A Matter of Time: Part 2.
Mike Dziekan
VP Engineering, Connecticut Analytical Corporation
Part 1 appeared in the 30 June 2006 issue of The
Citizen Scientist and is available here.
The Sundial
Most of us are familiar with that antique-looking,
flat, horizontal metal plate that sits (mostly ignored) in
many gardens. It was likely purchased as a decorative ornament
where the purchaser intended to set it up as a sundial to
indicate the time, only to be frustrated that the indicated
time is way off. If you are even the slightest bit serious
about purchasing a sundial, DO NOT buy one of those garden
center sundials unless it has an adjustable gnomon that can
be set for your exact latitude.
Not long ago the sundial was a very widely
used indicator of time. If you can afford to get a sundial
that can be adjusted for your latitude and longitude, then
the sundial time will equal the clock time, with the exception
of the approximately +/- 15 minute annual variation and daylight
savings time (DST). There are many benefits and drawbacks
of sundials. One very obvious drawback is contained in the
name itself – sundial. The sun is an integral component of
any sundial, and at night or during cloudy weather, a sundial
no longer functions.
Recall from our previous
discussion on time zones how the time difference is four
minutes for every degree of longitude. Many people configure
their sundial for DST with the logic being that one is more
apt to be outdoors more often in the summer than in the winter!
Each sundial must have a gnomon angle that
is equal to the exact latitude of your location to be accurate.
If the seller happily agrees to sell you a garden variety
sundial and states that it will be accurate without asking
you where you live (your exact coordinates), then the seller
intentionally deceptive or woefully ignorant of how sundials
work! If the seller continues to argue that sundials aren't
that accurate, and that the indicated time will be close enough,
ask if 75% or 80% of the purchase price will be “close enough!”
A properly adjusted and orientated sundial can be pretty accurate.
But because of the popularity of garden center sundials, they
have an undeserved reputation for inaccuracy.
Readers of The Citizen Scientist
wise enough to own a copy of the Amateur
Scientist CD Rom will be rewarded with a good deal of
information relating to sundials, their construction and proper
use. In fact, there is a good article by C. L. Stong, from
March 1964, that explains how to construct an easy to make
sundial that reads “clock time” directly.
Local time is what the sundial will
indicate, and this is commonly referred to as “apparent time.”
To correct your sundial to read “clock time,” a longitude
correction is necessary. This is taken into consideration
when you order a custom sundial, for you will need to provide
your exact coordinates. The custom dial will include a gnomon
set to the correct angle for your latitude, and the numbering
will be adjusted to match your exact longitude. I have only
been discussing one specific type of sundial, but there are
many different types with different advantages to each. There
is even a national organization called the North
American Sundial Society (NASS).
I am a member of the North American Sundial
Society. For a small membership fee you are privy to a wealth
of very detailed information on “dialing.” The NASS has information
ranging from the most basic concepts to very advanced theoretical
analysis of the sun's motion and spherical trigonometry. I
strongly urge members of the Society
for Amateur Scientists to visit their website
and download a sample copy of their quarterly Compendium
. As far as I am concerned, the best source for “dialing”
information is the NASS.
The Equation of Time
(EOT)
Earlier I mentioned that a sundial can be
off by about +/- 15 minutes. More precisely, it can be ahead
by approximately 17 minutes and behind by 14 minutes during
a calendar year. The equation of time (EOT) is used to
calculate the amount of deviation in apparent time (sundial
time) throughout the year. This provides mean solar time that
assures that local noon does not vary throughout the year.
The Earth orbits the sun in a slight ellipse
rather than a perfect circle. Kepler's
laws of planetary motion, specifically his second law,
provides that a body in an elliptical orbit around a star
will sweep out equal areas in equal intervals of time.
As the Earth orbits near the Sun, the velocity
of the orbit is greater. When the Earth is orbiting further
away from the Sun, the orbital velocity is less. There are
two key points here in the orbital path, perihelion and aphelion.
Perihelion is the shortest distance in the orbital path between
the star and the orbiting body, while the aphelion is the
furthest distance. The orbital velocity at aphelion is slower
than at perihelion. I should point out that the Earth's orbit
around the sun is only slightly elliptical, and the image
drawn in Fig. 1 is greatly exaggerated for illustrative purposes.
The Earth orbit eccentricity in reality is only about 0.02,
very nearly a circle.

Figure 1. An example of Kepler’s second
law, equal areas in equal time.
Changes in the velocity of the Earth in its
orbit, slight inclination of the Earth's orbital path and
the precession about the Earth's axis will cause some minor
but measurable differences in the observed local noon. This
is the reason for the approximate +/- 15 minute difference
in the time indicated by a properly adjusted sundial.

Figure 2. A plot of the EOT (Equation Of
Time) due to the combination of the Earth's tilt and orbital
velocity change at aphelion and perihelion.
I used Excel to create the plot in Fig. 2
of the equation of time to illustrate graphically why sundials
indicate a difference in local noon throughout the year. As
you look at Fig. 2, you will notice three distinct plots. The yellow
dashed line is the error introduced by the tilt of the Earth
on its axis. The red dashed line is the error introduced by
the difference in orbital speed of the elliptical orbit of
the Earth around the Sun – faster in the winter and slower
in the summer. The combination of these two plots generates
a third plot, the equation of time. The black plot is an indication
of how much sundial time (apparent time) will differ from
that of a clock.
The EOT corrected time is known as mean
solar time and is usually applied to the sundial as an
inscription or an attached plate that lists corrections in
minutes throughout the year. Sometimes there is just a listing
of numbers, and sometimes the graphical plot is also included.
An example of such an EOT plaque for sundials is shown by
the EOT chart image in Fig. 3..

Figure 3. A common example of an EOT plaque
found on many sundials.
Since the sundial apparent time will be slower
by 14 minutes in February, then the EOT chart indicates that
we must add 14 minutes to correct for the error. If we had
a custom made sundial that was specific to our latitude and
longitude, then when our sundial indicates noon on 4 February,
our clock would indicate fourteen minutes past noon. Therefore,
by adding fourteen minutes to our sundial's apparent time
we find the corrected time is 12:14 P.M. If we look at a sundial
that was not corrected for its longitude, then if we correct
the sundial time for the difference by using the EOT, we would
be dismayed to find that it would probably not agree with
our watch! Unless we correct for the longitude, our sundial
can never give a direct reading of clock time.
I should point out that the EOT does not
remain exactly the same from year to year. Each year the amounts
of deviation will be slightly offset from that of the previous
year.
Precession of the
Equinoxes
The Earth not only rotates around its spin
axis, but it also precesses
. If you examine Fig. 4, you will notice that in addition
to the rotational spin of the Earth, there is also an additional
rotation. Just as a spinning top wobbles in a slow circular
fashion as it spins, the Earth also wobbles. This is called
gyroscopic precession. The dashed red line indicates
the gyroscopic precession or wobble of the Earth. Although
I have drawn a nice smooth circle, in reality this “circle”
is more of a wobble motion, then a smooth circular motion.

Figure 4. Diagram of the Earth's axis in
relation to the Earth's precessional motion.
The period of procession is approximately
25,800 years. This means that Polaris, the Northern Pole star,
will no longer be aligned to the Earth's North Pole in several
thousand years (see Fig. 5). In fact, several stars will take
the place of Polaris as the Northern Pole star over the precession
cycle. After one cycle of precession (25,800 years), we will
return to alignment with Polaris as the Northern Pole star.
If you have played with a spinning top, you may recall that
the top wobbles in a slow circular fashion as it spins. This
is called gyroscopic precession. As in the case of
the top, the Earth also precesses. There is also a slight
wobble, technically called nutation, caused by the
Earth's varying gravitational attraction of the moon and sun
on the Earth's equatorial bulge. The nutation period is only
18.6 years as opposed to the nearly 26,000 years for precession.

Figure 5. Diagram of the Earth's axis in
relation to the ecliptic.
Figure 5 shows that the equinoxes do not
occur on set dates, but at points of intersection between
the ecliptic and the celestial equator. Precession of the
equinoxes is the westward motion of the points of intersection
along the ecliptic. The reason for this precession of the
equinoxes is due to the Earth's own precession. Referring
back to Fig. 4, as the Earth slowly precesses the points of
intersection for the Equinoxes will slowly advance. The ecliptic
lies in a plane of Earth's orbit around the Sun. The Celestial
Equator lies in a plane of the Earth's equator. The intersection
of these two planes determines the equinoxes. By looking at
Fig. 5, one can more easily see how the precession of the
Earth would cause these points of intersection to slowly move
throughout the 25,800 year precession cycle.
The Analemma
Now we come to the analemma, the figure eight
pattern printed on most globes like the one shown in Fig.
6. Technically, the analemma is a plot of the EOT on one axis
and the Suns declination on the other. If you search the web
for sundials, you will see various depictions and animations
of the analemma.

Figure 6. Author Mike Dziekan holding a globe
showing the analemma.
Figure 7 is a plot of the position of the
Sun for one year with one point for each hour. This plot shows
how the analemma varies over time in a pattern that would
otherwise be hidden in the data. I color-coded the analemma
in blue for the first half of the year and red for the second
half. The plot also indicates the sun's position for the summer
solstice, vernal and autumnal equinoxes and the winter solstice.
You can also see from this plot of the sun's position that
the sun actually moves east and west throughout the year.
After the summer solstice, the sun rises more west each morning
until the winter solstice, when it sets more eastward each
evening. The two equinoxes' overlap each other in the plot
and are difficult to distinguish.

Figure 7. This is a plot of the daily motion
of the sun throughout the year. The analemmas are produced
by plotting only the hourly position of the sun, while the
solstices and equinoxes are plotted as continuous lines. The
slight flattening of the top is produced because the arc is
plotted as a flat structure instead of a curved one.
An actual photograph of the analemma made
by photographer Anthony Ayiomamitis is shown in Fig. 8. Anthony
photographed the sun about once a week throughout the year
at the same time of day. Anthony's remarkable photograph shows
that the analemma is literally written in the sky!

Figure 8. This remarkable photograph of the
analemma was made by photographer Anthony Ayiomamitis. The
image was made from his home in Athens by taking 47 separate
images at the same time of day during one year (30 March 2003
to 24 March 2004 at 12:00:00 UT + 2). The ruins in the foreground
are the Temple of Zeus. For more details about this image,
see "Analemma
photographed over the Temple of Zeus in Athens, Greece"
by Anthony Ayiomamitis in The Citizen Scientist (30
June 2006). Also see Anthony's website.
Copyright by Anthony Ayiomamitis. All rights reserved.
Used with permission.
Now that you know that the sun will vary
its apparent position in the sky throughout the year, we can
address some typical Hollywood mistakes. If you have ever
watched the movie “National Treasure”, then you may have noticed
the scene where they had to wait for a specific time when
the shadow of the top of the old Liberty bell tower in Philadelphia
would cast a shadow on a specific brick in the wall. I am
not saying that this would not work, but it would only work
if you knew what specific day it was intended. Basically,
the shadow of the old bell tower steeple would sketch out
a shadow pattern of an analemma throughout the year, and,
depending upon the distance between the two, it could be off
by a meter (several feet)! It is also a good thing that it
just happened to be sunny that day, but then again, it's Hollywood!
North American
Sundial Society and the TV show NUMB3RS
No, it's not a typo. There is a television
show called NUMB3RS,
and it is about a brilliant mathematician who uses math to
help solve cases for the FBI. A while back, the producers
of the show contacted Fred Sawyer, president of the North
American Sundial Society . They wanted to have an episode
where several photographs were found in a digital camera at
a crime scene. As Fred Sawyer explained, "They wanted
a poor man's GPS.” The pictures indicated the exact time they
were taken, and they depicted objects that had standard heights,
including a basketball hoop that cast a shadow on a flat surface
covered with bricks.
The bricks were all of uniform size, and
the basketball hoop was of standard height. Because the surface
was flat, the length of the shadow could be accurately measured
from the photographs. Because each photograph was time stamped
and several photos were taken at different times, the location
of the photographs could be reasonably pinpointed. This is
because the Sun can cast a shadow of a specific length and
angle only at an exact time for any specific location.
If you are a member of NASS, then you have access to the society's
Compendium (volume 12, December 2005) in which Fred
describes the entire correspondence related to this problem.
It's a fascinating story.
If you are wondering why I related this story,
it is all related to sundials. If you can determine the exact
time from a sundial, then the opposite is true. If you know
the exact height of an object, and the exact length and angle
of its shadow, in addition to knowing the exact time and the
Sun's position, then you can determine a unique location on
Earth. I should mention that the only payment that Fred wanted
for his assistance with the TV program was that two of the
main characters would state that they are card carrying members
of the North American Sundial Society. The small sundial that
Charlie occasionally picked up and held during the program
was donated to the show by Fred Sawyer.
In Part 3 Mike Dziekan will conclude
his journey through the world of time with more about time
and calendars. Editor. 
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