Lab 4 – 2024 – Basic Coordinates and Seasons
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Apr 3, 2024
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Astronomy 020 —Lab 4 Basic
Coordinates & Seasons
There are three main sections to this lab: 1.
terrestrial coordinates, 2.
celestial equatorial coordinates
3.
understanding how the ecliptic is related to seasons on the Earth Each of these sections has its own simulator(s). The background material necessary to utilize these tools is
contained in each section. All of this content is organized on the following webpage:
https://astro.unl.edu/naap/motion1/motion1.html
Terrestrial Coordinates
Work through the explanatory material on units of longitude and latitude
, finding longitude and latitude
,
and a bit of history (optional).
•
Open the flat map explorer
.
•
Familiarize yourself with the cursor and how it prints out the longitude and latitude of the active
map location.
•
Note that you can vary the central meridian of the map (i.e. change its longitude) by using the shift-
click feature of the cursor for control.
•
Note what information is accessible through the show cities and show map features check boxes.
•
Center the cursor on your present location. Click the open Google Maps button to launch the
Google Map tool focused on this location. Question 1: Use the flat map explorer to complete the following table. You are encouraged to try and
predict the answers and then use the map’s cursor and other features to check the accuracy of your
estimates.
Location
Longitude
Latitude
The center of the island of Sri Lanka.
18.4° W
33.9º S
International Date Line
16.8° S
150.5° W
Tropic of Capricorn
Reykjavík, Iceland
91° 04’ E
29° 37’ N
23° 43’ E
37° 55’ N
Pigeon Forge, Tennessee
25.7° E
Arctic Circle
66.1° W
18.4° N
106° 45’ E
6° 09’ S
Question 2: Using show cities
, which city shown in the flat map explorer is the closest to the Tropic of
Cancer?
Question 3: The exact coordinates of the Great Pyramid of Giza (tomb of pharaoh Khufu) are 31.134° E
and 29.979° N. What are these exact coordinates in sexagesimal notation? Show your calculations below. •
Open the globe explorer. You are encouraged to use the Terrestrial Coordinate Explorers link
which opens both simulators at the same time for the following two questions. Familiarize yourself
with the features noting that they are very similar to those in the flat map explorer.
Question 4: A) Where is the north pole on the flat map explorer
? What is its shape?
B) Where is the north pole on the globe explorer
? What is its shape?
C) Why does the north pole not have the same shape in the two different map explorers?
RA
DEC
D) This difference in shape of the north pole is indicative of what happens to shapes represented in both types
of maps. At what latitudes are shapes most dramatically affected by changing a map from a globe to flat?
Why is this the case? Question 5: Compare the relative sizes of Greenland and Australia in the two maps? The true values of the
surface areas for these countries are Greenland (2.2 million km
2
) and Australia (7.7 million km
2
). Does
each map demonstrate these true values? Explain the implications of your answer. Celestial Equatorial Coordinates
Work through the introductory material on the page entitled Celestial Equator, Declination, Right Ascension
.
•
Open either the Flat Sky Map Explorer or the Sky Map Explorer
.
•
Familiarize yourself with the same set of features (cursor movement, shifting the map, decimal/sexagesimal) that were available on the previous maps.
•
Make sure that you understand what each check box does.
Question 6: What are the coordinates of the star Eta
Piscium? This star is in the Pisces constellation and
is shown in the figure to the left. Enable show zodiac constellations to be able to locate the correct
star.
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Question 7: The image below, from the Sky Map
Explorer,
shows the celestial sphere including
labeled representations of the celestial equator, the
ecliptic, and the galactic equator. What does it mean
that the galactic equator is angled relative to the
ecliptic? Consider describing the ecliptic plane as a
disk in your answer, or discussing what the galactic
plane might appear to an observer on Earth. Question 8: Complete the following table of positions on the ecliptic.
Ecliptic Location
Approximate Date
Right Ascension
Declination
Vernal Equinox
March 21
Summer Solstice
June 21
Autumnal Equinox
December 21
Question 9: Complete the descriptive criteria for the following items from the Flat Sky Map Explorer
:
Shape of the ecliptic
:
Total range of declination angle of ecliptic
:
Shape of the galactic equator
:
Total range of declination angle of galactic equator
:
Seasons and the Ecliptic
Work through the introductory material on the page entitled Orbits and Light
.
•
Open the Seasons and Ecliptic Simulator
.
•
Note that there are three main panels (left, upper right, and lower right) each of which have two
different views. Controls run along the bottom of the simulation that affect more than one panel.
Click animate and then move through the six views to get an overview this simulator’s capabilities.
We will address each of these six views separately.
•
Experiment with the various methods to advance time in the simulator. You may click the start
animate/stop animation button, drag the yearly time slider, or drag either the sun or the earth in the
left panel to advance time.
•
Note that this animation does not illustrate the rotation of the earth. Because the timescales of
rotation and revolution are so different, it isn’t possible to effectively show both simultaneously. Left
Panel
–
Orbit View
•
Practice clicking and dragging in this panel to change the perspective.
Change the perspective so that you are looking directly down onto the plane
of the Earth’s orbit
•
Click labels. Note that you can see how the direct rays of the sun hit at
different latitudes throughout the year.
•
Experiment with this view until you can quickly create the two views shown below. Note that these
images explain the shape of the elliptic on the celestial sphere. In the image on the left (summer
solstice) an observer on the Earth sees the sun above the celestial equator. In the image on the right
(winter solstice) an observer on the Earth sees the sun below the celestial equator.
Left
Panel
–
Celestial
Sphere
•
This view shows the earth at the center of the celestial sphere. The celestial
equator and the ecliptic with the sun’s location are shown. Note that you may
click on the sun and drag it and read out its coordinates.
•
Experiment with this view until you can quickly create the image to the right –
the direct rays of the sun hitting the earth on the summer solstice.
Upper
Right
Panel
–
View
from
Sun
•
This view shows the earth as seen from the sun. It gives the best view of the
subsolar point – the location on the earth where the
direct rays of the sun are hitting. The noon
observer’s location on the Earth is indicated by a red
parallel of latitude which can be dragged to new latitudes (this affects the
appearance of the lower right panel). It is possible for the red parallel to be
Tip: Note that if you
click and drag the
Earth,
you
will
change the date and
location rather than
the perspective.
at an inaccessible location in this view.
•
Create the image shown to the right – an observer at latitude 80°N on the
summer solstice.
Right
Panel
–
View
from
Side
•
This view shows the earth as seen from a location in the plane of the
ecliptic along a line tangent to the Earth’s orbit. It allows one to easily
see the regions of the Earth that are in daylight and those that are in
shadow.
•
Dragging the stick figure allows one to change latitude very
conveniently. Dragging the stick figure on top of the subsolar point
effectively puts the observer at the latitude where the direct rays of the
sun are hitting.
•
Although rotation is suppressed in this simulation, keep in mind that
the stick figure is on a planet that is rotating with a period of 24 hours
about an axis connecting the north and south poles. Thus, 12 hours
later it will be on the other side of the earth.
•
Set up the simulator for the image at right – the winter solstice for an observer at 80
° N. Since this
observer’s parallel of latitude is located entirely in the shaded region, this observer will not see the
sun on this day.
Lower
Right
Panel
–
Sunbeam Spread
•
This view shows a “cylinder” of light coming from the sun. It is projected on a grid to convey the
area over which the light is spread. As this light is spread over a larger area, its intensity decreases.
Lower
Right
Panel
–
Sunlight
Angle
•
This view shows the angle with which rays of
sunlight are striking the Earth. It lists the noon
sun’s angle with respect to the horizon (its
altitude).
•
Verify that when the noon observer is at the
latitude where the most direct rays of the sun are
hitting, the sun is directly overhead making an
angle of 90
° with the ground.
•
Verify that when the noon observer is at the
latitude where the least direct rays of the sun are
hitting, the sun is on the horizon.
Tip: Once the stick figure is
selected you can gain
greater precision over its
motion by moving the
mouse a distance away
from the figure.
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Question 10: The table below contains entries for the coordinates for the sun on the ecliptic as well as the latitude on Earth where are found the most direct and least direct sunlight rays (just before no light rays). Use the simulation to complete the table.
Question 11: Using the data in the table above, formulate general rules relating the declination of the sun to
the latitude where the most direct and least direct rays of the sun are hitting. Describe your general rule in
the language of a mathematical equation.
Date
RA
DEC
Latitude of Most Direct Sun Rays
Latitude of Least
Direct Sun Rays
January 29
th
February 27
th
22.7
h
−
8.4
°
8.3
° S
81.4
° N
March 13
th
May 18
th
June 24
th
August 31
st
October 8
th
November 15
th
December 22
nd
Question 12: Use the simulator to complete the table below. For each latitude write a short paragraph which
describes the variations in sunlight (seasons) that are experienced at this latitude throughout the year.
Latitude
Description of Yearly Pattern of Sunlight
0°
The noon sun’s angular height above the horizon ranges from 90° on the
vernal equinox, to 66.5° on the summer solstice, to 90° on the autumnal
equinox, and back to 66.5° on the winter solstice. Thus, the equator always
receives very direct intense sunlight throughout the year which accounts for
the very high temperatures.
23.5° N
41° N
66.5° N
90° N
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