Question
and Answers on Earth Shape and Geographic Grid
Chapter
4
Q1:
List and define the three more accurate approximations to the earth’s
shape?
1. The earth
is a sphere: The earth is
considered as spherical shape
Pythagoras (in 6th Century BC) said
that ‘humans must live on a perfect sphere’? Aristotle also argues in the
favor of a spherical earth.
For small scale mapping (continents,
countries, large areas), the earth is still considered as sphere “authalic
sphere” with 6,371 Kilometers as radius and 40,030 KM as a circumference.
2. The earth
is an ellipsoid: The earth is
considered as an ellipse
In 1670, Issac Newton proposed that earth
is an ellipsoid based on his theory of gravity. Earth bulged at equator and
flattened near the poles
Based on satellite data World Geodetic
System (WGS) 72 and 84 ellipsoid gives nearly best fit to the earth shape
(Draw Figure 4.2 on Page 43).
3. The earth
is a geoid:
The earth is considered as 3 Dimension
shape that approximate the Mean Sea Level (MSL) and it is a surface of equal
gravity (equi-potential surface)
Q2: What are
the cartographic use of sphere,
ellipsoid, and geoid?
Sphere
: For small scale mapping
(continents, countries, large areas)
Ellipsoid
: For large scale mapping (topographic maps and cadastral plans)
Geoid
: For horizontal and vertical positions of control points (Elevation
related to Mean Sea Level, Triangulation)
Q3: List and
define the most common coordinate systems used in cartography?
1. Geographical Coordinates: Based on
equator and prime meridian (latitude, longitude)
Draw Figure 4.4 and 4.5
on page 47.
2. Plane coordinates (Cartesian system):
Based on geocenteric approach (the earth’s center) and (X, Y, Z)
Draw Figure 6.7 on page 98.
Q4:Define the
followings:
Latitude
: North-South
angular distance from the equator
Longitude:
East-West angular distance from prime meridian (Greenwich)
Authalic Latitude: North-South distance on
sphere between each degree of latitude (identical value 111.2 KM).
Geodetic Latitude: Distance between
geodetic latitude is not quite same (see authalic latitude). It is greater in
polar areas
(111.69 KM) and less near
the equator (110.57).
Parallel:
Line joining points with the same latitude
Meridian:
Line joining points with the same longitude
Graticule: Imaginary
network of parallels and meridians
Great Circle: the shortest path between
any two points on sphere
Loxodrome: Line of constant azimuth