CONS127_Assignment2_2023_Term1
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University of British Columbia *
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Course
127
Subject
Geography
Date
Dec 6, 2023
Type
Pages
6
Uploaded by PresidentCrabPerson696
1
Cons 127 Observing the Earth from Space
Assignment 2: Where Are You? Google Earth and Geodesy
Instructor: Chris Colton (chris.colton@mail.ubc.ca)
Office: FSC 2223
TA: Tristan Douglas (tjdoug@mail.ubc.ca)
Office hours: Please see the zoom page on the CONS 127 canvas site for office hour details.
Objectives
•
Learn how to use geographic coordinate systems to find and describe locations on the globe.
•
Apply your knowledge of datums and how they can affect geospatial location mapping.
•
Apply your knowledge of projection systems.
Deliverables
•
Answers to questions
1 through 16
•
Submit your answers to the
Assignment 2 Quiz before Oct 5
th
at 11.59 pm
Websites used
•
Google Earth Web
•
Compare Map Projections
•
Convert Geographic Units
•
What UTM Zone am I in?
•
Movable Type Scripts
Notes
•
Please ask assignment questions via the Assignment 2 discussion board, this way your peers can
also benefit from your question. Feel free to email Tristan (
tjdoug@mail.ubc.ca
) if you do not
want to share your question or require an extension for this assignment.
•
Some websites, including
Google Earth Web
and
Compare Map Projections
, are only fully
accessible through a small number of internet browsers. The website are fully accessible via
Google Chrome, Mozilla Firefox and Microsoft Edge
.
•
If the YouTube videos are not available in your country than you should use
UBC’s VPN server
.
Note that the videos are not essential for making this assignment.
•
The internet is at your disposal, feel free to use it to help answer the questions. You are not
expected to memorise every property of each projection, use the internet to investigate the
properties of the projections mentioned in the assignment.
2
Open
Google Earth Web
and change settings following to the
introduction video
. This includes turning off
fly animations, switching measurement units to
‘
meters and kilometers
’
, and changing geographic units
to ‘degree
s, minutes, s
econds’
.
1.
Look up the coordinate
0, 0
and move your cursor around the marker that appears. Watch how the
coordinates at the bottom of the screen are changing in the different directions.
2.
Now make sure gridlines are shown on the map. A latitude and longitude graticule will appear on the
map.
Q1. What are the names of the line of latitude and longitude crossing the 0, 0 coordinate?
3.
Zoom out so that you can see the whole Earth. You should be able to see several yellow lines now
highlighting the Tropics of Cancer and Capricorn and even the Arctic and Antarctic Circles. If you
rotate the Earth, east or west, you should also be able to see the Anti-meridian
Q2. State whether the following statements about the prime meridian, tropics and circles are True
or False.
o
The prime meridian is adopted as the zero of latitude.
o
The prime meridian passes through Greenwich, England.
o
The prime meridian was established by delegates of 25 nations at the international meridian
conferenc
e in 1884, which was held in London on behalf of the United Kingdom’s prime
minister.
o
An international standard prime meridian was mainly established to make navigation over
long distance easier.
o
The tropic of Cancer is the most northern latitude, 23.43658° north of the Equator, where
the sun can be directly overhead. This happens yearly around 21 December (+/- 1 day).
o
The position of the Antarctic Circle is fixed at
66°33′49.3″ south of the Equat
or.
4.
From this distance, i.e. zoomed out, it is easy to see the spherical shape of the Earth. A datum, which
is a reference surface used to generate coordinates (latitude and longitude), is used to approximately
represent the Earth in 3D. This would include
more of the irregularities of the Earth’s surface, such as
the bulge at the equator. However, datums are not detailed enough to represent topographic features
like mountains and valleys.
Q3. Which datum, i.e. reference ellipsoid, is used by Google Earth?
5.
It is also helpful to represent the Earth in two dimensions (2D). A projection is the result of taking 3D
points from a datum (or the Earth’s surface itself) and doing some geometrical transformations to
display them on a 2D flat surface, like a map. A simple introduction of map projections is given in
this
3
video
, including why we need map projections, types and properties (what is distorted and what
preserved).
Q4. What projection system is typically used by online map providers such as OpenStreetMap and
Bing Maps?
Q5. What is the name of map projections that preserve angles locally?
6.
Visit the website
Compare Map Projections
by Tobias Jung. Select and compare a few different map
projections and look at how the grid of graticules changes. Specifically, look at how the boxes change
shape and size vertically and horizontally across the maps. Also, note the comparison of map
silhouettes and the Tissot indicatrix. A Tissot’s Indicatrix uses circles to show the distortion of a
projection at a particular point on the map.
7.
Compare
the ‘Mercator’
,
‘Lambert Cylindrical’
and ‘Gall
-
Peters’
map projections. All are cylindrical
map projections which have straight graticules that cross at 90° angles. The Mercator projection is
one of the most well-known cylindrical map projections. They were developed for different purposes
and preserve metric properties (area, shape, direction and distance) differently.
Q6. Indicate for each map projection whether the metric properties area, shape, direction and
distance are preserved or distorted
Map Projection
Mercator
Lambert Cylindrical
Gall-Peters
Area
Shape
Direction
Distance
8.
On the same website (
Compare Map Projections)
select the ‘Mollweide’
and ‘
Winkel Tripel
’
projection
and inspect the Tissot’s Indicatri
ces to answer Question 7. You may find it helpful to use the
ArcGIS
map projections descriptions
to help answer.
Q7. Indicate whether the following statements are TRUE or FALSE
•
The Mollweide projection preserves scale along the equator
•
The Mollweide projection preserves shapes at two points on the central meridian
•
The Winkel Tripel projection preserves scale along the equator
•
The Winkel Tripel projection preserves area better than the Mollweide projection
9.
Now we have a feel for what different projections do, lets apply this knowledge to a hypothetical
example.
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