.

The explanation for this law centers around the fact that a planet close to the sun orbits faster than one far from the sun. The closer a planet is to the sun the faster it travels. Since orbits are ellipses a planet has a close approach to the sun (perihelion) and a point where it is farthest from the sun (aphelion). When the planet is at perihelion it is traveling faster than average because it is closer to the sun. Conversely, when the planet reaches aphelion it is has a slower than average velocity. A planet travels at different speeds depending on where it is in its orbit. If the planet is moving much faster at perihelion than at aphelion it covers more distance around its orbit when it is close to perihelion than it does near aphelion. This is where Kepler's 2nd Law, also known as the law of equal areas comes in. If you draw an imaginary line between the planet and the sun you find that it sweeps out an equal area in an equal amount of time regardless of where the planet is in its orbit.

A diagram of the perihelion, closest approach to the sun, and aphelion, farthest point from the sun, of an orbit

Kepler's 3rd Law: The square of the sidereal period of a planet is directly proportional to the cube of the semimajor axis of the orbit.

Well, so what the heck does that mean? It really means that the time it takes a planet to orbit the sun is related to how far away the planet is from the sun. Makes more sense stated that way, doesn't it. :)

Kepler's 3rd Law comes down to one equation........P2 = a3

            But only if the period (P) is measured in years and the semimajor axis (a) is measured in astronomical units (AU). Otherwise there is a constant in the equation.

Kepler's 3rd Law does make some logical sense. The farther out a planet orbits from the sun the longer it takes that planet to orbit. It takes longer for two reasons: (1) It is farther out and so has a longer orbit to travel than a planet closer in, and (2) the gravitational pull on the farther planet is not as strong and it moves slower through its orbit relative to the closer planet.
 
 

Why do we have seasons?

The changing of the seasons has nothing to do with how close the earth is to the sun. It all comes down to how much energy is received per area on the earth, and that is determined by the position of the sun in the sky. In the winter the sun is far south in the sky (for us in North America). It does not rise very high overhead and does not stay up for a very long time. With the sun so low, its energy gets spread out over a larger area (a smaller energy per area ratio). The sun always puts out the same amount of energy but in winter it is more spread out, so each individual place, or unit area, receives less energy. Adding to the decreased energy is the fact that the sun is not out very long in the winter, consequently it does not get very warm in the winter. The summer is the opposite situation. During the summer the energy from the sun is more focused because the sun is high in the sky. It rises in the northeast, instead of the southeast, and travels high overhead. Say that during the winter the energy we receive from the sun is spread out over a unit and a half of area. Then in the summertime that same energy could be spread over less than one unit of area. So each unit of area receives more energy in the summer than in the winter.

Today we know that the earth moves, not the sun, and the seasons are controlled by the earth's tilt. The tilt is what makes it look like the sun is moving north and south in the sky. Earth's orbit is nearly circular, so it's not significantly closer to the sun at any time. However, as the tilted earth orbits the sun different parts of the earth are leaning toward the sun, and that is what influences the seasons. During the winter, the northern hemisphere is tilted away from the sun so the energy per area is spread out. Again, the summer months are just the opposite, with the northern hemisphere tilted toward the sun and the energy more focused. Also, the day is much longer in the summer which increases the heating.

You can convince yourself of this by using a flashlight for the sun and a basketball, or other large, round object, as the Earth. Shine the flashlight sun down onto the basketball Earth and tilt the earth at different angles. Notice how the beam that falls on the basketball will spread out or contract as you tilt the basketball.
 
 

One of these things is not like the other

Uranus is a strange planet, and my favorite. Uranus is a fairly typical gas giant, bigger than Neptune and smaller than Saturn. But something happened during Uranus' early life that really knocked it off-center. All of the planets rotate standing up, but Uranus rotates on its side. Somehow Uranus got pushed over and its rotation axis is tilted 98 degrees. To put this into perspective, Earth has a pretty good tilt to its axis but its tilt is only 23 degrees. This means that for much of the year either the north pole or the south pole of Uranus faces the sun. So Uranus is on its side, and so is everything else in that system. Uranus does have thin rings, which look like they run around the north-south pole line. The moons of Uranus also orbit along this line. While the rest of the solar system is standing up Uranus is lying down on the job. How could this have happened? Well on idea is that some large asteroid type object hit Uranus while it was still forming. It was not big enough to break the planet apart but was big enough to knock it over.

Normal planet rotation versus Uranus, which rotates on its side


Is Pluto a Planet?

Do you consider Pluto to be a planet? Whether or not Pluto is a planet really comes down to semantics. How do you decide what is a planet and what isn't. Personally, I don't think Pluto is a planet. I would call it the largest object in a class of objects contained in the Kuiper Belt. Let me make my case. It is most likely that Pluto and Charon are captured items from the Kuiper Belt. Whether or not you want to call Pluto a planet is up to you. It does orbit the sun but it is not similar to any other planets. If you'd like to take that route you could call Jupiter and its moons a mini solar system. Some of Jupiter's moons are so big that if they were orbiting the sun rather than Jupiter we would gladly call them planets. Where do you draw the line?

Last updated by Jill Jacobs, 19 August 2000
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