Naked Eye Astronomy

Introduction to Astronomy
and
Astronomy Without a Telescope

This set of notes by Nick Strobel covers: Introduction to astronomy, Naked eye astronomy (note to Jesse Helms and Sen. Exon: that means astronomy without the use of a telescope). The vocabulary terms are italicized.

Contents

Introduction

Index

I'll start by setting the stage for what we're up against when we try to understand the physical universe in the discipline we call astronomy or astrophysics. The next section will cover everything we notice by taking a look at the sky without the use of a telescope.

The movie Powers of Ten gave you some idea of the size scales involved in astronomy. Now let's try to get a feel for the time scales. I'll use the analogy of the cosmic calendar in which every second in the calendar corresponds to 475 normal years (so 24 calendar days = 1 billion regular years). Assuming that the universe is 15 billion years old, we can squeeze that huge timescale to one cosmic calendar year. Here are some important dates relevant to us humans:

   Origin of the Universe--Jan. 1.                     Origin of our galaxy--May 1.
   Solar system origin--Sept. 9.                       Earth Formation--Sept. 14.
   Life on Earth--Sept. 30.                            Sexual reproduction advent--Nov. 25.
   Oxygen atmosphere--Dec. 1.                          Cambrian explosion (600 mil years ago
                                                       when most complex organisms
                                                       appear, fish, trilobites)--Dec. 17.
   Land plants & insects--Dec. 19, 20.             First amphibians--Dec. 22.
   First reptiles & trees--Dec. 23.                First dinosaurs--Dec. 25.
   KT impact, mammal age, birds--10:00 AM Dec. 30.     First primates--Dec. 30.
   Australopithicenes (Lucy, etc.)--10:00 PM Dec. 31.  Homo habilis--11:25 PM Dec. 31.
   Homo erectus--11:40 PM Dec. 31.                     Early Homo sapiens--11:25 PM Dec. 31.
   Neanderthal man--11:57 PM Dec. 31                   Cro-Magnon man--11:58:38 PM
   Homo sapiens sapiens--11:58:57 PM Dec. 31.          Human history--11:59:39
   Ancient Greeks to now--last five seconds.           Average human life span--0.15 seconds.

It is rather surprising that we've been able to discover so much about the long term evolution of the universe and the things in it, especially when you consider that we've only been seriously observing the universe for about 100 years, which is only a very slight fraction of the universe's lifetime. About 100 years ago is when photography was first used in astronomy, making truly systematic observation programs possible. How can we say that the sun will go through a red giant phase in about 5 billion years from now with confidence? Is it hubris to confidently talk about the Earth's formation process about 4.5 billion years ago? To give you an idea of the difficulties in studying long timespans consider this analogy: An alien comes to Earth to search for life and to understand how it evolved. ET has a camera and has just 15 seconds to take as many photographs as possible. Fifteen seconds is the same proportion of a human lifetime as the 100 years is to the universe's age (15 seconds/human lifetime = 100 years/universe age). ET returns home and her colleagues try to understand Earth from this 15 second period of snapshots. They won't see any important evolutionary changes. How will they determine the dominant life form? They could use a variety of criteria: 1) Size: leads them to choose whales or elephants; 2) Numbers: choose insects; 3) amount of land space controlled by one species: choose automobiles.

Suppose they somehow decide humans are dominant. They now have further problems. There is considerable diversity among the humans (though to ET with 10 tentacles, 200 eyes, and a silicon outer shell, the humans all look alike!). ET and colleagues try to systematically classify the humans. The humans come in a variety of sizes. In a coarse classification scheme, they break the sizes down into small, medium, and large. They also come in variety of optical colors for their outer shell: red, black, brown, yellow, and white. There appears to be 2 separate sexes (ET is both male and female). After some false starts with theories that used hair length and eye color, they are ready to ask themselves, ``Do small, brown, female humans evolve into large, red, male humans?'' ``Do the small stay small and the large stay large?'' ``Why is there a tendency for small humans to be with one or two large humans?'' With the three characteristics [size (3 divisions), color (5 divisions), and sex (2 divisions)], ET has 3x5x2 different combinations and 30x30 possible evolutionary schemes to consider! Well, the universe has a lot more characteristics and, therefore, many more combinations to consider!

Science in General

Index

The scientist usually learns about nature by using controlled experiments in which only one thing at a time is varied, and the experiments can be repeated by anyone as many times as they want to verify that the effect is reproducible. The astronomer cannot do controlled experiments. We cannot even examine things from a variety of angles. What we do is collect light and other radiation from celestial objects and use all of our information and creativity to interpret the signals from afar. We try to look for the experiments nature has set up for us and hone on a few basic characteristics at a time. Like any scientist, the astronomer makes observations, which suggest hypotheses. These speculations are made into predictions of what may be observed under slightly different observing and/or analysis circumstances. The astronomer returns to the telescope to see if the predictions pan out or if some revision needs to be made in the theory. Theory and observation play off each other.

Often the evidence for a particular hypothesis is indirect and will actually support other hypotheses as well. The goal is to make an observation that conclusively disproves one or more of the competing theories. Currently unresolvable questions may be resolved later with later improved observations using more sophisticated/accurate equipment. Sometimes new equipment shows that previously accepted theories/hypotheses are wrong!

Value of Astronomy in the Scientific Endeavor

Index

However, not all is negative. The universe gives us a vast number of different phenomena to observe. Many of these things cannot be reproduced in Earth laboratories. There are gas clouds in such a rarefied state that they give off radiation not seen on Earth. Some objects are so dense that their gravitational fields bend light so much that it is prevented from leaving the object! Many things that are unlikely or impossible on Earth are routinely observed in the cosmos. Many of the scientific theories in other fields make predictions of what would happen under very extreme circumstances. Sometimes those extreme circumstances are the only situations distinguishing two or more contradictory theories. Unfortunately, the scientists of those other disciplines cannot test their ``wild'' ideas-is it hogwash or reality? Astronomy allows those theories to be tested. Very subtle and easily missed but crucial processes may be missed by observers focussing on the Earth, but the astronomer can see those processes magnified to easily noticeable levels in some other celestial object.

Now back to the long term evolution side of the coin. We actually have a time machine! Not the H.G. Wells variety or G. Roddenberry's Gate of Eternity but something much simpler due to the large distances and finite speed of light (300,000 km/sec!). It takes time for radiation from a celestial object to reach us. Therefore, when we examine an object at a large distance from us, we see it as it was. The farther away the object is, the longer it took the radiation to reach, and the further back in time we observe it. The sun is 150 million kilometers from us, so we see the sun as it was 8 1/3 minutes ago. The farthest object you can see without a telescope is the Andromeda galaxy about 1.9*10^19 km from us so we see it as it was a little over 2 million years ago. By the way, we'll use a more convenient length scale than the really short kilometer. We'll use a light year which is equal to the distance light travels in one year (about 9.46*10^12 km). So the Andromeda galaxy is a little over 2 million light years away from us.

To study the evolution of long-lived objects like stars (with lifetimes of millions to billions of years) or galaxies, we observe the object of interest at different distances from us so we see it at different epochs. We then see the object at various different ages or evolutionary stages.

Sky Observations Without Telescopes

Index

Celestial Sphere Defined

Now that we have some feeling for the scales of time and space that astronomy encompasses and some of the difficulties caused by being Earth-bound (well, okay: solar-system bound!), let's take a look at what is up there in the sky beyond the clouds. For the first few weeks of the course, we'll use a simple model of the sky that any observer would consider reasonable or at least workable. Imagine the sky as a great, hollow, sphere surrounding the Earth. The stars are attached to this sphere-some bigger and brighter than others-which rotates around the stationary Earth roughly every 24 hours. Alternatively, you can imagine the stars as holes in the sphere and the light from the heavens beyond the sphere shines through those holes. Of course, we now know that a star's apparent brightness is determined by its distance, as well as, its physical size and temperature. We also know that it is actually the Earth that is rotating. This imaginary sphere is called the celestial sphere, and has a very large radius so that no part of the Earth is significantly closer to a given star than any other part. Therefore, the sky always looks like a great sphere centered on our position. The celestial sphere (and, therefore, the stars) appears to move westward-stars rise in the east and set in the west.

Why a sphere? The Earth is spherical! This was known much earlier than Columbus' time. Sailors had long known that as a ship sailed away from the shore it not only diminished in apparent size, but it also appeared to sink into the water. The simplest explanation to use was that the Earth was curved (particularly, since those ships did come back without falling off some edge!). They also knew that if one traveled in a north-south direction, some stars disappeared from view while others appeared. The simplest explanation said that the Earth is round, not flat. Pythagoras noted that the shadow of the Earth falling on the Moon during a lunar eclipse was always curved and the amount of the curvature was always the same. The only object that always casts a circular shadow regardless of its orientation is a sphere. We know about this Pythagorean argument through the writings of Aristotle.

Reference Markers

Index

Now for some reference makers: The stars rotate around the North and South Celestial Poles. These are the points in the sky directly above the geographic north and south pole, respectively. The Earth's axis of rotation intersects the celestial sphere at the celestial poles. The number of degrees the celestial pole is above the horizon is equal to the latitude of the observer. Fortunately, for those of us in the northern hemisphere, there is a fairly bright star real close to the North Celestial Pole (Polaris or the North star). Another important reference marker is the celestial equator: an imaginary line around the sky directly above the Earth's equator. It is always 90 degrees from the poles. All the stars rotate in a path that is parallel to the celestial equator. The celestial equator intercepts the horizon at the points directly east and west anywhere on the Earth. If you joined Santa last break, you would have seen Polaris straight overhead and the celestial equator on your horizon. The point straight overhead for any observer is called the zenith and is always 90 degrees from the horizon. Question: What path in the sky would the stars have followed as they rotated around you? What angle would their nightly path make with the horizon?

For each degree you moved south, the North Celestial Pole (NCP from here on) moved 1 degree away from the zenith toward the north and the highest point of the celestial equator's curved path in the sky moved up one degree from the southern horizon. By the time you reached Seattle (at latitude 47 degrees N) the NCP had moved 43 degrees away from the zenith so it was now 90 - 43 = 47 degrees above the horizon. The celestial equator was 43 degrees above the southern horizon and it still intercepted the horizon due east and west. Question: What path in the sky would the stars have followed as they rotated around you? To warm Rudolph's frozen nose, Santa headed down to the equator. At the equator, you would have seen the celestial equator arcing from east to the zenith to the west. The NCP would have been on your northern horizon. Question: What path in the sky would the stars have followed as they rotated around you? Continuing southward (Opus' relatives had been good this year), you would have seen the NCP disappear below the horizon and the SCP rise above the southern horizon one degree for every one degree of latitude south of the equator you went. The arc of the celestial equator would have moved to the north, but the arc still intercepted the horizon at the east/west points.

Angles

Index

To describe distances across the sky, we use ``angles on the sky'' as if the celestial objects were actually attached somehow to the celestial sphere. There are 360 degrees in a full circle and 90 degrees in a right angle (two perpendicular lines intersecting each other make a right angle). Each degree is divided into 60 minutes of arc. A quarter viewed face-on from across the length of a football field is about 1 arc minute across. Each minute of arc is divided into 60 seconds of arc. The ball in the tip of a ballpoint pen viewed from across the length of a football field is about 1 arc second across. The sun and moon are both about 0.5 degrees = 30 arc minutes in diameter. The pointer stars in the bowl of the Big Dipper are about 5 degrees apart and the bowl of the Big Dipper is about 30 degrees from the NCP.

Motion of the Sun

Index

Now that we have our bearings, let's focus on solar-system objects. First the sun. Every day the sign rises in an easterly direction and sets in a westerly direction and it takes the sun on average 24 hours to go from noon position to noon position the next day. The ``noon position'' is when the sun is highest above the horizon on a given day. Our clocks are based on this solar day. However, the exact position on the horizon of the rising and setting sun varies throughout the year. Furthermore, the sun appears to drift eastward with respect to the stars (or lag behind the stars) over a year's time. It makes one full circuit of 360 degrees in 365.25 days (very close to 1 degrees or twice its diameter per day). The apparent path of the sun through the stars is called the ecliptic. This circular path is tilted 23.5 degrees with respect to the celestial equator. The ecliptic and celestial equator intersect at two points: the vernal (spring) equinox and autumnal equinox. The sun crosses the celestial equator moving northward at the vernal equinox around March 21 and crosses the celestial equator moving southward at the autumnal equinox around September 22. When the sun is on the celestial equator at the equinoxes, everybody on the Earth experiences 12 hours of daylight and 12 hours of night (hence, the name ``equinox'' for equal night).

Let's make sure we understand this. No matter where you are on the Earth, you will see 1/2 of the celestial equator's arc (except for the geographic poles). Since the sky appears to rotate around us in 24 hours, anything on the celestial equator takes 12 hours to go from due east to due west. Every celestial object's diurnal (daily) motion is parallel to the celestial equator. So for us northern observers, anything south of the celestial equator takes less than 12 hours between rise and set, because most of its rotation arc around is hidden below the horizon. Anything north of the celestial equator takes more than 12 hours between rising and setting because most of its rotation arc is above the horizon. For observers in the southern hemisphere, the situation is reversed. However, remember, that everybody anywhere on the Earth sees 1/2 of the celestial equator so at the equinox, when the sun is on the equator, we see 1/2 of its rotation arc around us, and therefore we have 12 hours of daylight and 12 hours of nightime everyplace on the Earth.

The geographic poles are a special case. The celestial equator is right along the horizon and the full circle of the celestial equator is visible. Since a celestial object's diurnal path is parallel to the celestial equator, stars do not rise or set at the geographic poles. On the equinoxes the Sun moves along the horizon. At the North Pole the Sun ``rises'' on March 21st and ``sets'' on September 22. The situation is reversed for the South Pole.

Since the ecliptic is tilted 23.5 degrees with respect to the celestial equator, the sun's maximum distance from the celestial equator is 23.5 degrees. This happens at the solstices. For observers in the northern hemisphere, the farthest northern point above the celestial equator is the summer solstice, and the farthest southern point is the winter solstice. The sun reaches winter solstice around December 21 and we see the least part of its diurnal path all year-this is the shortest ``day''. The sun reaches the summer solstice around June 21 and we see the greatest part of its diurnal path all year-this is the longest ``day''.

Solar and Sidereal Day

Index

The fact that our clocks are based on the solar day and the sun appears to drift eastward with respect to the stars (or lag behind the stars) by about 1 degrees per day means that if we look closely at the positions of the stars over a period of several days, we notice that according to our clocks, the stars rise and set 4 minutes earlier each day. Our clocks say that the day is 24 hours long, so the stars move around the Earth in 23 hours 56 minutes. This time period is called the sidereal day because it is measured with respect to the stars. One month later (30 days) a given star will rise 2 hours (30*4 minutes = 120 minutes) earlier than it did before. A year later that star will rise at the same time as it did today. Another way to look at it is that the sun has made one full circuit of 360 degrees in a year of 365.25 days (very close to 1 degree per day). This means that, from noon to noon, the Earth has to turn nearly 361 degrees, not 360 degrees, in 24 hours. This makes the length of time for one rotation with respect to the background stars a little less than 24 hours on the clock.

Solar and Sidereal Time as Viewed from Space

Index

Let's jump to a more modern view and take a position off the Earth and see the Earth revolving around the Sun in 365.25 days and rotating on its axis every 23 hours 56 minutes. The Earth's rotation plane is tilted by 23.5 degrees from its orbital plane which is projected against the background stars to form the ecliptic.

Note that the Earth's rotation axis is always pointed toward the Celestial Poles. Currently the North Celestial Pole is very close to the star Polaris.

Imagine that at noon we have a huge arrow that is pointing at the Sun and a star directly in line behind the sun. The observer on the Earth sees the Sun at its highest point above the horizon: on the arc going through the north-zenith-south points, which is called the meridian. The observer is also experiencing local noon. If the sun were not there, the observer would also see the star on the meridian.

Now as time goes on the Earth moves in its orbit and it rotates from west to east (counterclockwise if viewed from above the north pole). One sidereal period later (23 hours 56 minutes) or one true rotation period later, the arrow is again pointing toward the star. The observer on the Earth sees the star on the meridian. The arrow is not pointing at the sun! In fact the Earth needs to rotate a little more to get the arrow lined up with the sun. The observer on the Earth sees the Sun a little bit east of the meridian. Four minutes later or one degree of further rotation aligns the arrow and Sun and we have one solar day (24 hours) since the last time the Sun was on the meridian. That night the Earth observer will see certain stars visible like those in Taurus, for example. (Notice that the Earth's rotation axis is still pointed toward Polaris.) A half of a year later Taurus will not be visible but those stars in Scorpius will be visible. (Again, notice that the Earth's rotation axis is still pointed toward Polaris.)

Time Zones

Index

People east of you will see the sun on their meridian before you see it on yours. Those in Spokane will see the sun on their meridian about 20 minutes before we see the sun on ours. They experience local noon about 20 minutes before we do. That is because they are at longitude 117.4 degrees West longitude while Seattle is at 122.3 degrees West longitude (or about 5 degrees difference). For each one degree in longitude East a person is from us, the time between their local noon and ours will increase by 4 minutes. It used to be that every town's clocks were set according to their local noon and this got very confusing for the railroad system so they got the nation to adopt a more sensible clock scheme called time zones. Each person within a time zone has the same clock time. Each time zone is 15 degrees wide which corresponds to 15*4 minutes = 60 minutes = 1 hour worth of time. Those in the next time zone east of us (Mountain standard time) have clocks that are 1 hour ahead of ours.

Equation of Time

Index

This subsection can be skipped for those in a hurry. The careful observer will notice some peculiarities with the solar motion and will want to read this paragraph.

There is a further complication in that the actual sun's drift against the stars is not uniform. Part of the non-uniformity is due to the fact that on top of the general eastward drift among the stars the sun is moving along the ecliptic northward or southward with respect to the celestial equator. Thus, during some periods the Sun appears to move eastward faster than during others. Apparent solar time is based on the component of the Sun's motion parallel to the celestial equator. This effect alone would account for as much as 9 minutes difference between the actual Sun and a mean Sun moving uniformily along the celestial equator. Another effect to consider is that the Earth's orbit is elliptical so when the Earth is at its closest point to the Sun (perihelion) it moves quickest. When at farthest point from the Sun (aphelion) it moves slowest. Remember that a solar day is the time between meridian passages of the Sun. At perihelion the Earth is moving rapidly so the Sun appears to move quicker eastward than at other times of the year. The Earth has to rotate through a greater angle to get the Sun back to local noon. This effect alone accounts for up to 10 min difference between the actual Sun and the mean Sun. However, the maximum and minimum of these two effects do not coincide so the combination of the two (called the Equation of time) is a bit complicated. This explains why the earliest sunset and latest sunrise is not at the winter solstice. Yet, the shortest day is at the winter solstice. Rather than resetting our clocks everyday to this variable Sun, our clocks are based on a uniformly moving Sun that moves at a rate along the celestial equator of 360 degrees/365.2564 per day. Aren't you glad that your watch keeps track of time for you?

Seasons

Index

The seasonal temperature depends on the amount of heat we receive from the Sun. To hold the temperature constant, there must be a balance between the amount of heat we gain and the amount we radiate to space. If we receive more heat than we lose, we get warmer; if we lose more than we gain, we get cooler. The Voyager lab ``The Sun and the Seasons'' asks you to consider some basic observations of the seasons: 1) The northern hemisphere gets warmer during June-August (northern summer) while the southern hemisphere get cooler at the same time (southern winter). 2) Shadows tend to be longer and days tend to be shorter during the winter months. 3) The Suns seems to rise and set further north during the northern hemisphere's summer. If you're in the southern hemisphere, during your summer (October-January) the Sun rises and sets further south. 4) The Sun seems to appear higher in the sky at local noon during the summer. What is going on? You will find out when you do that Voyager lab. Remember that the Earth's axis is tilted with respect to its orbital plane.

Motions of the Moon

Index

The moon moves rapidly with respect to the background stars. It moves about 13 degrees (26 times its apparent diameter) in 24 hours (slightly greater than its own diameter in one hour)! Its rapid motion has given it a unique role in the history of astronomy. For thousands of years it has been used as the basis of calendars. Isaac Newton got crucial information from the Moon's motion around the Earth for his law of gravity. Almost everyone has noted that we see the same face of the Moon all of the time. It's the ``man in the moon'', ``woman in the moon'', ``rabbit in the moon'' etc. One thing this shows us is that the moon turns exactly once on its axis each time that it goes around the Earth. Later on we'll find out how tidal forces have caused this face-to-face dance of the Earth and Moon. It drifts eastward with respect to the background stars (or it lags behind the stars). It returns to the same position with respect to the background stars every 27.323 days. This is its sidereal period.

Phases and Eclipses

Index

One of the most familiar things about the Moon is that it goes through phases from new (all shadow) to first quarter (1/2 appears to be in shadow) to full (all lit up) to third quarter (opposite to the first quarter) and back to new. This cycle takes about 29.53 days. This time period is known as the Moon's synodic period. Because the moon moves through its phases in about four weeks, new moon, first quarter, full moon, third quarter, and new moon occur at nearly one-week intervals. We know that the phases are due to how the Sun illuminates the Moon and the relative positioning of the Earth, Moon, and Sun. We observe that not much of the Moon is illuminated when it is close to the Sun. In fact, the smaller the angular distance between the Moon and the Sun, the less we see illuminated. When the angle is within about 6 degrees we see it in a new phase. Sometimes that angle = 0 degrees and we have a solar eclipse-the moon is in new phase and it is covering up the sun. Conversely, the greater the angular distance is between the Moon and the Sun, the more we see illuminated. Around 180 degrees we see the Moon in full phase. Sometimes (about twice a year) the Moon-Sun angle is exactly 180 degrees and we see the Earth's shadow covering the Moon-a lunar eclipse.

Why are the synodic and sidereal periods not equal to each other? For a reason similar to the reason why the solar day and sidereal day are not the same. Remember that a solar day was slightly longer than a sidereal day because of the sun's apparent motion around the Earth (caused by the Earth's motion around the Sun). The Moon's synodic period is longer than its sidereal period because of its motion around the Earth. At new moon, the Sun and Moon are seen from the Earth against the same background stars. One sidereal period later, the Moon has returned to the same place in its orbit and to the same place among the stars, but the in the meantime, the Sun has been moving eastward, so the Moon has not yet caught up to the Sun. The Moon must travel a little over two more days to reach the Sun and establish the new moon geometry again.

The modern model has the moon going around the Earth with the Sun far away. At different positions in its orbit we see different phases all depending on the relative positions of the Earth-Moon-Sun. Another possible model was presented by the highly-esteemed Harvard graduates. They proposed that the dark part of the moon is the result of portions of the moon lying in the shadow of the Earth. Question: If the Harvard model was true, what would be the difference in Moon rise time and the sun rise time for a New Moon or first quarter phase? What would be the angular separation between the Moon and the Sun for a New Moon or first quarter phase in the Harvard model?

Relationship of Tides and Lunar Phases

Index

When you look in the paper at the section containing the tide tables, you'll often see the phase of the moon indicated as well. That's because the ocean tides are caused by the gravity of the Moon. We'll go into the nitty-gritty details of gravity a little later, but now you just need to know that gravity depends on mass and distance--greater distance means less gravity. The side of the Earth facing the moon is about 4000 miles closer to the Moon than the center of the Earth is, and the Moon's gravity pulls on the near side of the Earth more strongly than on the Earth's center. This produces a tidal bulge on the side of the Earth facing the Moon. The Earth rock is not perfectly rigid; the side facing the Moon responds by rising toward the Moon by a few centimeters on the near side. The more fluid seawater responds by flowing into a bulge on the side of the Earth facing the moon. That bulge is the high tide. At the same time the Moon exerts an attractive force on the Earth's center that is stronger than that exerted on the side away from the Moon. The Moon pulls the Earth away from the oceans on the far side, which flow into a bulge on the far side, producing a second high tide on the far side.

These tidal bulges are always along the Earth-Moon line and the Earth rotates beneath the tidal bulge. When the part of the Earth where you are located sweeps under the bulges, you will notice a high tide; when it passes under one of the depressions, you experience a low tide. An ideal coast should experience the rise and fall of the tides twice a day. In reality, the tidal cycle also depends on the latitude of the site, the shape of the shore, winds, etc.

The Sun's gravity also produces tides that are about half as strong as the Moon's and produces its own pair of tidal bulges. They combine with the lunar tides. At new and full moon, the Sun and Moon produce tidal bulges that add together to produce extreme tides. These are called spring tides (the waters really spring up!). When the Moon and Sun are at right angles to each other (1st & 3rd quarter), the solar tides reduce the lunar tides and we have neap tides.

Tides Slow Earth Rotation

Index

As the Earth rotates beneath the tidal bulges, it attempts to drag the bulges along with it. A large amount of friction is produced which slows down the Earth's spin. The day has been getting longer and longer by about 0.0016 seconds each century. Over the course of time this effect can have a noticeable effect. Astronomers trying to compare ancient solar eclipse records with their predictions found that they were off by a significant amount. But when they took the slowing down of the Earth's rotation into account, their predictions agreed with the solar eclipse records. Also growth rings in ancient corals about 400 hundred million years old show that the day was only 22 hours long so that there were over 400 days in a year. Eventually the Earth's rotation will slow down to where it keeps only one face toward the Moon. Gravity acts both ways so the Earth has been creating tidal bulges on the Moon and has slowed it's rotation down so much that it rotates once every orbital period. The Moon keeps one face always toward the Earth.

Several people have asked me for references about the evidence for the slowing down of the Earth's rotation so here's a list:

  1. Growth Rhythms and the History of the Earth's rotation, edited by G.D. Rosenberg and S.K. Runcorn (Wiley: New York, 1975). An excellent source on the eclipse records and the biology of coral and their use as chronometers.
  2. Tidal Friction and the Earth's Rotation, edited by P. Brosche and J. Sündermann (Springer Verlag, 1978). The second volume put out in 1982 does not talk about eclipse records or the use of coral but, instead, goes into the astrophysics of the Earth-Moon dynamics and geophysics of internal Earth processes effects on the Earth's rotation.
  3. Earth's Rotation from Eons to Days, edited by P. Brosche and J. Sündermann (Springer Verlag, 1990). Has several articles about the use of ancient Chinese observations.
  4. Richard Monastersky 1994, Ancient tidal fossils unlock lunar secrets in Science News vol. 146, no. 11, p. 165 of the 10 Sept 1994 issue.

Tides Enlarge Moon Orbit

Index

Friction with the ocean beds drags the tidal bulges eastward out of a direct Earth-Moon line and since these bulges contain a lot of mass, their gravity pulls the moon forward in its orbit. The Moon's orbit is growing larger, receding from the Earth at about 3 cm per year. We have been able to measure this slow spiralling out with lasers bouncing off reflectors left by the Apollo astronauts on the lunar surface. The consequence of the Moon's recession from the Earth because of the slowing down of the Earth's rotation is also an example of the conservation of angular momentum. Angular momentum is the amount of spin motion an object or group of objects has. It depends on the geometric size of the object or group of objects, how fast the object (or group of objects) is moving, and the mass of the object (or the group). We will talk more about the concept of angular momentum a little later in the course. The slow spiralling out of the Moon means that there will come a time in the future when the angular size of the Moon will be smaller than the Sun's and we won't have any more solar eclipses!

Eclipse Details: Lunar Eclipse

Index

Let's talk a little more about lunar and solar eclipses. Remember that an eclipse happens when an object passes through another object's shadow. Any shadow consists of two parts: an umbra which is the region of total shadow and the penumbra which is the outer region of partial shadow. If the Moon were to pass through the Earth's umbra, a Moon observer would not be able to see the Sun at all-she would observe a solar eclipse! An Earth observer would see a total lunar eclipse. The Earth's shadow is pretty big compared to the Moon so a total lunar eclipse lasts about 1 hour 45 minutes. If the Moon only passed through the outer part of the shadow (the penumbra) then the Moon observer would see the Sun only partially covered up-a partial solar eclipse. The Earth observer would see the Moon only partially dimmed-a partial lunar eclipse. During a total lunar eclipse we see another interesting effect-the Moon turns a coppery (or bloody) red. This is due to sunlight refracting or bending through the Earth's atmosphere. Dust particles in the Earth's atmosphere have removed much of the bluer colors in the sunlight so only the redder colors make it to the Moon. The amount of dust determines the deepness of the red colors. This is also why the Sun appear redder at sunset on Earth. The Moon observer would see a reddish ring around the Earth.

Eclipse Details: Solar Eclipse

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The Moon's shadow also has an umbra and penumbra. The shadow is much smaller than the Earth's. Only if the Moon is in the ecliptic plane when it is exactly New Moon will we have the Moon's shadow hitting the Earth. Where the umbra hits the Earth, we'll see a total solar eclipse. Where the penumbra hits the Earth, we'll see a partial solar eclipse. In a total solar eclipse the bright disk of the sun is completely covered up by the Moon and we see the other parts of the sun like the corona, chromosphere, and prominences. Unfortunately, only the tip of the Moon's umbra reaches the Earth (the tip hitting the Earth is 270 km [168 miles] in diameter) and it zips along the Earth's surface at over 1600 kph (1000 mph) as the Moon moves around the rotating Earth so a total solar eclipse can last a maximum of only 7.5 min. Usually total solar eclipses only last 3-4 minutes. Because of the orbital motion of the Moon and the rotation of the Earth, the umbra makes a long, narrow path of totality. Question: Why is the path of totality different each time? Why does the latitude of the path vary? Why can the totality path be more than 23.5 degrees in latitude from the equator?

Sometimes the umbra does not reach the Earth at all (only the penumbra) even though the Moon is on the ecliptic and it is exactly in New Moon phase. We see a bright ring around the Moon when it is lined up with the Sun-an annular eclipse (because of the annulus of light around the Moon). Question: Why would the umbra not touch the Earth? What does the fact that we sometimes observe annular eclipses and sometimes total solar eclipses indicate about the shape of the Moon's orbit?

Planetary Motions

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There are other celestial objects that drift eastward with respect to the stars. They are the planets (Greek for ``wanderers''). There is much to be learned from observing the planetary motions with the naked eye (no telescope). There are 5 planets visible without a telescope, Mercury, Venus, Mars, Jupiter, and Saturn (6 if you include Uranus for those with sharp eyes!). All of them move within 7 degrees of the ecliptic. Question: What does that imply about their orbital planes? What would an edge-on view of our solar system look like? Two of the planets (Mercury and Venus) are never far from the Sun. Venus can get about 48 degrees from the Sun, while Mercury can only manage a 27.5 degrees separation from the Sun. When Venus and/or Mercury are east of the Sun, we'll see them as an ``evening star'' even though they are not stars at all. When either of them is west of the Sun they are called a ``morning star''. Planets produce no visible light of their own; we see them by reflected sunlight. True stars produce their own visible light. Venus can be the brightest of all the planets, sometimes getting so bright that it can create a shadow! Mercury and Venus are never visible at around midnight (or opposite the Sun), the other planets can be visible then. Sometimes a strange thing happens--a planet will slow down its eastward drift among the stars, halt, and then back up and head westward for a few weeks or months (retrograde motion), then halt and move eastward again. The planet executes a loop against the stars! What causes that? The answer to that question involved a long process of cultural evolution, political strife, and paradigm shifts. We'll investigate the question when we look at geocentric (Earth-centered) models of the universe and heliocentric (Sun-centered) models of the universe.

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last update: 05 Dec 95


Nick Strobel -- Email: strobel@astro.washington.edu

(206) 543-1979
University of Washington
Astronomy
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