Chapter 3 How Earth and Sky Work-Effects of Latitude: Sphere Is An Imaginary Sphere With The
Chapter 3 How Earth and Sky Work-Effects of Latitude: Sphere Is An Imaginary Sphere With The
Chapter 3 How Earth and Sky Work-Effects of Latitude: Sphere Is An Imaginary Sphere With The
In chapters 3 and 4 we will learn why our view of the heavens depends on our position on the
Earth, the time of day, and the day of the year. We will explore views of the Earth, the sky, and an
observer as seen from space and as seen from the surface of the Earth.
Today we know that the Earth is a sphere and we are tiny by comparison. The distance to every
other celestial body is MUCH larger than the diameter of the Earth. Because we are so much
smaller than the Earth, the Earth appears to take up half of all the directions we can look when we
are on the Earths surface. (What would we see from space far from the Earth?)
We know that Earth and the other planets orbit the Sun, while stars are at various large distances
and orbit the Milky Way galaxy. But we can use the idea of the Celestial Sphere to describe the
appearance of the sky. The Celestial
Sphere is an imaginary sphere with the
Earth at its center. Stars, the Moon, the
planets, the Sun, galaxies etc appear to be
pasted on the Celestial Sphere. Straight up
from Earths north pole is the North Celestial
Pole, straight down is the South Celestial
Pole. The Earths poles and Celestial Poles
are lined up and remain lined up. Similarly
the Earths equator lines up with the
Celestial Equator.
The figure shows our relationship to the
Celestial Sphere. The observer stands on
the Earth. The patterned surface is the
apparent (flat) surface of the Earth,
bounding the half of the sky visible to the
observer.
Meridian
Circle through Zenith,
North Celestial Pole,
South Celestial Pole
Zenith
Direction Straight Up
from Observer
Observer
CAN see
North
Pole
Observer
Horizon
Boundary between
Visible and Invisible
We have been considering what the observer can see. The Earth spins and the observer moves
with it, changing what is visible. The stars move but they do not go around the Sun or the Earth.
Because stars are so far away, none of their individual motions of the stars is noticeable.
Astronomers measure stars motions by photographing them and comparing their relative positions
over many years.
Chapter 3
Because the stars positions change so slowly, we can define their positions and patterns on the
Celestial Sphere. We do this using coordinates that are similar to Latitude and Longitude on Earth
(Other planets, moons and the Sun are also assigned their own Latitude and Longitude systems.)
Lets review Latitude and Longitude.
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Latitude is zero at the equator and 90 at the
poles. Longitude is zero at the Prime Meridian
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in Greenwich England. It goes East for 180
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and west for 180 . The International Date
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Lines is approximately at the 180 line.
The coordinates for the Celestial Sphere are
called Right Ascension and Declination.
They are similar to latitude and longitude on
the Earth. Each location on the Celestial
Sphere, that is each direction in the sky, can
be identified by its Right Ascension and
Declination.
Earth
North Pole
On Earth
Meridians of Longitude
Run N-S
They tell the E-W position
Starts at Greenwich, England
North Pole
South Pole
Earth
Parallels of Latitude
Run E-W
They tell the N-S position
Starts at the Equator
South Pole
On Celestial Sphere
Meridians of Right Ascension
Run N-S
They tell the E-W position
Start at Vernal Equinox
Run Parallel to Longitude Lines
North Pole
South Pole
North Celestial Pole
North Pole
Parallels of Declination
Run E-W
They tell the N-S position
Start at the Celestial Equator
Line up with Earth Latitudes
South Pole
We think of the Celestial Sphere as fixed and the Earth spinning. As the Earth moves orbits and
spins, the Earths poles remain aligned with the poles of the Celestial Sphere and the parallels of
latitude remain aligned with the parallels of declination. Meridians of longitude and of Right
Ascension are parallel, but there is no one-to-one alignment.
You may be wondering how the imaginary Celestial Sphere fits with the overall concept of the
Universe, where the Earth orbits the Sun. The overall concept is in the figure below.
Chapter 3
The Celestial Sphere is so large that the Earth's orbital motion is insignificant by
comparison.
The Earth moves in three dimensions, but to make it easier to draw, we will consider the
appearance two dimensions at a time. First we will consider the view from the right of the image.
When viewed from this direction, we see the effect of latitude on what can EVER be viewed.
Then we will look from above the North Pole of the Solar System. This will tell what can be seen at
a given time and date, but will ignore
the effect of latitude. The visibility
curves at the end of chapter 4,
combine both effects.
In each
situation, we will learn to compute what
can be seen.
Chapter 3
Lets zoom out away from the Earth and the Celestial Sphere and see what happens as the Earth
spins (every 23 hr 56 minutes) and the Celestial Sphere stays still. The observer and her/his
horizon and meridian are carried along. Some stars rise and set, others are always seen.
Even though the Earth is really spinning, the appearance is that the sky is moving. If the figure
were redrawn to show the Celestial sphere moving, it would appear as follows.
In 12 hours, the sphere moves half way around. Ignoring depth in the diagram, stars, the Sun, the
Moon and the planets appear to move horizontally from one side of the figure to the other,
keeping the same declination. Over the next 12 hours they move back to their original positions.
Bodies at some positions remain visible the entire time (circumpolar for this latitude); others
remain invisible (never seen); yet others change from visible to invisible. Bodies at these positions
are said to rise and set.
These pictures show the apparent motion of the sky, but do not provide a way to compute whether
a star will be visible all the time, some of the time, or none of the time. To find this, we need to
relate the declination, horizon position on the sky and the observers latitude.
The observers latitude tells the angle from the equator to the observer. If we draw the Earth flat on
and label the declinations above it, the following picture results. North is toward the top. South is
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toward the bottom. The Declination values start at +90 at the northernmost point and progress
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lower and lower until they reach -90 .
Chapter 3
The Latitudes on the Earth and the Declinations on the Celestial Sphere line up, so
Latitude =Declination at Zenith
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The observer always stands perpendicular (at a 90 angle) to his/her horizon. The part of the
Celestial Sphere on the side of the horizon with the observers head is the visible part. The rest is
blocked by the horizon and invisible. In this picture, North is up, toward the top of the page and
South is down.
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The declinations where the horizon cuts the Celestial Sphere, are 90 away from the observers
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zenith. To find these declinations, count off the 90 from the observers zenith. This isnt the same
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as adding or subtracting 90 , since the Declination system goes only from +90 to 90 . The
declination values where the horizon cuts the Celestial Sphere are equal and opposite values.
Declination at ends of Horizon = ( 90-|latitude|)
Either you know the observers latitude and can find the horizon, or you know something about the
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horizon so you can draw the horizon and can draw the observer 90 away.
There are standard questions that you can answer when the observers latitude is known. These
questions follow. The blank would have a number in it.
What is the furthest north that an observer at latitude _______ can see?
What is the furthest south that an observer at latitude _______can see?
What is the range of declinations that an observer at latitude ________can see?
What is the range of declinations that an observer at latitude ________ can NEVER see?
What is the range of circumpolar declinations for an observer at latitude ____?
What are these questions asking and how can they be answered?
Circumpolar, the part of the sky that is always above the horizon from your location The
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circumpolar region starts at either +90 or -90 , whichever is above the horizon for the observer.
The circumpolar region extends to the closest end of the horizon. The circumpolar region NEVER
Chapter 3
crosses the equator. The observers latitude and the boundaries of the circumpolar region all have
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the same sign. Example. For an observer at +60 , the circumpolar region is +30 to +90 . If
declination is within the circumpolar region for an observer, EVERY location with that declination
number is circumpolar.
Never seen, the part of the Celestial Sphere that never comes above the horizon. It starts at
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either -90 or +90 , whichever is not visible to the observer. It extends to the closest end of the
horizon, the one with sign opposite the observers latitude. It is just the opposite of the circumpolar
region (that is the declination values are -1 times the values for the circumpolar region). For the
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observer at 60 , the never seen region would be -30 to -90 .
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Furthest South Seen - If the observer is in the northern hemisphere, -90 +latitude
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If the observer is in the southern hemisphere -90 .
Range of Declinations Which Can be Seen or Range of Declinations Visible - This is the
summation of declinations that are Always Seen plus the declinations that are Sometimes Seen. It
goes from the furthest north that is always or sometimes visible to the furthest south that is always
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or sometimes visible. It Always includes at least one 90 or -90 .
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If the observer is in the northern hemisphere, +90 to (90 -latitude)
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If the observer is in the southern hemisphere -90 to (90 -|latitude|)
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The observer in the previous figure is at latitude 60 , so her zenith is at declination 60 . Her
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horizon is at 90 from the zenith at declinations 30 . So what is the
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Furthest north that an observer at latitude ____60 _ can see? +90
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Furthest south that an observer at latitude ___60 _ _can see? -30
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Range of declinations that an observer at latitude ___60 _can see? From +90 to -30
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Range of declinations that an observer at latitude ___60 _can NEVER see? From -30 to -90
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Range of circumpolar declinations for an observer at latitude___60 _? From +90 to +30
To determine whether a body can be seen some, none, or all the time, compare the declination
to the limits of the circumpolar, never seen, and rise and set regions. Or use the diagram as
follows. You will be drawing something like the letter Z.
Chapter 3
A. Draw the horizon. It goes though the center of the picture and through (90 - |latitude| ) The
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horizon is always at 90 , a right angle, to the observers body. It does NOT matter whether
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observer and the horizon are on the right or left of the picture so long as they are at 90 to one
another.
B. Draw horizontal lines from the points where the horizon touches the Celestial Sphere to the
Celestial Sphere on the other side of the picture. The declination is the SAME number at each end
of the line. Your lines and the horizon make the shape Z or a reversed Z (NOT a sideward Z).
These lines are the boundaries of the circumpolar and never seen regions.
C. Draw a horizontal line representing the daily apparent motion of the body the declination
D. Check whether the path of the star crosses the Z you drew before. If so, it rises and sets. If the
path does not cross the Z and is always above the horizon as seen by the observer, it is
circumpolar. If the path does not cross the Z and is never above the horizon as seen by the
observer, it is Never Seen.
E. Use your horizon and the boundary lines to answer the standard questions.
Lost at Sea- Finding Where You Are From What You Can See
In the problems we have been considering, there is only one free parameter, the observer's
latitude. If we know the latitude, then we know the horizon and what can be seen, the circumpolar
region etc. There is little variety.
On the other hand, an observer can find his latitude by noting the range of circumpolar bodies,
the furthest south or north that can be seen etc. It is just a matter of using the information to find
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the horizon, then finding the location of the observer (90 from the horizon)
Example: You notice Vega at your Zenith, what is your latitude? Vega is a star and you can
find its declination from a star map.
Answer: You know that Latitude of observer = Declination of zenith and the problem says that
Vega, is at the zenith. So
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Vegas declination = declination at the observers zenith=observers latitude =39
Chapter 3
The Sky as We See It We have been making diagrams as though we are outside the
Celestial Sphere. But how does the path of a star really look from the ground?
The figure below shows how celestial objects appear to move through the sky. It is drawn for a mid
northern latitude location. Circumpolar objects appear to circle the pole, always remaining above
the horizon. Objects that rise and set make arcs starting in the East and ending in the West. The
never seen objects are, of course, never seen. The filled ellipse represents the ground.
As time goes by, the position of each object normally changes compared to the horizon and to the
cardinal points (the N, E, S, W positions on the horizon).
Chapter 3
The only points that dont appear to move are the North Celestial and the South Celestial poles.
The North star, Polaris, is about 5/6 of a degree from the North Celestial Pole. So it moves a little.
There is no bright star near the South Celestial Pole.
Altitude/Azimuth System Right Ascension and Declination are useful because they tell the
position of a location on a star map. They dont correspond to a fixed direction compared to the
observers horizon and meridian. The Altitude and Azimuth system does.
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Altitude is the angle from body to horizon. Altitude is 90 at the zenith, 0 at the horizon. Negative
altitudes are sometimes used to describe positions below the horizon (invisible).
Azimuth is the angle from
north to the point on the
horizon below the object.
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Chapter 3
The altitude of the celestial pole, whichever one you can see, is equal to the latitude of the
observer. Since the star Polaris is nearly at the North Celestial Pole, the altitude of Polaris equals
the observers latitude. This makes it easy to find latitude.
Orientation Practice Problems Set I (you may look up declinations etc. on the star map)
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